swissChili | 729acd5 | 2024-03-05 11:52:45 -0500 | [diff] [blame] | 1 | # |
| 2 | # This file is the units database for use with GNU units, a units conversion |
| 3 | # program by Adrian Mariano adrianm@gnu.org |
| 4 | # |
| 5 | # Febuary 2024 Version 3.19 |
| 6 | # last updated 16 February 2024 |
| 7 | # |
| 8 | # Copyright (C) 1996-2002, 2004-2020, 2022, 2024 |
| 9 | # Free Software Foundation, Inc |
| 10 | # |
| 11 | # This program is free software; you can redistribute it and/or modify |
| 12 | # it under the terms of the GNU General Public License as published by |
| 13 | # the Free Software Foundation; either version 3 of the License, or |
| 14 | # (at your option) any later version. |
| 15 | # |
| 16 | # This program is distributed in the hope that it will be useful, |
| 17 | # but WITHOUT ANY WARRANTY; without even the implied warranty of |
| 18 | # MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the |
| 19 | # GNU General Public License for more details. |
| 20 | # |
| 21 | # You should have received a copy of the GNU General Public License |
| 22 | # along with this program; if not, write to the Free Software |
| 23 | # Foundation, Inc., 51 Franklin Street, Fifth Floor, |
| 24 | # Boston, MA 02110-1301 USA |
| 25 | # |
| 26 | ############################################################################ |
| 27 | # |
| 28 | # Improvements and corrections are welcome. |
| 29 | # |
| 30 | # See the end of this file for a list of items we have chosen to exclude |
| 31 | # or have decided are out of scope for GNU units. |
| 32 | # |
| 33 | # Fundamental constants in this file are the 2018 CODATA recommended values. |
| 34 | # |
| 35 | # Most units data was drawn from |
| 36 | # 1. NIST Special Publication 811, Guide for the |
| 37 | # Use of the International System of Units (SI). |
| 38 | # Barry N. Taylor. 2008 |
| 39 | # https://www.nist.gov/pml/special-publication-811 |
| 40 | # 2. CRC Handbook of Chemistry and Physics 70th edition |
| 41 | # 3. Oxford English Dictionary |
| 42 | # 4. Webster's New Universal Unabridged Dictionary |
| 43 | # 5. Units of Measure by Stephen Dresner |
| 44 | # 6. A Dictionary of English Weights and Measures by Ronald Zupko |
| 45 | # 7. British Weights and Measures by Ronald Zupko |
| 46 | # 8. Realm of Measure by Isaac Asimov |
| 47 | # 9. United States standards of weights and measures, their |
| 48 | # creation and creators by Arthur H. Frazier. |
| 49 | # 10. French weights and measures before the Revolution: a |
| 50 | # dictionary of provincial and local units by Ronald Zupko |
| 51 | # 11. Weights and Measures: their ancient origins and their |
| 52 | # development in Great Britain up to AD 1855 by FG Skinner |
| 53 | # 12. The World of Measurements by H. Arthur Klein |
| 54 | # 13. For Good Measure by William Johnstone |
| 55 | # 14. NTC's Encyclopedia of International Weights and Measures |
| 56 | # by William Johnstone |
| 57 | # 15. Sizes by John Lord |
| 58 | # 16. Sizesaurus by Stephen Strauss |
| 59 | # 17. CODATA Recommended Values of Physical Constants available at |
| 60 | # http://physics.nist.gov/cuu/Constants/index.html |
| 61 | # 18. How Many? A Dictionary of Units of Measurement. Available at |
| 62 | # http://www.ibiblio.org/units/ |
| 63 | # 19. Numericana. http://www.numericana.com |
| 64 | # 20. UK history of measurement |
| 65 | # https://metrication.uk/more/timeline/ |
| 66 | # 21. NIST Handbook 44, Specifications, Tolerances, and |
| 67 | # Other Technical Requirements for Weighing and Measuring |
| 68 | # Devices. 2011 |
| 69 | # 22. NIST Special Publication 447, Weights and Measures Standards |
| 70 | # of the United States: a brief history. Lewis V. Judson. |
| 71 | # 1963; rev. 1976 |
| 72 | # 23. CRC Handbook of Chemistry and Physics, 96th edition |
| 73 | # 24. Dictionary of Scientific Units, 6th ed. H.G. Jerrard and D.B. |
| 74 | # McNeill. 1992 |
| 75 | # 25. NIST Special Publication 330, The International System of |
| 76 | # Units (SI). ed. Barry N. Taylor and Ambler Thompson. 2008 |
| 77 | # https://www.nist.gov/pml/special-publication-330 |
| 78 | # 26. BIPM Brochure, The International System of Units (SI). |
| 79 | # 9th ed., 2019 |
| 80 | # https://www.bipm.org/en/publications/si-brochure/ |
| 81 | # |
| 82 | ########################################################################### |
| 83 | # |
| 84 | # If units you use are missing or defined incorrectly, please contact me. |
| 85 | # If your country's local units are missing and you are willing to supply |
| 86 | # them, please send me a list. |
| 87 | # |
| 88 | ########################################################################### |
| 89 | |
| 90 | ########################################################################### |
| 91 | # |
| 92 | # Brief Philosophy of this file |
| 93 | # |
| 94 | # Most unit definitions are made in terms of integers or simple fractions of |
| 95 | # other definitions. The typical exceptions are when converting between two |
| 96 | # different unit systems, or the values of measured physical constants. In |
| 97 | # this file definitions are given in the most natural and revealing way in |
| 98 | # terms of integer factors. |
| 99 | # |
| 100 | # If you make changes be sure to run 'units --check' to check your work. |
| 101 | # |
| 102 | # The file is USA-centric, but there is some modest effort to support other |
| 103 | # countries. This file is now coded in UTF-8. To support environments where |
| 104 | # UTF-8 is not available, definitions that require this character set are |
| 105 | # wrapped in !utf8 directives. |
| 106 | # |
| 107 | # When a unit name is used in different countries with the different meanings |
| 108 | # the system should be as follows: |
| 109 | # |
| 110 | # Suppose countries ABC and XYZ both use the "foo". Then globally define |
| 111 | # |
| 112 | # ABCfoo <some value> |
| 113 | # XYZfoo <different value> |
| 114 | # |
| 115 | # Then, using the !locale directive, define the "foo" appropriately for each of |
| 116 | # the two countries with a definition like |
| 117 | # |
| 118 | # !locale ABC |
| 119 | # foo ABCfoo |
| 120 | # !endlocale |
| 121 | # |
| 122 | ########################################################################### |
| 123 | |
| 124 | !locale en_US |
| 125 | ! set UNITS_ENGLISH US |
| 126 | !endlocale |
| 127 | |
| 128 | !locale en_GB |
| 129 | ! set UNITS_ENGLISH GB |
| 130 | !endlocale |
| 131 | |
| 132 | !set UNITS_ENGLISH US # Default setting for English units |
| 133 | |
| 134 | !set UNITS_SYSTEM default # Set a default value |
| 135 | |
| 136 | !varnot UNITS_SYSTEM si emu esu gaussian gauss hlu natural natural-gauss hartree planck planck-red default |
| 137 | !message Unknown unit system given with -u or UNITS_SYSTEM environment variable |
| 138 | !message Valid systems: si, emu, esu, gauss[ian], hlu, natural, natural-gauss |
| 139 | !message planck, planck-red, hartree |
| 140 | !message Using SI |
| 141 | !prompt (SI) |
| 142 | !endvar |
| 143 | |
| 144 | !var UNITS_SYSTEM si |
| 145 | !message SI units selected |
| 146 | !prompt (SI) |
| 147 | !endvar |
| 148 | |
| 149 | ########################################################################### |
| 150 | # # |
| 151 | # Primitive units. Any unit defined to contain a '!' character is a # |
| 152 | # primitive unit which will not be reduced any further. All units should # |
| 153 | # reduce to primitive units. # |
| 154 | # # |
| 155 | ########################################################################### |
| 156 | |
| 157 | # |
| 158 | # SI units |
| 159 | # |
| 160 | # On 20 May 2019, the SI was revised to define the units by fixing the |
| 161 | # values of physical constants that depend on those units. |
| 162 | # |
| 163 | # https://www.nist.gov/si-redefinition/ |
| 164 | # |
| 165 | # The BIPM--the International Bureau of Weights and Measures--provides a |
| 166 | # succinct description of the new SI in its Concise Summary: |
| 167 | # |
| 168 | # https://www.bipm.org/utils/common/pdf/si-brochure/SI-Brochure-9-concise-EN.pdf |
| 169 | # |
| 170 | # The SI is the system of units in which: |
| 171 | # |
| 172 | # * the unperturbed ground state hyperfine transition frequency of the |
| 173 | # caesium 133 atom is delta nu_Cs = 9 192 631 770 Hz, |
| 174 | # * the speed of light in vacuum, c, is 299 792 458 m/s, |
| 175 | # * the Planck constant, h, is 6.626 070 15 * 10^-34 J s, |
| 176 | # * the elementary charge, e, is 1.602 176 634 * 10^-19 C, |
| 177 | # * the Boltzmann constant, k, is 1.380 649 * 10^-23 J/K, |
| 178 | # * the Avogadro constant, N_A, is 6.022 140 76 * 10^23 mol^-1, |
| 179 | # * the luminous efficacy of monochromatic radiation of frequency |
| 180 | # 540 * 10^12 Hz, K_cd, is 683 lm/W, |
| 181 | # |
| 182 | # where the hertz, joule, coulomb, lumen, and watt, with unit symbols Hz, |
| 183 | # J, C, lm, and W, respectively, are related to the units second, metre, |
| 184 | # kilogram, ampere, kelvin, mole, and candela, with unit symbols s, m, kg, |
| 185 | # A, K, mol, and cd, respectively, according to Hz = s^-1, J = kg m^2 s^-2, |
| 186 | # C = A s, lm = cd m^2 m^-2 = cd sr, and W = kg m^2 s^-3. |
| 187 | # |
| 188 | # These definitions specify the exact numerical value of each constant when |
| 189 | # its value is expressed in the corresponding SI unit. By fixing the exact |
| 190 | # numerical value the unit becomes defined, since the product of the |
| 191 | # numerical value and the unit has to equal the value of the constant, |
| 192 | # which is invariant. |
| 193 | # |
| 194 | # The defining constants have been chosen such that, when taken together, |
| 195 | # their units cover all of the units of the SI. In general, there is no |
| 196 | # one-to-one correspondence between the defining constants and the SI base |
| 197 | # units. Any SI unit is a product of powers of these seven constants and a |
| 198 | # dimensionless factor. |
| 199 | # |
| 200 | # Until 2018, the SI was defined in terms of base units and derived units. |
| 201 | # These categories are no longer essential in the SI, but they are maintained |
| 202 | # in view of their convenience and widespread use. They are arguably more |
| 203 | # intuitive than the new definitions. (They are also essential to the |
| 204 | # operation of GNU units.) The definitions of the base units, which follow |
| 205 | # from the definition of the SI in terms of the seven defining constants, are |
| 206 | # given below. |
| 207 | # |
| 208 | |
| 209 | s ! # The second, symbol s, is the SI unit of time. It is defined |
| 210 | second s # by taking the fixed numerical value of the unperturbed |
| 211 | # ground-state hyperfine transition frequency of the |
| 212 | # cesium-133 atom to be 9 192 631 770 when expressed in the |
| 213 | # unit Hz, which is equal to 1/s. |
| 214 | # |
| 215 | # This definition is a restatement of the previous one, the |
| 216 | # duration of 9192631770 periods of the radiation corresponding |
| 217 | # to the cesium-133 transition. |
| 218 | |
| 219 | nu_133Cs 9192631770 Hz # Cesium-133 transition frequency (exact) |
| 220 | |
| 221 | c_SI 299792458 |
| 222 | c 299792458 m/s # speed of light in vacuum (exact) |
| 223 | |
| 224 | m ! # The metre, symbol m, is the SI unit of length. It is |
| 225 | meter m # defined by taking the fixed numerical value of the speed |
| 226 | metre m # of light in vacuum, c, to be 299 792 458 when expressed in |
| 227 | # units of m/s. |
| 228 | # |
| 229 | # This definition is a rewording of the previous one and is |
| 230 | # equivalent to defining the meter as the distance light |
| 231 | # travels in 1|299792458 seconds. The meter was originally |
| 232 | # intended to be 1e-7 of the length along a meridian from the |
| 233 | # equator to a pole. |
| 234 | |
| 235 | h_SI 6.62607015e-34 |
| 236 | h 6.62607015e-34 J s # Planck constant (exact) |
| 237 | |
| 238 | kg ! # The kilogram, symbol kg, is the SI unit of mass. It is |
| 239 | kilogram kg # defined by taking the fixed numerical value of the Planck |
| 240 | # constant, h, to be 6.626 070 15 * 10^-34 when expressed in |
| 241 | # the unit J s which is equal to kg m^2 / s. |
| 242 | # |
| 243 | # One advantage of fixing h to define the kilogram is that this |
| 244 | # affects constants used to define the ampere. If the kg were |
| 245 | # defined by directly fixing the mass of something, then h |
| 246 | # would be subject to error. |
| 247 | # |
| 248 | # The previous definition of the kilogram was the mass of the |
| 249 | # international prototype kilogram. The kilogram was the last |
| 250 | # unit whose definition relied on reference to an artifact. |
| 251 | # |
| 252 | # It is not obvious what this new definition means, or |
| 253 | # intuitively how fixing Planck's constant defines the |
| 254 | # kilogram. To define the kilogram we need to give the mass |
| 255 | # of some reference in kilograms. Previously the prototype in |
| 256 | # France served as this reference, and it weighed exactly 1 |
| 257 | # kg. But the reference can have any weight as long as you |
| 258 | # know the weight of the reference. The new definition uses |
| 259 | # the "mass" of a photon, or more accurately, the mass |
| 260 | # equivalent of the energy of a photon. The energy of a |
| 261 | # photon depends on its frequency. If you pick a frequency, |
| 262 | # f, then the energy of the photon is hf, and hence the mass |
| 263 | # equivalent is hf/c^2. If we reduce this expression using |
| 264 | # the constant defined values for h and c the result is a |
| 265 | # value in kilograms for the mass-equivalent of a photon of |
| 266 | # frequency f, which can therefore define the size of the |
| 267 | # kilogram. |
| 268 | # |
| 269 | # For more on the relationship between mass an Planck's |
| 270 | # constant: |
| 271 | # |
| 272 | # https://www.nist.gov/si-redefinition/kilogram-mass-and-plancks-constant |
| 273 | # This definition may still seem rather abstract: you can't |
| 274 | # place a "kilogram of radiation" on one side of a balance. |
| 275 | # Metrologists realize the kilogram using a Kibble Balance, a |
| 276 | # device which relates mechanical energy to electrical energy |
| 277 | # and can measure mass with extreme accuracy if h is known. |
| 278 | # |
| 279 | # For more on the Kibble Balance see |
| 280 | # |
| 281 | # https://www.nist.gov/si-redefinition/kilogram-kibble-balance |
| 282 | # https://en.wikipedia.org/wiki/Kibble_balance |
| 283 | |
| 284 | k_SI 1.380649e-23 |
| 285 | boltzmann 1.380649e-23 J/K # Boltzmann constant (exact) |
| 286 | k boltzmann |
| 287 | |
| 288 | K ! # The kelvin, symbol K, is the SI unit of thermodynamic |
| 289 | kelvin K # temperature. It is defined by taking the fixed numerical |
| 290 | # value of the Boltzmann constant, k, to be 1.380 649 * 10^-23 |
| 291 | # when expressed in the unit J/K, which is equal to |
| 292 | # kg m^2/s^2 K. |
| 293 | # |
| 294 | # The boltzmann constant establishes the relationship between |
| 295 | # energy and temperature. The average thermal energy carried |
| 296 | # by each degree of freedom is kT/2. A monatomic ideal gas |
| 297 | # has three degrees of freedom corresponding to the three |
| 298 | # spatial directions, which means its thermal energy is |
| 299 | # (3/2) k T. |
| 300 | # |
| 301 | # The previous definition of the kelvin was based on the |
| 302 | # triple point of water. The change in the definition of the |
| 303 | # kelvin will not have much effect on measurement practice. |
| 304 | # Practical temperature calibration makes use of two scales, |
| 305 | # the International Temperature Scale of 1990 (ITS-90), which |
| 306 | # covers the range of 0.65 K to 1357.77K and the Provisional |
| 307 | # Low Temperature Scale of 2000 (PLTS-2000), which covers the |
| 308 | # range of 0.9 mK to 1 K. |
| 309 | # https://www.bipm.org/en/committees/cc/cct/publications-cc.html |
| 310 | # |
| 311 | # The ITS-90 contains 17 reference points including things |
| 312 | # like the triple point of hydrogen (13.8033 K) or the |
| 313 | # freezing point of gold (1337.33 K), and of course the triple |
| 314 | # point of water. The PLTS-2000 specifies four reference |
| 315 | # points, all based on properties of helium-3. |
| 316 | # |
| 317 | # The redefinition of the kelvin will not affect the values of |
| 318 | # these reference points, which have been determined by |
| 319 | # primary thermometry, using thermometers that rely only on |
| 320 | # relationships that allow temperature to be calculated |
| 321 | # directly without using any unknown quantities. Examples |
| 322 | # include acoustic thermometers, which measure the speed of |
| 323 | # sound in a gas, or electronic thermometers, which measure |
| 324 | # tiny voltage fluctuations in resistors. Both variables |
| 325 | # depend directly on temperature. |
| 326 | |
| 327 | e_SI 1.602176634e-19 |
| 328 | e 1.602176634e-19 C # electron charge (exact) |
| 329 | |
| 330 | A ! # The ampere, symbol A, is the SI unit of electric current. |
| 331 | ampere A # It is defined by taking the fixed numerical value of the |
| 332 | amp ampere # elementary charge, e, to be 1.602 176 634 * 10^-19 when |
| 333 | # expressed in the unit C, which is equal to A*s. |
| 334 | # |
| 335 | # The previous definition was the current which produces a |
| 336 | # force of 2e-7 N/m between two infinitely long wires a meter |
| 337 | # apart. This definition was difficult to realize accurately. |
| 338 | # |
| 339 | # The ampere is actually realized by establishing the volt and |
| 340 | # the ohm, since A = V / ohm. These measurements can be done |
| 341 | # using the Josephson effect and the quantum Hall effect, |
| 342 | # which accurately measure voltage and resistance, respectively, |
| 343 | # with reference to two fixed constants, the Josephson |
| 344 | # constant, K_J=2e/h and the von Klitzing constant, R_K=h/e^2. |
| 345 | # Under the previous SI system, these constants had official |
| 346 | # fixed values, defined in 1990. This created a situation |
| 347 | # where the standard values for the volt and ohm were in some |
| 348 | # sense outside of SI because they depended primarily on |
| 349 | # constants different from the ones used to define SI. After |
| 350 | # the revision, since e and h have exact definitions, the |
| 351 | # Josephson and von Klitzing constants will also have exact |
| 352 | # definitions that derive from SI instead of the conventional |
| 353 | # 1990 values. |
| 354 | # |
| 355 | # In fact we know that there is a small offset between the |
| 356 | # conventional values of the electrical units based on the |
| 357 | # conventional 1990 values and the SI values. The new |
| 358 | # definition, which brings the practical electrical units back |
| 359 | # into SI, will lead to a one time change of +0.1ppm for |
| 360 | # voltage values and +0.02ppm for resistance values. |
| 361 | # |
| 362 | # The previous definition resulted in fixed exact values for |
| 363 | # the vacuum permeability (mu0), the impedance of free space |
| 364 | # (Z0), the vacuum permittivity (epsilon0), and the Coulomb |
| 365 | # constant. With the new definition, these four values are |
| 366 | # subject to experimental error. |
| 367 | |
| 368 | avogadro 6.02214076e23 / mol # Size of a mole (exact) |
| 369 | N_A avogadro |
| 370 | |
| 371 | mol ! # The mole, symbol mol, is the SI unit of amount of |
| 372 | mole mol # substance. One mole contains exactly 6.022 140 76 * 10^23 |
| 373 | # elementary entities. This number is the fixed numerical |
| 374 | # value of the Avogadro constant, N_A, when expressed in the |
| 375 | # unit 1/mol and is called the Avogadro number. The amount of |
| 376 | # substance, symbol n, of a system is a measure of the number |
| 377 | # of specified elementary entities. An elementary entity may |
| 378 | # be an atom, a molecule, an ion, an electron, any other |
| 379 | # particle or specified group of particles. |
| 380 | # |
| 381 | # The atomic mass unit (u) is defined as 1/12 the mass of |
| 382 | # carbon-12. Previously the mole was defined so that a mole |
| 383 | # of carbon-12 weighed exactly 12g, or N_A u = 1 g/mol |
| 384 | # exactly. This relationship is now an experimental, |
| 385 | # approximate relationship. |
| 386 | # |
| 387 | # To determine the size of the mole, researchers used spheres |
| 388 | # of very pure silicon-28 that weighed a kilogram. They |
| 389 | # measured the molar mass of Si-28 using mass spectrometry and |
| 390 | # used X-ray diffraction interferometry to determine the |
| 391 | # spacing of the silicon atoms in the sphere. Using the |
| 392 | # sphere's volume it was then possible to determine the number |
| 393 | # of silicon atoms in the sphere, and hence determine the |
| 394 | # Avogadro constant. The results of this experiment were used |
| 395 | # to define N_A, which is henceforth a fixed, unchanging |
| 396 | # quantity. |
| 397 | |
| 398 | cd ! # The candela, symbol cd, is the SI unit of luminous intensity |
| 399 | candela cd # in a given direction. It is defined by taking the fixed |
| 400 | # numerical value of the luminous efficacy of monochromatic |
| 401 | # radiation of the frequency 540e12 Hz to be 683 when |
| 402 | # expressed in the unit lumen/watt, which is equal to |
| 403 | # cd sr/W, or cd sr s^3/kg m^2 |
| 404 | # |
| 405 | # This definition is a rewording of the previous definition. |
| 406 | # Luminous intensity differs from radiant intensity (W/sr) in |
| 407 | # that it is adjusted for human perceptual dependence on |
| 408 | # wavelength. The frequency of 540e12 Hz (yellow; |
| 409 | # wavelength approximately 555 nm in vacuum) is where human |
| 410 | # perception is most efficient. |
| 411 | |
| 412 | K_cd 683 lumen/W # Luminous efficiency at 540e12 Hz (exact) |
| 413 | |
| 414 | # Angular Measure |
| 415 | # |
| 416 | # The radian and steradian are defined as dimensionless primitive units. |
| 417 | # The radian is equal to m/m and the steradian to m^2/m^2 so these units are |
| 418 | # dimensionless. Retaining them as named units is useful because it allows |
| 419 | # clarity in expressions and makes the meaning of unit definitions more clear. |
| 420 | # These units will reduce to 1 in conversions but not for sums of units or for |
| 421 | # arguments to functions. |
| 422 | # |
| 423 | |
| 424 | radian !dimensionless # Plane angle subtended at the center of a circle by |
| 425 | # an arc equal in length to the radius of the |
| 426 | # circle. |
| 427 | # Dimension: LENGTH (of arc) / DISTANCE (radius) |
| 428 | |
| 429 | sr !dimensionless # Solid angle which cuts off an area of the surface |
| 430 | steradian sr # of the sphere equal to that of a square with |
| 431 | # sides of length equal to the radius of the |
| 432 | # sphere. |
| 433 | # Dimension: AREA (of surface) / DISTANCE^2 |
| 434 | # (radius^2) |
| 435 | # |
| 436 | # A primitive non-SI unit |
| 437 | # |
| 438 | |
| 439 | bit ! # Basic unit of information (entropy). The entropy in bits |
| 440 | # of a random variable over a finite alphabet is defined |
| 441 | # to be the sum of -p(i)*log2(p(i)) over the alphabet where |
| 442 | # p(i) is the probability that the random variable takes |
| 443 | # on the value i. |
| 444 | |
| 445 | # |
| 446 | # Currency: the primitive unit of currency is defined in currency.units. |
| 447 | # It is usually the US$ or the euro, but it is user selectable. |
| 448 | # |
| 449 | |
| 450 | # |
| 451 | # Absolute value |
| 452 | # |
| 453 | |
| 454 | abs(x) noerror sqrt(x^2) |
| 455 | |
| 456 | ########################################################################### |
| 457 | # # |
| 458 | # Prefixes (longer names must come first) # |
| 459 | # # |
| 460 | ########################################################################### |
| 461 | |
| 462 | quetta- 1e30 # Allegedly from "q" plus Greek "deka" (ten) |
| 463 | ronna- 1e27 # Allegedly from "r" plus Greek "ennea" (nine) |
| 464 | yotta- 1e24 # Greek or Latin "octo" (eight) |
| 465 | zetta- 1e21 # Latin "septem" (seven) |
| 466 | exa- 1e18 # Greek "hex" (six) |
| 467 | peta- 1e15 # Greek "pente" (five) |
| 468 | tera- 1e12 # Greek "teras" (monster) |
| 469 | giga- 1e9 # Greek "gigas" (giant) |
| 470 | mega- 1e6 # Greek "megas" (large) |
| 471 | myria- 1e4 # Not an official SI prefix |
| 472 | kilo- 1e3 # Greek "chilioi" (thousand) |
| 473 | hecto- 1e2 # Greek "hekaton" (hundred) |
| 474 | deca- 1e1 # Greek "deka" (ten) |
| 475 | deka- deca |
| 476 | deci- 1e-1 # Latin "decimus" (tenth) |
| 477 | centi- 1e-2 # Latin "centum" (hundred) |
| 478 | milli- 1e-3 # Latin "mille" (thousand) |
| 479 | micro- 1e-6 # Latin "micro" or Greek "mikros" (small) |
| 480 | nano- 1e-9 # Latin "nanus" or Greek "nanos" (dwarf) |
| 481 | pico- 1e-12 # Spanish "pico" (a bit) |
| 482 | femto- 1e-15 # Danish-Norwegian "femten" (fifteen) |
| 483 | atto- 1e-18 # Danish-Norwegian "atten" (eighteen) |
| 484 | zepto- 1e-21 # Latin "septem" (seven) |
| 485 | yocto- 1e-24 # Greek or Latin "octo" (eight) |
| 486 | ronto- 1e-27 # Allegedly "r" plus Latin "novum" (nine) |
| 487 | quecto- 1e-30 # Allegedly "q" plus Latin "decim" (ten) |
| 488 | |
| 489 | quarter- 1|4 |
| 490 | semi- 0.5 |
| 491 | demi- 0.5 |
| 492 | hemi- 0.5 |
| 493 | half- 0.5 |
| 494 | double- 2 |
| 495 | triple- 3 |
| 496 | treble- 3 |
| 497 | |
| 498 | kibi- 2^10 # In response to the improper and confusing |
| 499 | mebi- 2^20 # use of SI prefixes for powers of two, |
| 500 | gibi- 2^30 # the International Electrotechnical |
| 501 | tebi- 2^40 # Commission aproved these binary prefixes |
| 502 | pebi- 2^50 # in IEC 60027-2 Amendment 2 (1999). |
| 503 | exbi- 2^60 |
| 504 | zebi- 2^70 # Zebi- and yobi- were added in the 2005 ed., |
| 505 | yobi- 2^80 # later superseded by ISO/IEC 80000-13:2008. |
| 506 | robi- 2^90 |
| 507 | quebi- 2^100 |
| 508 | Ki- kibi |
| 509 | Mi- mebi |
| 510 | Gi- gibi |
| 511 | Ti- tebi |
| 512 | Pi- pebi |
| 513 | Ei- exbi |
| 514 | Zi- zebi |
| 515 | Yi- yobi |
| 516 | Ri- robi |
| 517 | Qi- quebi |
| 518 | |
| 519 | Q- quetta |
| 520 | R- ronna |
| 521 | Y- yotta |
| 522 | Z- zetta |
| 523 | E- exa |
| 524 | P- peta |
| 525 | T- tera |
| 526 | G- giga |
| 527 | M- mega |
| 528 | k- kilo |
| 529 | h- hecto |
| 530 | da- deka |
| 531 | d- deci |
| 532 | c- centi |
| 533 | m- milli |
| 534 | u- micro # it should be a mu but u is easy to type |
| 535 | n- nano |
| 536 | p- pico |
| 537 | f- femto |
| 538 | a- atto |
| 539 | z- zepto |
| 540 | y- yocto |
| 541 | r- ronto |
| 542 | q- quecto |
| 543 | |
| 544 | # |
| 545 | # Names of some numbers |
| 546 | # |
| 547 | |
| 548 | one 1 |
| 549 | two 2 |
| 550 | double 2 |
| 551 | couple 2 |
| 552 | three 3 |
| 553 | triple 3 |
| 554 | four 4 |
| 555 | quadruple 4 |
| 556 | five 5 |
| 557 | quintuple 5 |
| 558 | six 6 |
| 559 | seven 7 |
| 560 | eight 8 |
| 561 | nine 9 |
| 562 | ten 10 |
| 563 | eleven 11 |
| 564 | twelve 12 |
| 565 | thirteen 13 |
| 566 | fourteen 14 |
| 567 | fifteen 15 |
| 568 | sixteen 16 |
| 569 | seventeen 17 |
| 570 | eighteen 18 |
| 571 | nineteen 19 |
| 572 | twenty 20 |
| 573 | thirty 30 |
| 574 | forty 40 |
| 575 | fifty 50 |
| 576 | sixty 60 |
| 577 | seventy 70 |
| 578 | eighty 80 |
| 579 | ninety 90 |
| 580 | hundred 100 |
| 581 | thousand 1000 |
| 582 | million 1e6 |
| 583 | |
| 584 | twoscore two score |
| 585 | threescore three score |
| 586 | fourscore four score |
| 587 | fivescore five score |
| 588 | sixscore six score |
| 589 | sevenscore seven score |
| 590 | eightscore eight score |
| 591 | ninescore nine score |
| 592 | tenscore ten score |
| 593 | twelvescore twelve score |
| 594 | |
| 595 | # These number terms were described by N. Chuquet and De la Roche in the 16th |
| 596 | # century as being successive powers of a million. These definitions are still |
| 597 | # used in most European countries. The current US definitions for these |
| 598 | # numbers arose in the 17th century and don't make nearly as much sense. These |
| 599 | # numbers are listed in the CRC Concise Encyclopedia of Mathematics by Eric |
| 600 | # W. Weisstein. |
| 601 | |
| 602 | shortbillion 1e9 |
| 603 | shorttrillion 1e12 |
| 604 | shortquadrillion 1e15 |
| 605 | shortquintillion 1e18 |
| 606 | shortsextillion 1e21 |
| 607 | shortseptillion 1e24 |
| 608 | shortoctillion 1e27 |
| 609 | shortnonillion 1e30 |
| 610 | shortnoventillion shortnonillion |
| 611 | shortdecillion 1e33 |
| 612 | shortundecillion 1e36 |
| 613 | shortduodecillion 1e39 |
| 614 | shorttredecillion 1e42 |
| 615 | shortquattuordecillion 1e45 |
| 616 | shortquindecillion 1e48 |
| 617 | shortsexdecillion 1e51 |
| 618 | shortseptendecillion 1e54 |
| 619 | shortoctodecillion 1e57 |
| 620 | shortnovemdecillion 1e60 |
| 621 | shortvigintillion 1e63 |
| 622 | |
| 623 | centillion 1e303 |
| 624 | googol 1e100 |
| 625 | |
| 626 | longbillion million^2 |
| 627 | longtrillion million^3 |
| 628 | longquadrillion million^4 |
| 629 | longquintillion million^5 |
| 630 | longsextillion million^6 |
| 631 | longseptillion million^7 |
| 632 | longoctillion million^8 |
| 633 | longnonillion million^9 |
| 634 | longnoventillion longnonillion |
| 635 | longdecillion million^10 |
| 636 | longundecillion million^11 |
| 637 | longduodecillion million^12 |
| 638 | longtredecillion million^13 |
| 639 | longquattuordecillion million^14 |
| 640 | longquindecillion million^15 |
| 641 | longsexdecillion million^16 |
| 642 | longseptdecillion million^17 |
| 643 | longoctodecillion million^18 |
| 644 | longnovemdecillion million^19 |
| 645 | longvigintillion million^20 |
| 646 | |
| 647 | # These numbers fill the gaps left by the long system above. |
| 648 | |
| 649 | milliard 1000 million |
| 650 | billiard 1000 million^2 |
| 651 | trilliard 1000 million^3 |
| 652 | quadrilliard 1000 million^4 |
| 653 | quintilliard 1000 million^5 |
| 654 | sextilliard 1000 million^6 |
| 655 | septilliard 1000 million^7 |
| 656 | octilliard 1000 million^8 |
| 657 | nonilliard 1000 million^9 |
| 658 | noventilliard nonilliard |
| 659 | decilliard 1000 million^10 |
| 660 | |
| 661 | # For consistency |
| 662 | |
| 663 | longmilliard milliard |
| 664 | longbilliard billiard |
| 665 | longtrilliard trilliard |
| 666 | longquadrilliard quadrilliard |
| 667 | longquintilliard quintilliard |
| 668 | longsextilliard sextilliard |
| 669 | longseptilliard septilliard |
| 670 | longoctilliard octilliard |
| 671 | longnonilliard nonilliard |
| 672 | longnoventilliard noventilliard |
| 673 | longdecilliard decilliard |
| 674 | |
| 675 | # The long centillion would be 1e600. The googolplex is another |
| 676 | # familiar large number equal to 10^googol. These numbers give overflows. |
| 677 | |
| 678 | # |
| 679 | # The short system prevails in English speaking countries |
| 680 | # |
| 681 | |
| 682 | billion shortbillion |
| 683 | trillion shorttrillion |
| 684 | quadrillion shortquadrillion |
| 685 | quintillion shortquintillion |
| 686 | sextillion shortsextillion |
| 687 | septillion shortseptillion |
| 688 | octillion shortoctillion |
| 689 | nonillion shortnonillion |
| 690 | noventillion shortnoventillion |
| 691 | decillion shortdecillion |
| 692 | undecillion shortundecillion |
| 693 | duodecillion shortduodecillion |
| 694 | tredecillion shorttredecillion |
| 695 | quattuordecillion shortquattuordecillion |
| 696 | quindecillion shortquindecillion |
| 697 | sexdecillion shortsexdecillion |
| 698 | septendecillion shortseptendecillion |
| 699 | octodecillion shortoctodecillion |
| 700 | novemdecillion shortnovemdecillion |
| 701 | vigintillion shortvigintillion |
| 702 | |
| 703 | # |
| 704 | # Numbers used in India |
| 705 | # |
| 706 | |
| 707 | lakh 1e5 |
| 708 | crore 1e7 |
| 709 | arab 1e9 |
| 710 | kharab 1e11 |
| 711 | neel 1e13 |
| 712 | padm 1e15 |
| 713 | shankh 1e17 |
| 714 | |
| 715 | ############################################################################# |
| 716 | # # |
| 717 | # Derived units which can be reduced to the primitive units # |
| 718 | # # |
| 719 | ############################################################################# |
| 720 | |
| 721 | |
| 722 | |
| 723 | # |
| 724 | # Named SI derived units (officially accepted) |
| 725 | # |
| 726 | |
| 727 | newton kg m / s^2 # force |
| 728 | N newton |
| 729 | pascal N/m^2 # pressure or stress |
| 730 | Pa pascal |
| 731 | joule N m # energy |
| 732 | J joule |
| 733 | watt J/s # power |
| 734 | W watt |
| 735 | coulomb A s # charge |
| 736 | C coulomb |
| 737 | volt W/A # potential difference |
| 738 | V volt |
| 739 | ohm V/A # electrical resistance |
| 740 | siemens A/V # electrical conductance |
| 741 | S siemens |
| 742 | farad C/V # capacitance |
| 743 | F farad |
| 744 | weber V s # magnetic flux |
| 745 | Wb weber |
| 746 | henry V s / A # inductance, also Wb/A, but needs to be |
| 747 | H henry # defined this way for CGS units |
| 748 | tesla Wb/m^2 # magnetic flux density |
| 749 | T tesla |
| 750 | hertz /s # frequency |
| 751 | Hz hertz |
| 752 | |
| 753 | # |
| 754 | # Dimensions. These are here to help with dimensional analysis and |
| 755 | # because they will appear in the list produced by hitting '?' at the |
| 756 | # "You want:" prompt to tell the user the dimension of the unit. |
| 757 | # |
| 758 | |
| 759 | LENGTH meter |
| 760 | AREA LENGTH^2 |
| 761 | VOLUME LENGTH^3 |
| 762 | MASS kilogram |
| 763 | AMOUNT mole |
| 764 | ANGLE radian |
| 765 | SOLID_ANGLE steradian |
| 766 | MONEY US$ |
| 767 | FORCE newton |
| 768 | PRESSURE FORCE / AREA |
| 769 | STRESS FORCE / AREA |
| 770 | FREQUENCY hertz |
| 771 | WAVELENGTH LENGTH |
| 772 | WAVENUMBER 1/WAVELENGTH # number of waves per distance |
| 773 | VELOCITY DISPLACEMENT / TIME # a vector (includes direction) |
| 774 | SPEED DISTANCE / TIME # a scalar |
| 775 | ACCELERATION VELOCITY / TIME |
| 776 | MOMENTUM MASS VELOCITY # Also ENERGY / VELOCITY or IMPULSE |
| 777 | IMPULSE FORCE TIME |
| 778 | DISPLACEMENT LENGTH |
| 779 | DISTANCE LENGTH |
| 780 | ELONGATION LENGTH |
| 781 | STRAIN ELONGATION / LENGTH |
| 782 | ENERGY joule |
| 783 | POWER watt |
| 784 | WORK FORCE DISTANCE |
| 785 | DENSITY MASS / VOLUME |
| 786 | LINEAR_DENSITY MASS / LENGTH |
| 787 | SPECIFIC_ENERGY ENERGY / MASS |
| 788 | VISCOSITY FORCE TIME / AREA |
| 789 | KINEMATIC_VISCOSITY VISCOSITY / DENSITY |
| 790 | CURRENT ampere |
| 791 | CHARGE coulomb |
| 792 | CAPACITANCE farad |
| 793 | RESISTANCE ohm |
| 794 | CONDUCTANCE siemens |
| 795 | # It may be easier to understand the relationship by considering |
| 796 | # an object with specified dimensions and resistivity, whose |
| 797 | # resistance is given by the resistivity * length / area. |
| 798 | RESISTIVITY RESISTANCE AREA / LENGTH |
| 799 | CONDUCTIVITY CONDUCTANCE LENGTH / AREA |
| 800 | INDUCTANCE henry |
| 801 | E_FIELD ELECTRIC_POTENTIAL / LENGTH |
| 802 | B_FIELD tesla |
| 803 | # The D and H fields are related to the E and B fields by factors of |
| 804 | # epsilon and mu respectively, so their units can be found by |
| 805 | # multiplying/dividing by the epsilon0 and mu0. The more complex |
| 806 | # definitions below make it possible to use D_FIELD and E_FIELD to |
| 807 | # convert between SI and CGS units for these dimensions. |
| 808 | D_FIELD E_FIELD epsilon0 / epsilon0_SI # mu0_SI c^2 F / m |
| 809 | H_FIELD B_FIELD / (mu0/mu0_SI) |
| 810 | ELECTRIC_DIPOLE_MOMENT C m |
| 811 | MAGNETIC_DIPOLE_MOMENT J / T |
| 812 | POLARIZATION ELECTRIC_DIPOLE_MOMENT / VOLUME |
| 813 | MAGNETIZATION MAGNETIC_DIPOLE_MOMENT / VOLUME |
| 814 | ELECTRIC_POTENTIAL ENERGY / CHARGE #volt |
| 815 | VOLTAGE ELECTRIC_POTENTIAL |
| 816 | E_FLUX E_FIELD AREA |
| 817 | D_FLUX D_FIELD AREA |
| 818 | B_FLUX B_FIELD AREA |
| 819 | H_FLUX H_FIELD AREA |
| 820 | |
| 821 | # |
| 822 | # units derived easily from SI units |
| 823 | # |
| 824 | |
| 825 | gram millikg |
| 826 | gm gram |
| 827 | g gram |
| 828 | tonne 1000 kg |
| 829 | t tonne |
| 830 | metricton tonne |
| 831 | sthene tonne m / s^2 |
| 832 | funal sthene |
| 833 | pieze sthene / m^2 |
| 834 | quintal 100 kg |
| 835 | bar 1e5 Pa # About 1 atm |
| 836 | b bar |
| 837 | vac millibar |
| 838 | micron micrometer # One millionth of a meter |
| 839 | bicron picometer # One brbillionth of a meter |
| 840 | cc cm^3 |
| 841 | are 100 m^2 |
| 842 | a are |
| 843 | liter 1000 cc # The liter was defined in 1901 as the |
| 844 | oldliter 1.000028 dm^3 # space occupied by 1 kg of pure water at |
| 845 | L liter # the temperature of its maximum density |
| 846 | l liter # under a pressure of 1 atm. This was |
| 847 | # supposed to be 1000 cubic cm, but it |
| 848 | # was discovered that the original |
| 849 | # measurement was off. In 1964, the |
| 850 | # liter was redefined to be exactly 1000 |
| 851 | # cubic centimeters. |
| 852 | Ah amp hour # Unit of charge |
| 853 | mho siemens # Inverse of ohm, hence ohm spelled backward |
| 854 | galvat ampere # Named after Luigi Galvani |
| 855 | angstrom 1e-10 m # Convenient for describing molecular sizes |
| 856 | xunit xunit_cu # Used for measuring x-ray wavelengths. |
| 857 | siegbahn xunit # Originally defined to be 1|3029.45 of |
| 858 | xunit_cu 1.00207697e-13 m # the spacing of calcite planes at 18 |
| 859 | xunit_mo 1.00209952e-13 m # degC. It was intended to be exactly |
| 860 | # 1e-13 m, but was later found to be |
| 861 | # slightly off. Current usage is with |
| 862 | # reference to common x-ray lines, either |
| 863 | # the K-alpha 1 line of copper or the |
| 864 | # same line of molybdenum. |
| 865 | angstromstar 1.00001495 angstrom # Defined by JA Bearden in 1965 to replace |
| 866 | # the X unit. The wavelength of the |
| 867 | # tungsten K alpha1 line was defined as |
| 868 | # exactly 0.20901 angstrom star, with the |
| 869 | # value chosen to try to make the new |
| 870 | # unit close to the angstrom. |
| 871 | silicon_d220 1.920155716e-10 m # Silicon lattice spacing |
| 872 | siliconlattice sqrt(8) silicon_d220# Silicon lattice parameter, (a), the side |
| 873 | # length of the unit cell for the diamond |
| 874 | # centered cubic structure of silicon. |
| 875 | fermi 1e-15 m # Convenient for describing nuclear sizes |
| 876 | # Nuclear radius is from 1 to 10 fermis |
| 877 | barn 1e-28 m^2 # Used to measure cross section for |
| 878 | # particle physics collision, said to |
| 879 | # have originated in the phrase "big as |
| 880 | # a barn". |
| 881 | shed 1e-24 barn # Defined to be a smaller companion to the |
| 882 | # barn, but it's too small to be of |
| 883 | # much use. |
| 884 | brewster micron^2/N # measures stress-optical coef |
| 885 | diopter /m # measures reciprocal of lens focal length |
| 886 | fresnel 1e12 Hz # occasionally used in spectroscopy |
| 887 | shake 1e-8 sec |
| 888 | svedberg 1e-13 s # Used for measuring the sedimentation |
| 889 | # coefficient for centrifuging. |
| 890 | gamma microgram # Also used for 1e-9 tesla |
| 891 | lambda microliter |
| 892 | spat 1e12 m # Rarely used for astronomical measurements |
| 893 | preece 1e13 ohm m # resistivity |
| 894 | planck J s # action of one joule over one second |
| 895 | sturgeon /henry # magnetic reluctance |
| 896 | daraf 1/farad # elastance (farad spelled backwards) |
| 897 | leo 10 m/s^2 |
| 898 | poiseuille N s / m^2 # viscosity |
| 899 | mayer J/g K # specific heat |
| 900 | mired / microK # reciprocal color temperature. The name |
| 901 | # abbreviates micro reciprocal degree. |
| 902 | crocodile megavolt # used informally in UK physics labs |
| 903 | metricounce 25 g |
| 904 | mounce metricounce |
| 905 | finsenunit 1e5 W/m^2 # Measures intensity of ultraviolet light |
| 906 | # with wavelength 296.7 nm. |
| 907 | fluxunit 1e-26 W/m^2 Hz # Used in radio astronomy to measure |
| 908 | # the energy incident on the receiving |
| 909 | # body across a specified frequency |
| 910 | # bandwidth. [12] |
| 911 | jansky fluxunit # K. G. Jansky identified radio waves coming |
| 912 | Jy jansky # from outer space in 1931. |
| 913 | flick W / cm^2 sr micrometer # Spectral radiance or irradiance |
| 914 | pfu / cm^2 sr s # particle flux unit -- Used to measure |
| 915 | # rate at which particles are received by |
| 916 | # a spacecraft as particles per solid |
| 917 | # angle per detector area per second. [18] |
| 918 | pyron cal_IT / cm^2 min # Measures heat flow from solar radiation, |
| 919 | # from Greek work "pyr" for fire. |
| 920 | katal mol/sec # Measure of the amount of a catalyst. One |
| 921 | kat katal # katal of catalyst enables the reaction |
| 922 | # to consume or produce one mol/sec. |
| 923 | solarluminosity 382.8e24 W # A common yardstick for comparing the |
| 924 | # output of different stars. |
| 925 | # http://nssdc.gsfc.nasa.gov/planetary/factsheet/sunfact.html |
| 926 | # at mean Earth-Sun distance |
| 927 | solarirradiance solarluminosity / (4 pi sundist^2) |
| 928 | solarconstant solarirradiance |
| 929 | TSI solarirradiance # total solar irradiance |
| 930 | |
| 931 | # |
| 932 | # time |
| 933 | # |
| 934 | |
| 935 | sec s |
| 936 | minute 60 s |
| 937 | min minute |
| 938 | hour 60 min |
| 939 | hr hour |
| 940 | day 24 hr |
| 941 | d day |
| 942 | da day |
| 943 | week 7 day |
| 944 | wk week |
| 945 | sennight 7 day |
| 946 | fortnight 14 day |
| 947 | blink 1e-5 day # Actual human blink takes 1|3 second |
| 948 | ce 1e-2 day |
| 949 | cron 1e6 years |
| 950 | watch 4 hours # time a sentry stands watch or a ship's |
| 951 | # crew is on duty. |
| 952 | bell 1|8 watch # Bell would be sounded every 30 minutes. |
| 953 | |
| 954 | # French Revolutionary Time or Decimal Time. It was Proposed during |
| 955 | # the French Revolution. A few clocks were made, but it never caught |
| 956 | # on. In 1998 Swatch defined a time measurement called ".beat" and |
| 957 | # sold some watches that displayed time in this unit. |
| 958 | |
| 959 | decimalhour 1|10 day |
| 960 | decimalminute 1|100 decimalhour |
| 961 | decimalsecond 1|100 decimalminute |
| 962 | beat decimalminute # Swatch Internet Time |
| 963 | |
| 964 | # |
| 965 | # angular measure |
| 966 | # |
| 967 | |
| 968 | circle 2 pi radian |
| 969 | degree 1|360 circle |
| 970 | deg degree |
| 971 | arcdeg degree |
| 972 | arcmin 1|60 degree |
| 973 | arcminute arcmin |
| 974 | ' arcmin |
| 975 | arcsec 1|60 arcmin |
| 976 | arcsecond arcsec |
| 977 | " arcsec |
| 978 | '' " |
| 979 | rightangle 90 degrees |
| 980 | quadrant 1|4 circle |
| 981 | quintant 1|5 circle |
| 982 | sextant 1|6 circle |
| 983 | |
| 984 | sign 1|12 circle # Angular extent of one sign of the zodiac |
| 985 | turn circle |
| 986 | revolution turn |
| 987 | rev turn |
| 988 | pulsatance radian / sec |
| 989 | gon 1|100 rightangle # measure of grade |
| 990 | grade gon |
| 991 | centesimalminute 1|100 grade |
| 992 | centesimalsecond 1|100 centesimalminute |
| 993 | milangle 1|6400 circle # Official NIST definition. |
| 994 | # Another choice is 1e-3 radian. |
| 995 | pointangle 1|32 circle # Used for reporting compass readings |
| 996 | centrad 0.01 radian # Used for angular deviation of light |
| 997 | # through a prism. |
| 998 | mas milli arcsec # Used by astronomers |
| 999 | seclongitude circle (seconds/day) # Astronomers measure longitude |
| 1000 | # (which they call right ascension) in |
| 1001 | # time units by dividing the equator into |
| 1002 | # 24 hours instead of 360 degrees. |
| 1003 | # |
| 1004 | # Some geometric formulas |
| 1005 | # |
| 1006 | |
| 1007 | circlearea(r) units=[m;m^2] range=[0,) pi r^2 ; sqrt(circlearea/pi) |
| 1008 | spherevolume(r) units=[m;m^3] range=[0,) 4|3 pi r^3 ; \ |
| 1009 | cuberoot(spherevolume/4|3 pi) |
| 1010 | spherevol() spherevolume |
| 1011 | square(x) range=[0,) x^2 ; sqrt(square) |
| 1012 | |
| 1013 | # |
| 1014 | # Solid angle measure |
| 1015 | # |
| 1016 | |
| 1017 | sphere 4 pi sr |
| 1018 | squaredegree 1|180^2 pi^2 sr |
| 1019 | squareminute 1|60^2 squaredegree |
| 1020 | squaresecond 1|60^2 squareminute |
| 1021 | squarearcmin squareminute |
| 1022 | squarearcsec squaresecond |
| 1023 | sphericalrightangle 1|8 sphere |
| 1024 | octant 1|8 sphere |
| 1025 | |
| 1026 | # |
| 1027 | # Concentration measures |
| 1028 | # |
| 1029 | |
| 1030 | percent 0.01 |
| 1031 | % percent |
| 1032 | mill 0.001 # Originally established by Congress in 1791 |
| 1033 | # as a unit of money equal to 0.001 dollars, |
| 1034 | # it has come to refer to 0.001 in general. |
| 1035 | # Used by some towns to set their property |
| 1036 | # tax rate, and written with a symbol similar |
| 1037 | # to the % symbol but with two 0's in the |
| 1038 | # denominator. [18] |
| 1039 | proof 1|200 # Alcohol content measured by volume at |
| 1040 | # 60 degrees Fahrenheit. This is a USA |
| 1041 | # measure. In Europe proof=percent. |
| 1042 | ppm 1e-6 |
| 1043 | partspermillion ppm |
| 1044 | ppb 1e-9 |
| 1045 | partsperbillion ppb # USA billion |
| 1046 | ppt 1e-12 |
| 1047 | partspertrillion ppt # USA trillion |
| 1048 | karat 1|24 # measure of gold purity |
| 1049 | caratgold karat |
| 1050 | gammil mg/l |
| 1051 | basispoint 0.01 % # Used in finance |
| 1052 | fine 1|1000 # Measure of gold purity |
| 1053 | |
| 1054 | # The pH scale is used to measure the concentration of hydronium (H3O+) ions in |
| 1055 | # a solution. A neutral solution has a pH of 7 as a result of dissociated |
| 1056 | # water molecules. |
| 1057 | |
| 1058 | pH(x) units=[1;mol/liter] range=(0,) 10^(-x) mol/liter ; (-log(pH liters/mol)) |
| 1059 | |
| 1060 | |
| 1061 | # |
| 1062 | # Temperature |
| 1063 | # |
| 1064 | # Two types of units are defined: units for converting temperature differences |
| 1065 | # and functions for converting absolute temperatures. Conversions for |
| 1066 | # differences start with "deg" and conversions for absolute temperature start |
| 1067 | # with "temp". |
| 1068 | # |
| 1069 | # If the temperature inside is 72 degrees Fahrenheit and you want to |
| 1070 | # convert this to degrees Celsius then you need absolute temperature: |
| 1071 | # |
| 1072 | # You have: tempF(72) |
| 1073 | # You want: tempC |
| 1074 | # 22.222222 |
| 1075 | # |
| 1076 | # If the temperature rose 72 degrees Fahrenheit during the chemical reaction |
| 1077 | # then this is a temperature difference: |
| 1078 | # |
| 1079 | # You have: 72 degF |
| 1080 | # You want: degC |
| 1081 | # * 40 |
| 1082 | # / 0.025 |
| 1083 | # |
| 1084 | |
| 1085 | TEMPERATURE kelvin |
| 1086 | TEMPERATURE_DIFFERENCE kelvin |
| 1087 | |
| 1088 | # In 1741 Anders Celsius introduced a temperature scale with water boiling at |
| 1089 | # 0 degrees and freezing at 100 degrees at standard pressure. After his death |
| 1090 | # the fixed points were reversed and the scale was called the centigrade |
| 1091 | # scale. Due to the difficulty of accurately measuring the temperature of |
| 1092 | # melting ice at standard pressure, the centigrade scale was replaced in 1954 |
| 1093 | # by the Celsius scale which is defined by subtracting 273.15 from the |
| 1094 | # temperature in Kelvins. This definition differed slightly from the old |
| 1095 | # centigrade definition, but the Kelvin scale depends on the triple point of |
| 1096 | # water rather than a melting point, so it can be measured accurately. |
| 1097 | |
| 1098 | tempC(x) units=[1;K] domain=[-273.15,) range=[0,) \ |
| 1099 | x K + stdtemp ; (tempC +(-stdtemp))/K |
| 1100 | tempcelsius() tempC |
| 1101 | degcelsius K |
| 1102 | degC K |
| 1103 | |
| 1104 | # Fahrenheit defined his temperature scale by setting 0 to the coldest |
| 1105 | # temperature he could produce in his lab with a salt water solution and by |
| 1106 | # setting 96 degrees to body heat. In Fahrenheit's words: |
| 1107 | # |
| 1108 | # Placing the thermometer in a mixture of sal ammoniac or sea |
| 1109 | # salt, ice, and water a point on the scale will be found which |
| 1110 | # is denoted as zero. A second point is obtained if the same |
| 1111 | # mixture is used without salt. Denote this position as 30. A |
| 1112 | # third point, designated as 96, is obtained if the thermometer |
| 1113 | # is placed in the mouth so as to acquire the heat of a healthy |
| 1114 | # man." (D. G. Fahrenheit, Phil. Trans. (London) 33, 78, 1724) |
| 1115 | |
| 1116 | tempF(x) units=[1;K] domain=[-459.67,) range=[0,) \ |
| 1117 | (x+(-32)) degF + stdtemp ; (tempF+(-stdtemp))/degF + 32 |
| 1118 | tempfahrenheit() tempF |
| 1119 | degfahrenheit 5|9 degC |
| 1120 | degF 5|9 degC |
| 1121 | |
| 1122 | |
| 1123 | degreesrankine degF # The Rankine scale has the |
| 1124 | degrankine degreesrankine # Fahrenheit degree, but its zero |
| 1125 | degreerankine degF # is at absolute zero. |
| 1126 | degR degrankine |
| 1127 | tempR degrankine |
| 1128 | temprankine degrankine |
| 1129 | |
| 1130 | tempreaumur(x) units=[1;K] domain=[-218.52,) range=[0,) \ |
| 1131 | x degreaumur+stdtemp ; (tempreaumur+(-stdtemp))/degreaumur |
| 1132 | degreaumur 10|8 degC # The Reaumur scale was used in Europe and |
| 1133 | # particularly in France. It is defined |
| 1134 | # to be 0 at the freezing point of water |
| 1135 | # and 80 at the boiling point. Reaumur |
| 1136 | # apparently selected 80 because it is |
| 1137 | # divisible by many numbers. |
| 1138 | |
| 1139 | degK K # "Degrees Kelvin" is forbidden usage. |
| 1140 | tempK K # For consistency |
| 1141 | |
| 1142 | # Gas mark is implemented below but in a terribly ugly way. There is |
| 1143 | # a simple formula, but it requires a conditional which is not |
| 1144 | # presently supported. |
| 1145 | # |
| 1146 | # The formula to convert to degrees Fahrenheit is: |
| 1147 | # |
| 1148 | # 25 log2(gasmark) + k_f gasmark<=1 |
| 1149 | # 25 (gasmark-1) + k_f gasmark>=1 |
| 1150 | # |
| 1151 | # k_f = 275 |
| 1152 | # |
| 1153 | gasmark[degR] \ |
| 1154 | .0625 634.67 \ |
| 1155 | .125 659.67 \ |
| 1156 | .25 684.67 \ |
| 1157 | .5 709.67 \ |
| 1158 | 1 734.67 \ |
| 1159 | 2 759.67 \ |
| 1160 | 3 784.67 \ |
| 1161 | 4 809.67 \ |
| 1162 | 5 834.67 \ |
| 1163 | 6 859.67 \ |
| 1164 | 7 884.67 \ |
| 1165 | 8 909.67 \ |
| 1166 | 9 934.67 \ |
| 1167 | 10 959.67 |
| 1168 | |
| 1169 | |
| 1170 | # The Beaufort wind force scale was developed from 1805-1807 by Sir Francis |
| 1171 | # Beaufort to categorize wind conditions at sea. It is normally defined from |
| 1172 | # Beaufort 0, also called "Force 0," through Beaufort 12. Beaufort numbers |
| 1173 | # 13-17 were later defined for tropical cyclones but are rarely used. The |
| 1174 | # original Beaufort scale was qualitative and did not relate directly to wind |
| 1175 | # speed. In 1906, George Simpson of the British Met Office fit wind-speed |
| 1176 | # measurements to visual Beaufort estimates made from five coastal and inland |
| 1177 | # stations in Britain. Simpson's formula was adopted by the World Meterological |
| 1178 | # Organization in 1946 to produce a table, known as WMO Code 1100, giving mean |
| 1179 | # (and min/max) wind speed equivalents at a height of 10 meters for each |
| 1180 | # Beaufort number. This is the "operational" Beaufort scale that mariners |
| 1181 | # use. Meterological and climatic researchers typically use a "scientific" |
| 1182 | # Beaufort scale based on more recent and comprehensive fits. See Wallbrink and |
| 1183 | # Cook, Historical Wind Speed Equivalents Of The Beaufort Scale, 1850-1950, at |
| 1184 | # https://icoads.noaa.gov/reclaim/pdf/Hisklim13.pdf |
| 1185 | # |
| 1186 | beaufort_WMO1100(B) units=[1;m/s] domain=[0,17] range=[0,) \ |
| 1187 | 0.836 B^3|2 m/s; (beaufort_WMO1100 s / 0.836 m)^2|3 |
| 1188 | |
| 1189 | beaufort(B) units=[1;m/s] domain=[0,17] range=[0,) \ |
| 1190 | beaufort_WMO1100(B); ~beaufort_WMO1100(beaufort) |
| 1191 | |
| 1192 | # Units cannot handle wind chill or heat index because they are two-variable |
| 1193 | # functions, but they are included here for your edification. Clearly these |
| 1194 | # equations are the result of a model fitting operation. |
| 1195 | # |
| 1196 | # wind chill index (WCI) a measurement of the combined cooling effect of low |
| 1197 | # air temperature and wind on the human body. The index was first defined |
| 1198 | # by the American Antarctic explorer Paul Siple in 1939. As currently used |
| 1199 | # by U.S. meteorologists, the wind chill index is computed from the |
| 1200 | # temperature T (in deg F) and wind speed V (in mi/hr) using the formula: |
| 1201 | # WCI = 0.0817(3.71 sqrt(V) + 5.81 - 0.25V)(T - 91.4) + 91.4. |
| 1202 | # For very low wind speeds, below 4 mi/hr, the WCI is actually higher than |
| 1203 | # the air temperature, but for higher wind speeds it is lower than the air |
| 1204 | # temperature. |
| 1205 | # |
| 1206 | # heat index (HI or HX) a measure of the combined effect of heat and |
| 1207 | # humidity on the human body. U.S. meteorologists compute the index |
| 1208 | # from the temperature T (in deg F) and the relative humidity H (as a |
| 1209 | # value from 0 to 1). |
| 1210 | # HI = -42.379 + 2.04901523 T + 1014.333127 H - 22.475541 TH |
| 1211 | # - .00683783 T^2 - 548.1717 H^2 + 0.122874 T^2 H + 8.5282 T H^2 |
| 1212 | # - 0.0199 T^2 H^2. |
| 1213 | |
| 1214 | # |
| 1215 | # Physical constants |
| 1216 | # |
| 1217 | |
| 1218 | # Basic constants |
| 1219 | |
| 1220 | pi 3.14159265358979323846 |
| 1221 | tau 2 pi |
| 1222 | phi (sqrt(5)+1)/2 |
| 1223 | light c |
| 1224 | coulombconst alpha hbar c / e^2 # Coulomb constant |
| 1225 | k_C coulombconst # Gets overridden in CGS modes |
| 1226 | k_C_SI alpha hbar_SI c_SI / e_SI^2 |
| 1227 | epsilon0_SI 1 / 4 pi k_C_SI # Vacuum electric permittivity |
| 1228 | epsilon0 1 / 4 pi k_C # Also overridden in CGS modes |
| 1229 | mu0_SI 1 / epsilon0_SI c_SI^2 # Vacuum magnetic permeability |
| 1230 | mu0 1 / epsilon0 c^2 # Also overridden in CGS modes |
| 1231 | Z0 4 pi k_C / c # Free space impedance |
| 1232 | energy c^2 # Convert mass to energy |
| 1233 | hbar h / 2 pi |
| 1234 | hbar_SI h_SI / 2 pi |
| 1235 | spin hbar |
| 1236 | G_SI 6.67430e-11 |
| 1237 | G 6.67430e-11 N m^2 / kg^2 # Newtonian gravitational constant |
| 1238 | |
| 1239 | # Physico-chemical constants |
| 1240 | |
| 1241 | atomicmassunit_SI 1.66053906660e-27 # Unified atomic mass unit, defined as |
| 1242 | atomicmassunit 1.66053906660e-27 kg # Unified atomic mass unit, defined as |
| 1243 | u atomicmassunit # 1|12 of the mass of carbon 12. |
| 1244 | amu atomicmassunit # The relationship N_A u = 1 g/mol |
| 1245 | dalton u # is approximately, but not exactly |
| 1246 | Da dalton # true (with the 2019 SI). |
| 1247 | # Previously the mole was defined to |
| 1248 | # make this relationship exact. |
| 1249 | amu_chem 1.66026e-27 kg # 1|16 of the weighted average mass of |
| 1250 | # the 3 naturally occuring neutral |
| 1251 | # isotopes of oxygen |
| 1252 | amu_phys 1.65981e-27 kg # 1|16 of the mass of a neutral |
| 1253 | # oxygen 16 atom |
| 1254 | gasconstant k N_A # Molar gas constant (exact) |
| 1255 | R gasconstant |
| 1256 | kboltzmann boltzmann |
| 1257 | molarvolume R stdtemp / atm # Volume occupied by one mole of an |
| 1258 | V_m molarvolume # ideal gas at STP. (exact) |
| 1259 | loschmidt avogadro / molarvolume # Molecules per cubic meter of an |
| 1260 | n0 loschmidt # ideal gas at STP. Loschmidt did |
| 1261 | # work similar to Avogadro. |
| 1262 | molarvolume_si N_A siliconlattice^3 / 8 # Volume of a mole of crystalline |
| 1263 | # silicon. The unit cell contains 8 |
| 1264 | # silicon atoms and has a side |
| 1265 | # length of siliconlattice. |
| 1266 | stefanboltzmann pi^2 k^4 / 60 hbar^3 c^2 # The power per area radiated by a |
| 1267 | sigma stefanboltzmann # blackbody at temperature T is |
| 1268 | # given by sigma T^4. (exact) |
| 1269 | wiendisplacement (h c/k)/4.9651142317442763 # Wien's Displacement Law gives |
| 1270 | # the frequency at which the |
| 1271 | # Planck spectrum has maximum |
| 1272 | # intensity. The relation is lambda |
| 1273 | # T = b where lambda is wavelength, |
| 1274 | # T is temperature and b is the Wien |
| 1275 | # displacement. This relation is |
| 1276 | # used to determine the temperature |
| 1277 | # of stars. The constant is the |
| 1278 | # solution to x=5(1-exp(-x)). |
| 1279 | # This expression has no experimental |
| 1280 | # error, and x is defined exactly |
| 1281 | # by the equation above, so it is |
| 1282 | # an exact definition. |
| 1283 | K_J90 483597.9 GHz/V # Direct measurement of the volt is difficult. Until |
| 1284 | K_J 2e/h # recently, laboratories kept Weston cadmium cells as |
| 1285 | # a reference, but they could drift. In 1987 the |
| 1286 | # CGPM officially recommended the use of the |
| 1287 | # Josephson effect as a laboratory representation of |
| 1288 | # the volt. The Josephson effect occurs when two |
| 1289 | # superconductors are separated by a thin insulating |
| 1290 | # layer. A "supercurrent" flows across the insulator |
| 1291 | # with a frequency that depends on the potential |
| 1292 | # applied across the superconductors. This frequency |
| 1293 | # can be very accurately measured. The Josephson |
| 1294 | # constant K_J relates the measured frequency to the |
| 1295 | # potential. Two values given, the conventional |
| 1296 | # (exact) value from 1990, which was used until the |
| 1297 | # 2019 SI revision, and the current exact value. |
| 1298 | R_K90 25812.807 ohm # Measurement of the ohm also presents difficulties. |
| 1299 | R_K h/e^2 # The old approach involved maintaining resistances |
| 1300 | # that were subject to drift. The new standard is |
| 1301 | # based on the Hall effect. When a current carrying |
| 1302 | # ribbon is placed in a magnetic field, a potential |
| 1303 | # difference develops across the ribbon. The ratio |
| 1304 | # of the potential difference to the current is |
| 1305 | # called the Hall resistance. Klaus von Klitzing |
| 1306 | # discovered in 1980 that the Hall resistance varies |
| 1307 | # in discrete jumps when the magnetic field is very |
| 1308 | # large and the temperature very low. This enables |
| 1309 | # accurate realization of the resistance h/e^2 in the |
| 1310 | # lab. The 1990 value was an exact conventional |
| 1311 | # value used until the SI revision in 2019. This value |
| 1312 | # did not agree with measurements. The new value |
| 1313 | # is exact. |
| 1314 | |
| 1315 | # The 2019 update to SI gives exact definitions for R_K and K_J. Previously |
| 1316 | # the electromagnetic units were realized using the 1990 conventional values |
| 1317 | # for these constants, and as a result, the standard definitions were in some |
| 1318 | # sense outside of SI. The revision corrects this problem. The definitions |
| 1319 | # below give the 1990 conventional values for the electromagnetic units in |
| 1320 | # terms of 2019 SI. |
| 1321 | |
| 1322 | ampere90 (K_J90 R_K90 / K_J R_K) A |
| 1323 | coulomb90 (K_J90 R_K90 / K_J R_K) C |
| 1324 | farad90 (R_K90/R_K) F |
| 1325 | henry90 (R_K/R_K90) H |
| 1326 | ohm90 (R_K/R_K90) ohm |
| 1327 | volt90 (K_J90/K_J) V |
| 1328 | watt90 (K_J90^2 R_K90 / K_J^2 R_K) W |
| 1329 | |
| 1330 | # Various conventional values |
| 1331 | |
| 1332 | gravity 9.80665 m/s^2 # std acceleration of gravity (exact) |
| 1333 | # Established by the 3rd CGPM in |
| 1334 | # 1901. This is a nominal midrange |
| 1335 | # value, originally based on the |
| 1336 | # acceleration of a body at sea |
| 1337 | # level at 45 degrees latitude. |
| 1338 | # The value was actually determined |
| 1339 | # by measuring at the International |
| 1340 | # Bureau and correcting the |
| 1341 | # measurement by a theoretical |
| 1342 | # cofficient to get the 45 deg |
| 1343 | # latitude sea level value. |
| 1344 | # (Wikipedia: Standard gravity) |
| 1345 | force gravity # use to turn masses into forces |
| 1346 | atm 101325 Pa # Standard atmospheric pressure |
| 1347 | atmosphere atm |
| 1348 | Hg 13.5951 gram force / cm^3 # Standard weight of mercury (exact) |
| 1349 | water gram force/cm^3 # Standard weight of water (exact) |
| 1350 | waterdensity gram / cm^3 # Density of water |
| 1351 | H2O water |
| 1352 | wc water # water column |
| 1353 | mach 331.46 m/s # speed of sound in dry air at STP |
| 1354 | standardtemp 273.15 K # standard temperature |
| 1355 | stdtemp standardtemp |
| 1356 | normaltemp tempF(70) # for gas density, from NIST |
| 1357 | normtemp normaltemp # Handbook 44 |
| 1358 | |
| 1359 | # Weight of mercury and water at different temperatures using the standard |
| 1360 | # force of gravity. |
| 1361 | |
| 1362 | Hg10C 13.5708 force gram / cm^3 # These units, when used to form |
| 1363 | Hg20C 13.5462 force gram / cm^3 # pressure measures, are not accurate |
| 1364 | Hg23C 13.5386 force gram / cm^3 # because of considerations of the |
| 1365 | Hg30C 13.5217 force gram / cm^3 # revised practical temperature scale. |
| 1366 | Hg40C 13.4973 force gram / cm^3 |
| 1367 | Hg60F 13.5574 force gram / cm^3 |
| 1368 | H2O0C 0.99987 force gram / cm^3 |
| 1369 | H2O5C 0.99999 force gram / cm^3 |
| 1370 | H2O10C 0.99973 force gram / cm^3 |
| 1371 | H2O15C 0.99913 force gram / cm^3 |
| 1372 | H2O18C 0.99862 force gram / cm^3 |
| 1373 | H2O20C 0.99823 force gram / cm^3 |
| 1374 | H2O25C 0.99707 force gram / cm^3 |
| 1375 | H2O50C 0.98807 force gram / cm^3 |
| 1376 | H2O100C 0.95838 force gram / cm^3 |
| 1377 | |
| 1378 | # Atomic constants |
| 1379 | |
| 1380 | hartree 4.3597447222071e-18 J # Approximate electric potential energy |
| 1381 | E_h hartree # of the hydrogen atom in its ground |
| 1382 | # state, and approximately twice its |
| 1383 | # ionization energy. The hartree |
| 1384 | # energy is traditionally defined as |
| 1385 | # coulombconst^2 m_e e^4 / hbar^2, |
| 1386 | # but it can be measured to greater |
| 1387 | # precision using the relationship |
| 1388 | # hartree = 2 h c Rinfinity |
| 1389 | # because Rinfinity is one of the |
| 1390 | # most accurately measured physical |
| 1391 | # constants. Because h and c are |
| 1392 | # exact we can choose either hartree |
| 1393 | # or Rinfinity from CODATA to use as |
| 1394 | # the primary value without |
| 1395 | # affecting the precision. |
| 1396 | Rinfinity hartree / 2 h c # The wavelengths of a spectral series |
| 1397 | R_H Rinfinity m_p / (m_e + m_p) # can be expressed as |
| 1398 | # 1/lambda = R (1/m^2 - 1/n^2). |
| 1399 | # where R is a number that various |
| 1400 | # slightly from element to element. |
| 1401 | # For hydrogen, R_H is the value, |
| 1402 | # and for heavy elements, the value |
| 1403 | # approaches Rinfinity, which can be |
| 1404 | # computed from |
| 1405 | # Rinfinity = m_e c alpha^2 / 2 h |
| 1406 | # with loss of precision. Rinfinity |
| 1407 | # is one of the most accurately |
| 1408 | # measured physical constants and is |
| 1409 | # known to higher precision than m_e |
| 1410 | # or alpha. |
| 1411 | alpha 7.2973525693e-3 # The fine structure constant was |
| 1412 | # introduced to explain fine |
| 1413 | # structure visible in spectral |
| 1414 | # lines. |
| 1415 | bohrradius hbar / alpha m_e c |
| 1416 | a0 bohrradius |
| 1417 | prout 185.5 keV # nuclear binding energy equal to 1|12 |
| 1418 | # binding energy of the deuteron |
| 1419 | conductancequantum e^2 / pi hbar |
| 1420 | G0 conductancequantum |
| 1421 | magneticfluxquantum pi hbar / e |
| 1422 | Phi0 magneticfluxquantum |
| 1423 | |
| 1424 | # Particle radius |
| 1425 | |
| 1426 | electronradius coulombconst e^2 / electronmass c^2 # Classical |
| 1427 | deuteronchargeradius 2.12799e-15 m |
| 1428 | protonchargeradius 0.8751e-15 m |
| 1429 | |
| 1430 | # Masses of elementary particles |
| 1431 | |
| 1432 | electronmass_SI electronmass_u atomicmassunit_SI |
| 1433 | electronmass_u 5.48579909065e-4 |
| 1434 | electronmass 5.48579909065e-4 u |
| 1435 | m_e electronmass |
| 1436 | muonmass 0.1134289259 u |
| 1437 | m_mu muonmass |
| 1438 | taumass 1.90754 u |
| 1439 | m_tau taumass |
| 1440 | protonmass 1.007276466621 u |
| 1441 | m_p protonmass |
| 1442 | neutronmass 1.00866491595 u |
| 1443 | m_n neutronmass |
| 1444 | deuteronmass 2.013553212745 u # Nucleus of deuterium, one |
| 1445 | m_d deuteronmass # proton and one neutron |
| 1446 | alphaparticlemass 4.001506179127 u # Nucleus of He, two protons |
| 1447 | m_alpha alphaparticlemass # and two neutrons |
| 1448 | tritonmass 3.01550071621 u # Nucleus of H3, one proton |
| 1449 | m_t tritonmass # and two neutrons |
| 1450 | helionmass 3.014932247175 u # Nucleus of He3, two protons |
| 1451 | m_h helionmass # and one neutron |
| 1452 | |
| 1453 | # particle wavelengths: the compton wavelength of a particle is |
| 1454 | # defined as h / m c where m is the mass of the particle. |
| 1455 | |
| 1456 | electronwavelength h / m_e c |
| 1457 | lambda_C electronwavelength |
| 1458 | protonwavelength h / m_p c |
| 1459 | lambda_C,p protonwavelength |
| 1460 | neutronwavelength h / m_n c |
| 1461 | lambda_C,n neutronwavelength |
| 1462 | muonwavelength h / m_mu c |
| 1463 | lambda_C,mu muonwavelength |
| 1464 | |
| 1465 | # The g-factor or dimensionless magnetic moment is a quantity that |
| 1466 | # characterizes the magnetic moment of a particle. The electron g-factor is |
| 1467 | # one of the most precisely measured values in physics, with a relative |
| 1468 | # uncertainty of 1.7e-13. |
| 1469 | |
| 1470 | g_d 0.8574382338 # Deuteron g-factor |
| 1471 | g_e -2.00231930436256 # Electron g-factor |
| 1472 | g_h -4.255250615 # Helion g-factor |
| 1473 | g_mu -2.0023318418 # Muon g-factor |
| 1474 | g_n -3.82608545 # Neutron g-factor |
| 1475 | g_p 5.5856946893 # Proton g-factor |
| 1476 | g_t 5.957924931 # Triton g-factor |
| 1477 | |
| 1478 | fermicoupling 1.1663787e-5 / GeV^2 |
| 1479 | |
| 1480 | # Magnetic moments (derived from the more accurate g-factors) |
| 1481 | # |
| 1482 | # The magnetic moment is g * mu_ref * spin where in most cases |
| 1483 | # the reference is the nuclear magneton, and all of the particles |
| 1484 | # except the deuteron have spin 1/2. |
| 1485 | |
| 1486 | bohrmagneton e hbar / 2 electronmass # Reference magnetic moment for |
| 1487 | mu_B bohrmagneton # the electron |
| 1488 | mu_e g_e mu_B / 2 # Electron spin magnet moment |
| 1489 | mu_mu g_mu mu_B m_e / 2 muonmass # Muon spin magnetic moment |
| 1490 | nuclearmagneton mu_B m_e / protonmass # Convenient reference magnetic |
| 1491 | mu_N nuclearmagneton # moment for heavy particles |
| 1492 | mu_p g_p mu_N / 2 # Proton magnetic moment |
| 1493 | mu_n g_n mu_N / 2 # Neutron magnetic moment |
| 1494 | mu_d g_d mu_N # Deuteron magnetic moment, spin 1 |
| 1495 | mu_t g_t mu_N / 2 # Triton magnetic moment |
| 1496 | mu_h g_h mu_N / 2 # Helion magnetic moment |
| 1497 | |
| 1498 | # |
| 1499 | # Units derived from physical constants |
| 1500 | # |
| 1501 | |
| 1502 | kgf kg force |
| 1503 | technicalatmosphere kgf / cm^2 |
| 1504 | at technicalatmosphere |
| 1505 | hyl kgf s^2 / m # Also gram-force s^2/m according to [15] |
| 1506 | mmHg mm Hg |
| 1507 | torr atm / 760 # The torr, named after Evangelista |
| 1508 | # Torricelli, and is very close to the mm Hg |
| 1509 | tor Pa # Suggested in 1913 but seldom used [24]. |
| 1510 | # Eventually renamed the Pascal. Don't |
| 1511 | # confuse the tor with the torr. |
| 1512 | inHg inch Hg |
| 1513 | inH2O inch water |
| 1514 | mmH2O mm water |
| 1515 | eV e V # Energy acquired by a particle with charge e |
| 1516 | electronvolt eV # when it is accelerated through 1 V |
| 1517 | lightyear c julianyear # The 365.25 day year is specified in |
| 1518 | ly lightyear # NIST publication 811 |
| 1519 | lightsecond c s |
| 1520 | lightminute c min |
| 1521 | parsec au / tan(arcsec) # Unit of length equal to distance |
| 1522 | pc parsec # from the Sun to a point having |
| 1523 | # heliocentric parallax of 1 |
| 1524 | # arcsec (derived from parallax |
| 1525 | # second). A distant object with |
| 1526 | # parallax theta will be about |
| 1527 | # (arcsec/theta) parsecs from the |
| 1528 | # Sun (using the approximation |
| 1529 | # that tan(theta) = theta). |
| 1530 | rydberg 1|2 hartree # Rydberg energy |
| 1531 | crith 0.089885 gram # The crith is the mass of one |
| 1532 | # liter of hydrogen at standard |
| 1533 | # temperature and pressure. |
| 1534 | amagat N_A / molarvolume # Used to measure gas as a number |
| 1535 | amagatvolume mol molarvolume # density |
| 1536 | lorentz bohrmagneton / h c # Used to measure the extent |
| 1537 | # that the frequency of light |
| 1538 | # is shifted by a magnetic field. |
| 1539 | cminv h c / cm # Unit of energy used in infrared |
| 1540 | invcm cminv # spectroscopy. |
| 1541 | wavenumber 1/cm # |
| 1542 | kcal_mol kcal_th / mol N_A # kcal/mol is used as a unit of |
| 1543 | # energy by physical chemists. |
| 1544 | # |
| 1545 | # CGS system based on centimeter, gram and second |
| 1546 | # |
| 1547 | |
| 1548 | dyne cm gram / s^2 # force |
| 1549 | dyn dyne |
| 1550 | erg cm dyne # energy |
| 1551 | poise gram / cm s # viscosity, honors Jean Poiseuille |
| 1552 | P poise |
| 1553 | rhe /poise # reciprocal viscosity |
| 1554 | stokes cm^2 / s # kinematic viscosity |
| 1555 | St stokes |
| 1556 | stoke stokes |
| 1557 | lentor stokes # old name |
| 1558 | Gal cm / s^2 # acceleration, used in geophysics |
| 1559 | galileo Gal # for Earth's gravitational field |
| 1560 | # (note that "gal" is for gallon |
| 1561 | # but "Gal" is the standard symbol |
| 1562 | # for the gal which is evidently a |
| 1563 | # shortened form of "galileo".) |
| 1564 | barye dyne/cm^2 # pressure |
| 1565 | barad barye # old name |
| 1566 | kayser 1/cm # Proposed as a unit for wavenumber |
| 1567 | balmer kayser # Even less common name than "kayser" |
| 1568 | kine cm/s # velocity |
| 1569 | bole g cm / s # momentum |
| 1570 | pond gram force |
| 1571 | glug gram force s^2 / cm # Mass which is accelerated at |
| 1572 | # 1 cm/s^2 by 1 gram force |
| 1573 | darcy centipoise cm^2 / s atm # Measures permeability to fluid flow. |
| 1574 | # One darcy is the permeability of a |
| 1575 | # medium that allows a flow of cc/s |
| 1576 | # of a liquid of centipoise viscosity |
| 1577 | # under a pressure gradient of |
| 1578 | # atm/cm. Named for H. Darcy. |
| 1579 | mobileohm cm / dyn s # mobile ohm, measure of mechanical |
| 1580 | # mobility |
| 1581 | mechanicalohm dyn s / cm # mechanical resistance |
| 1582 | acousticalohm dyn s / cm^5 # ratio of the sound pressure of |
| 1583 | # 1 dyn/cm^2 to a source of strength |
| 1584 | # 1 cm^3/s |
| 1585 | ray acousticalohm |
| 1586 | rayl dyn s / cm^3 # Specific acoustical resistance |
| 1587 | eotvos 1e-9 Gal/cm # Change in gravitational acceleration |
| 1588 | # over horizontal distance |
| 1589 | # |
| 1590 | # Electromagnetic CGS Units |
| 1591 | # |
| 1592 | # For measuring electromagnetic quantities in SI, we introduce the new base |
| 1593 | # dimension of current, define the ampere to measure current, and derive the |
| 1594 | # other electromagnetic units from the ampere. With the CGS units one approach |
| 1595 | # is to use the basic equations of electromagnetism to define units that |
| 1596 | # eliminate constants from those equations. Coulomb's law has the form |
| 1597 | # |
| 1598 | # F = k_C q1 q2 / r^2 |
| 1599 | # |
| 1600 | # where k_C is the Coulomb constant equal to 1|4 pi epsilon0 in SI units. |
| 1601 | # Ampere's force law takes the form |
| 1602 | # |
| 1603 | # dF/dl = 2 k_A I1 I2 / r |
| 1604 | # |
| 1605 | # where k_A is the ampere constant. In the CGS system we force either k_C or |
| 1606 | # k_A to 1 which then defines either a unit for charge or a unit for current. |
| 1607 | # The other unit then becomes a derived unit. When k_C is 1 the ESU system |
| 1608 | # results. When k_A is 1 the EMU system results. Note that these parameters |
| 1609 | # are not independent of each other: Maxwell's equations indicate that |
| 1610 | # |
| 1611 | # k_C / k_A = c^2 |
| 1612 | # |
| 1613 | # where c is the speed of light. |
| 1614 | # |
| 1615 | # One more choice is needed to define a complete system. Using Coulomb's law |
| 1616 | # we define the electric field as the force per unit charge |
| 1617 | # |
| 1618 | # E = k_C 1 / r^2. |
| 1619 | # |
| 1620 | # But what about the magnetic field? It is derived from Ampere's law but we |
| 1621 | # have the option of adding a proportionality constant, k_B, that may have |
| 1622 | # dimensions: |
| 1623 | # |
| 1624 | # B = 2 k_A k_B I / r |
| 1625 | # |
| 1626 | # We can choose k_B = 1, which is done in the SI, ESU and EMU systems. But if |
| 1627 | # instead we give k_B units of length/time then the magnetic field has |
| 1628 | # the same units as the electric field. This choice leads to the Gaussian |
| 1629 | # and Heaviside-Lorentz systems. |
| 1630 | # |
| 1631 | # The relations above are used to determine the dimensions, but the units are |
| 1632 | # derived from the base units of CGS, not directly from those formulas. We |
| 1633 | # will use the notation [unit] to refer to the dimension of the unit in |
| 1634 | # brackets. This same process gives rise to the SI units such as the tesla, |
| 1635 | # which is defined by |
| 1636 | # |
| 1637 | # [tesla] = [2 (1/4 pi c^2 epsilon0) amp / m] = [(mu0 / 2) amp / m] |
| 1638 | # |
| 1639 | # which gives kg / A s^2 as expected. |
| 1640 | # |
| 1641 | # References: |
| 1642 | # |
| 1643 | # Classical Electrodynamics by John David Jackson, 3rd edition. |
| 1644 | # Cardarelli, Francois. 1999. Scientific Unit Conversion. 2nd ed. Trans. |
| 1645 | # M.J. Shields. London: Springer-Verlag. ISBN 1-85233-043-0 |
| 1646 | # |
| 1647 | # |
| 1648 | # All of the CGS systems result in electromagnetic units that involve the square |
| 1649 | # roots of the centimeter and gram. This requires a change in the primitive |
| 1650 | # units. |
| 1651 | # |
| 1652 | |
| 1653 | !var UNITS_SYSTEM esu emu gaussian gauss hlu |
| 1654 | sqrt_cm ! |
| 1655 | sqrt_centimeter sqrt_cm |
| 1656 | +m 100 sqrt_cm^2 |
| 1657 | sqrt_g ! |
| 1658 | sqrt_gram sqrt_g |
| 1659 | +kg kilo sqrt_g^2 |
| 1660 | !endvar |
| 1661 | |
| 1662 | # Electrostatic CGS (ESU) |
| 1663 | # |
| 1664 | # This system uses the statcoulomb as the fundamental unit of charge, with |
| 1665 | # derived units that parallel the conventional terminology but use the stat- |
| 1666 | # prefix. The statcoulomb is derived from Coulomb's law based on the dyne |
| 1667 | # |
| 1668 | # dyne = statcoulomb^2 / k_C cm^2. |
| 1669 | # |
| 1670 | # and in the EUS system, k_C=1. The statcoulomb is also called the |
| 1671 | # franklin or esu. |
| 1672 | # |
| 1673 | # The ESU system was specified by a committee report in 1873 and rarely used. |
| 1674 | |
| 1675 | statcoulomb sqrt(dyne cm^2/k_C) # Charge such that two charges |
| 1676 | esu statcoulomb # of 1 statC separated by 1 cm |
| 1677 | statcoul statcoulomb # exert a force of 1 dyne |
| 1678 | statC statcoulomb |
| 1679 | stC statcoulomb |
| 1680 | franklin statcoulomb |
| 1681 | Fr franklin |
| 1682 | |
| 1683 | !var UNITS_SYSTEM esu |
| 1684 | !message CGS-ESU units selected |
| 1685 | !prompt (ESU) |
| 1686 | +coulombconst 1 |
| 1687 | +epsilon0 1 / k_C # SI relation: 1 / 4 pi k_C |
| 1688 | +A 10 c_SI statamp |
| 1689 | !endvar |
| 1690 | |
| 1691 | statampere statcoulomb / s |
| 1692 | statamp statampere |
| 1693 | statA statampere |
| 1694 | stA statampere |
| 1695 | statvolt dyne cm / statamp sec |
| 1696 | statV statvolt |
| 1697 | stV statvolt |
| 1698 | statfarad statamp sec / statvolt |
| 1699 | statF statfarad |
| 1700 | stF statfarad |
| 1701 | cmcapacitance statfarad |
| 1702 | stathenry statvolt sec / statamp |
| 1703 | statH stathenry |
| 1704 | stH stathenry |
| 1705 | statohm statvolt / statamp |
| 1706 | stohm statohm |
| 1707 | statmho /statohm |
| 1708 | stmho statmho |
| 1709 | statweber statvolt sec |
| 1710 | statWb statweber |
| 1711 | stWb statweber |
| 1712 | stattesla statWb/cm^2 # Defined by analogy with SI; rarely |
| 1713 | statT stattesla # if ever used |
| 1714 | stT stattesla |
| 1715 | debye 1e-10 statC angstrom # unit of electrical dipole moment |
| 1716 | helmholtz debye/angstrom^2 # Dipole moment per area |
| 1717 | jar 1000 statfarad # approx capacitance of Leyden jar |
| 1718 | |
| 1719 | # Electromagnetic CGS (EMU) |
| 1720 | # |
| 1721 | # The abampere is the fundamental unit of this system, with the derived units |
| 1722 | # using the ab- prefix. The dimensions of the abampere are defined by assuming |
| 1723 | # that k_A=1, which |
| 1724 | # |
| 1725 | # [dyne / cm] = [2 abampere^2 / cm] |
| 1726 | # |
| 1727 | # where the brackets indicate taking the dimension of the unit in base units |
| 1728 | # and discarding any constant factors. This results in the definition from |
| 1729 | # base CGS units of: |
| 1730 | # |
| 1731 | # abampere = sqrt(dyne). |
| 1732 | # |
| 1733 | # The abampere is also called the biot. The magnetic field unit (the gauss) |
| 1734 | # follows from the assumption that k_B=1, which means |
| 1735 | # |
| 1736 | # B = 2 I / r, |
| 1737 | # |
| 1738 | # and hence the dimensions of the gauss are given by |
| 1739 | # |
| 1740 | # [gauss] = [2 abampere / cm] |
| 1741 | # |
| 1742 | # or rewriting in terms of the base units |
| 1743 | # |
| 1744 | # gauss = abampere / cm. |
| 1745 | # |
| 1746 | # The definition given below is different because it is in a form that |
| 1747 | # gives a valid reduction for SI and ESU and still gives the correct |
| 1748 | # result in EMU. (It can be derived from Faraday's law.) |
| 1749 | # |
| 1750 | # The EMU system was developed by Gauss and Weber and formalized as a system in |
| 1751 | # a committee report by the British Association for the Advancement of Science |
| 1752 | # in 1873. |
| 1753 | |
| 1754 | abampere 10 A # Current which produces a force of |
| 1755 | abamp abampere # 2 dyne/cm between two infinitely |
| 1756 | aA abampere # long wires that are 1 cm apart |
| 1757 | abA abampere |
| 1758 | biot abampere |
| 1759 | Bi biot |
| 1760 | |
| 1761 | !var UNITS_SYSTEM emu |
| 1762 | !message CGS-EMU units selected |
| 1763 | !prompt (EMU) |
| 1764 | +coulombconst c^2 |
| 1765 | +epsilon0 1 / k_C # SI relation: 1 / 4 pi k_C |
| 1766 | +abampere sqrt(dyne) |
| 1767 | +A 0.1 abamp |
| 1768 | !endvar |
| 1769 | |
| 1770 | abcoulomb abamp sec |
| 1771 | abcoul abcoulomb |
| 1772 | abC abcoulomb |
| 1773 | abfarad abampere sec / abvolt |
| 1774 | abF abfarad |
| 1775 | abhenry abvolt sec / abamp |
| 1776 | abH abhenry |
| 1777 | abvolt dyne cm / abamp sec |
| 1778 | abV abvolt |
| 1779 | abohm abvolt / abamp |
| 1780 | abmho /abohm |
| 1781 | maxwell erg / abamp # Also called the "line" |
| 1782 | Mx maxwell |
| 1783 | gauss maxwell / cm^2 # The magnetic field 2 cm from a wire |
| 1784 | Gs gauss # carrying a current of 1 abampere |
| 1785 | oersted gauss / mu0 # From the relation H = B / mu |
| 1786 | Oe oersted |
| 1787 | gilbert gauss cm / mu0 |
| 1788 | Gb gilbert |
| 1789 | Gi gilbert |
| 1790 | unitpole 4 pi maxwell # unit magnetic pole |
| 1791 | emu erg/gauss # "electro-magnetic unit", a measure of |
| 1792 | # magnetic moment, often used as emu/cm^3 |
| 1793 | # to specify magnetic moment density. |
| 1794 | |
| 1795 | # Electromagnetic CGS (Gaussian) |
| 1796 | # |
| 1797 | # The Gaussian system uses the statcoulomb and statamp from the ESU system |
| 1798 | # derived by setting k_C=1, but it defines the magnetic field unit differently |
| 1799 | # by taking k_B=c instead of k_B=1. As noted above, k_C and k_A are not |
| 1800 | # independent. With k_C=1 we must have k_A=c^-2. This results in the magnetic |
| 1801 | # field unit, the gauss, having dimensions give by: |
| 1802 | # |
| 1803 | # [gauss] = [2 (c^-2) c statamp / cm] = [statamp / c cm] |
| 1804 | # |
| 1805 | # We then define the gauss using base CGS units to obtain |
| 1806 | # |
| 1807 | # gauss = statamp / ((cm/s) cm) = statcoulomb / cm^2. |
| 1808 | # |
| 1809 | # Note that this definition happens to give the same result as the definition |
| 1810 | # for the EMU system, so the definitions of the gauss are consistent. |
| 1811 | # |
| 1812 | # This definition gives the same dimensions for the E and B fields and was also |
| 1813 | # known as the "symmetric system". This system was proposed by Hertz in 1888. |
| 1814 | |
| 1815 | !var UNITS_SYSTEM gaussian gauss |
| 1816 | !message CGS-Gaussian units selected |
| 1817 | !prompt (Gaussian) |
| 1818 | !endvar |
| 1819 | !var UNITS_SYSTEM gaussian gauss natural-gauss |
| 1820 | +coulombconst 1 |
| 1821 | +A 10 c_SI statamp |
| 1822 | # Some SI-based definitions need re-scaling |
| 1823 | # by factors of "c" and/or "4 pi": |
| 1824 | +epsilon0 1 / k_C # SI relation: 1 / 4 pi k_C |
| 1825 | +mu0 1 / epsilon0 # SI relation: 1 / epsilon0 c^2 |
| 1826 | +bohrmagneton (e hbar / 2 electronmass) / c |
| 1827 | +magneticfluxquantum c (pi hbar / e) |
| 1828 | +maxwell c (erg / abamp) |
| 1829 | +weber c (J / A) |
| 1830 | !endvar |
| 1831 | |
| 1832 | # Electromagnetic CGS (Heaviside-Lorentz) |
| 1833 | |
| 1834 | # The Heaviside-Lorentz system is similar to the Gaussian system, but it is |
| 1835 | # "rationalized" so that factors of 4 pi do not appear in Maxwell's equations. |
| 1836 | # The SI system is similarly rationalized, but the other CGS systems are not. |
| 1837 | # |
| 1838 | # The factor of 4 pi appears instead in Coulomb's law, so in this system |
| 1839 | # k_C = 1 / 4 pi, which means the charge unit is defined by |
| 1840 | # |
| 1841 | # dyne = (1 / 4 pi) hlu_charge^2 / cm^2. |
| 1842 | # |
| 1843 | # Since we have the leading constant of (1 / 4pi) the numerical value of the |
| 1844 | # charge number is larger by sqrt(4pi), which in turns means that the HLU |
| 1845 | # charge unit is smaller by this multiple. But note that the dimensions of the |
| 1846 | # charge unit are the same as the Gaussian system, so both systems measure |
| 1847 | # charge with cm^(3/2) g^(1/2) / s, but the amount of charge for this dimension |
| 1848 | # differs by a factor of sqrt(4pi) between the two systems. |
| 1849 | # |
| 1850 | # Ampere's law for the Heaviside-Lorentz system has the form |
| 1851 | # |
| 1852 | # B = 1/(2 pi c) * I/r |
| 1853 | |
| 1854 | # The Heaviside-Lorentz system does not appear to have any named units, so we |
| 1855 | # use "hlu" for "Heaviside-Lorentz unit" so we can define values for the basic |
| 1856 | # units in this system. |
| 1857 | |
| 1858 | hlu_charge statcoulomb / sqrt(4 pi) |
| 1859 | hlu_current hlu_charge / sec |
| 1860 | hlu_volt erg / hlu_charge |
| 1861 | hlu_efield hlu_volt / cm |
| 1862 | hlu_bfield sqrt(4 pi) gauss |
| 1863 | |
| 1864 | !var UNITS_SYSTEM hlu |
| 1865 | !message CGS-Heaviside-Lorentz Units selected |
| 1866 | !prompt (HLU) |
| 1867 | !endvar |
| 1868 | !var UNITS_SYSTEM hlu natural planck planck-red |
| 1869 | +coulombconst 1 / 4 pi |
| 1870 | +A 10 c_SI statamp |
| 1871 | # Some SI-based magnetism definitions |
| 1872 | # need re-scaling by factors of "c": |
| 1873 | +mu0 1 / epsilon0 # SI relation: 1 / epsilon0 c^2 |
| 1874 | +bohrmagneton (e hbar / 2 electronmass) / c |
| 1875 | +magneticfluxquantum c (pi hbar / e) |
| 1876 | +weber c (J / A) |
| 1877 | +maxwell c (erg / abamp) |
| 1878 | !endvar |
| 1879 | |
| 1880 | # "Natural units" (high energy physics and cosmology) |
| 1881 | # |
| 1882 | # In particle physics "natural units" (which don't seem to have a more specific |
| 1883 | # name) are defined by setting hbar = c = boltzmann = 1. In this system the |
| 1884 | # electron volt is the only base unit. The electromagnetic units can be |
| 1885 | # derived from the rationalized Heaviside-Lorentz units or from Gaussian units. |
| 1886 | # The default form is the rationalized HLU derived version. |
| 1887 | # |
| 1888 | # The basic mechanical and thermodynamic definitions for the natural |
| 1889 | # units are identical in both systems. These appear below. The |
| 1890 | # natural-gauss system has additional electromagnetic redefinitions |
| 1891 | # that appear above in the "Electromagnetic CGS (Gaussian)" Section. |
| 1892 | |
| 1893 | # These are the Heaviside-Lorentz natural units |
| 1894 | |
| 1895 | natural_energy eV |
| 1896 | natural_charge e / sqrt(4 pi alpha) |
| 1897 | natural_time hbar / natural_energy |
| 1898 | natural_length natural_time c |
| 1899 | natural_mass natural_energy / c^2 |
| 1900 | natural_temp natural_energy / boltzmann |
| 1901 | natural_force natural_energy / natural_length |
| 1902 | natural_power natural_energy / natural_time |
| 1903 | natural_volt natural_energy / natural_charge |
| 1904 | natural_Efield natural_volt / natural_length |
| 1905 | natural_Bfield natural_Efield / c |
| 1906 | natural_current natural_charge / natural_time |
| 1907 | |
| 1908 | !var UNITS_SYSTEM natural |
| 1909 | !message Natural units selected (Heavyside-Lorentz based) |
| 1910 | !prompt (natural) |
| 1911 | !endvar |
| 1912 | |
| 1913 | !var UNITS_SYSTEM natural-gauss |
| 1914 | !message Natural units selected (Gaussian based) |
| 1915 | !prompt (natgauss) |
| 1916 | !endvar |
| 1917 | |
| 1918 | # These definitions are the same in both natural unit systems |
| 1919 | |
| 1920 | !var UNITS_SYSTEM natural natural-gauss |
| 1921 | +eV ! |
| 1922 | +h 2 pi |
| 1923 | +c 1 |
| 1924 | +boltzmann 1 |
| 1925 | +m e_SI / hbar_SI c_SI eV |
| 1926 | +kg (c_SI^2 / e_SI) eV |
| 1927 | +s e_SI / hbar_SI eV |
| 1928 | +K (k_SI / e_SI) eV |
| 1929 | !endvar |
| 1930 | |
| 1931 | # |
| 1932 | # Planck units |
| 1933 | # |
| 1934 | # Planck units are a set of "natural" units based on physical constants c, G, |
| 1935 | # hbar, boltzmann's constant, and epsilon0, often used when working with |
| 1936 | # gravitational theory. In planck units, all quantities are dimensionless. |
| 1937 | # Some variations are possible for exactly how the units are defined. We |
| 1938 | # provide two variations, the rationalized planck units and the |
| 1939 | # rationalized-reduced planck units. |
| 1940 | # |
| 1941 | # In both forms the units are defined by c = hbar = boltzmann = 1. |
| 1942 | # But the choice of rationalized and reduced affects how epsilon0 and G |
| 1943 | # are treated. |
| 1944 | # |
| 1945 | # In the "rationalized" units, factors of 4 pi do not appear in Maxwell's |
| 1946 | # equation, and Coulomb's law bears a factor of 1/4 pi. See the section on |
| 1947 | # the Heaviside-Lorentz units for more about this. The choice of rationalized |
| 1948 | # units means that epsilon0 = 1. (In the unrationalized case, which is not |
| 1949 | # supported, 1/(4 pi epsilon0) = 1.) |
| 1950 | # |
| 1951 | # The "reduced" units similarly are defined to eliminate factors of 8 pi |
| 1952 | # from the Einstein field equations for gravitation. With reduced units |
| 1953 | # we set 8 pi G = 1 and with the unreduced units, simply G = 1. |
| 1954 | |
| 1955 | # Rationalized, unreduced planck units |
| 1956 | |
| 1957 | planckmass sqrt(hbar c / G) |
| 1958 | m_P planckmass |
| 1959 | planckenergy planckmass c^2 |
| 1960 | E_P planckenergy |
| 1961 | plancktime hbar / planckenergy |
| 1962 | t_P plancktime |
| 1963 | plancklength plancktime c |
| 1964 | l_P plancklength |
| 1965 | plancktemperature planckenergy / k |
| 1966 | T_P plancktemperature |
| 1967 | planckforce planckenergy / plancklength |
| 1968 | planckcharge sqrt(epsilon0 hbar c) |
| 1969 | planckcurrent planckcharge / plancktime |
| 1970 | planckvolt planckenergy / planckcharge |
| 1971 | planckEfield planckvolt / plancklength |
| 1972 | planckBfield planckEfield / c |
| 1973 | |
| 1974 | # Rationalized, reduced planck units |
| 1975 | |
| 1976 | planckmass_red sqrt(hbar c / 8 pi G) |
| 1977 | planckenergy_red planckmass_red c^2 |
| 1978 | plancktime_red hbar / planckenergy_red |
| 1979 | plancklength_red plancktime_red c |
| 1980 | plancktemperature_red planckenergy_red / k |
| 1981 | planckforce_red planckenergy_red / plancklength_red |
| 1982 | planckcharge_red sqrt(epsilon0 hbar c) |
| 1983 | planckcurrent_red planckcharge_red / plancktime_red |
| 1984 | planckvolt_red planckenergy_red / planckcharge_red |
| 1985 | planckEfield_red planckvolt_red / plancklength_red |
| 1986 | planckBfield_red planckEfield_red /c |
| 1987 | |
| 1988 | |
| 1989 | !var UNITS_SYSTEM planck |
| 1990 | !message Planck units selected |
| 1991 | !prompt (planck) |
| 1992 | +c 1 |
| 1993 | +h 2 pi |
| 1994 | +G 1 |
| 1995 | +boltzmann 1 |
| 1996 | +kg sqrt(G_SI / hbar_SI c_SI) |
| 1997 | +s c_SI^2 / hbar_SI kg |
| 1998 | +m s / c_SI |
| 1999 | +K k_SI / hbar_SI s |
| 2000 | !endvar |
| 2001 | |
| 2002 | |
| 2003 | !var UNITS_SYSTEM planck-red |
| 2004 | !message Reduced planck units selected |
| 2005 | !prompt (planck reduced) |
| 2006 | +c 1 |
| 2007 | +h 2 pi |
| 2008 | +G 1/8 pi |
| 2009 | +boltzmann 1 |
| 2010 | +kg sqrt(8 pi G_SI / hbar_SI c_SI) |
| 2011 | +s c_SI^2 / hbar_SI kg |
| 2012 | +m s / c_SI |
| 2013 | +K k_SI / hbar_SI s |
| 2014 | !endvar |
| 2015 | |
| 2016 | # |
| 2017 | # Some historical electromagnetic units |
| 2018 | # |
| 2019 | |
| 2020 | intampere 0.999835 A # Defined as the current which in one |
| 2021 | intamp intampere # second deposits .001118 gram of |
| 2022 | # silver from an aqueous solution of |
| 2023 | # silver nitrate. |
| 2024 | intfarad 0.999505 F |
| 2025 | intvolt 1.00033 V |
| 2026 | intohm 1.000495 ohm # Defined as the resistance of a |
| 2027 | # uniform column of mercury containing |
| 2028 | # 14.4521 gram in a column 1.063 m |
| 2029 | # long and maintained at 0 degC. |
| 2030 | daniell 1.042 V # Meant to be electromotive force of a |
| 2031 | # Daniell cell, but in error by .04 V |
| 2032 | faraday N_A e mol # Charge that must flow to deposit or |
| 2033 | faraday_phys 96521.9 C # liberate one gram equivalent of any |
| 2034 | faraday_chem 96495.7 C # element. (The chemical and physical |
| 2035 | faradayconst N_A e # values are off slightly from what is |
| 2036 | # obtained by multiplying by amu_chem |
| 2037 | # or amu_phys. These values are from |
| 2038 | # a 1991 NIST publication.) Note that |
| 2039 | # there is also a Faraday constant, |
| 2040 | # which has units of C/mol. |
| 2041 | kappline 6000 maxwell # Named by and for Gisbert Kapp |
| 2042 | siemensunit 0.9534 ohm # Resistance of a meter long column of |
| 2043 | # mercury with a 1 mm cross section. |
| 2044 | # |
| 2045 | # Printed circuit board units. |
| 2046 | # |
| 2047 | # Iowa State University Center for Nondestructive Evaluation |
| 2048 | # Electrical Conductivity and Resistivity |
| 2049 | # https://www.nde-ed.org/Physics/Materials/Physical_Chemical/Electrical.xhtml |
| 2050 | # |
| 2051 | # Conductivity is often expressed as a percentage of IACS. A copper wire a |
| 2052 | # meter long with a 1 mm^2 cross section has a resistance of 1|58 ohm at |
| 2053 | # 20 deg C. Copper density also has a standard IACS value at that temperature. |
| 2054 | # |
| 2055 | |
| 2056 | copperconductivity 58 siemens m / mm^2 # A wire a meter long with |
| 2057 | IACS copperconductivity # a 1 mm^2 cross section |
| 2058 | copperdensity 8.89 g/cm^3 # The "ounce" measures the |
| 2059 | ouncecopper oz / ft^2 copperdensity # thickness of copper used |
| 2060 | ozcu ouncecopper # in circuitboard fabrication |
| 2061 | |
| 2062 | # |
| 2063 | # Photometric units |
| 2064 | # |
| 2065 | |
| 2066 | LUMINOUS_INTENSITY candela |
| 2067 | LUMINOUS_FLUX lumen |
| 2068 | LUMINOUS_ENERGY talbot |
| 2069 | ILLUMINANCE lux |
| 2070 | EXITANCE lux |
| 2071 | |
| 2072 | candle 1.02 candela # Standard unit for luminous intensity |
| 2073 | hefnerunit 0.9 candle # in use before candela |
| 2074 | hefnercandle hefnerunit # |
| 2075 | violle 20.17 cd # luminous intensity of 1 cm^2 of |
| 2076 | # platinum at its temperature of |
| 2077 | # solidification (2045 K) |
| 2078 | |
| 2079 | lumen cd sr # Luminous flux (luminous energy per |
| 2080 | lm lumen # time unit) |
| 2081 | |
| 2082 | talbot lumen s # Luminous energy |
| 2083 | lumberg talbot # References give these values for |
| 2084 | lumerg talbot # lumerg and lumberg both. Note that |
| 2085 | # a paper from 1948 suggests that |
| 2086 | # lumerg should be 1e-7 talbots so |
| 2087 | # that lumergs/erg = talbots/joule. |
| 2088 | # lumerg = luminous erg |
| 2089 | lux lm/m^2 # Illuminance or exitance (luminous |
| 2090 | lx lux # flux incident on or coming from |
| 2091 | phot lumen / cm^2 # a surface) |
| 2092 | ph phot # |
| 2093 | footcandle lumen/ft^2 # Illuminance from a 1 candela source |
| 2094 | # at a distance of one foot |
| 2095 | metercandle lumen/m^2 # Illuminance from a 1 candela source |
| 2096 | # at a distance of one meter |
| 2097 | |
| 2098 | mcs metercandle s # luminous energy per area, used to |
| 2099 | # measure photographic exposure |
| 2100 | |
| 2101 | nox 1e-3 lux # These two units were proposed for |
| 2102 | skot 1e-3 apostilb # measurements relating to dark adapted |
| 2103 | # eyes. |
| 2104 | # Luminance measures |
| 2105 | |
| 2106 | LUMINANCE nit |
| 2107 | |
| 2108 | nit cd/m^2 # Luminance: the intensity per projected |
| 2109 | stilb cd / cm^2 # area of an extended luminous source. |
| 2110 | sb stilb # (nit is from latin nitere = to shine.) |
| 2111 | |
| 2112 | apostilb cd/pi m^2 |
| 2113 | asb apostilb |
| 2114 | blondel apostilb # Named after a French scientist. |
| 2115 | |
| 2116 | # Equivalent luminance measures. These units are units which measure |
| 2117 | # the luminance of a surface with a specified exitance which obeys |
| 2118 | # Lambert's law. (Lambert's law specifies that luminous intensity of |
| 2119 | # a perfectly diffuse luminous surface is proportional to the cosine |
| 2120 | # of the angle at which you view the luminous surface.) |
| 2121 | |
| 2122 | equivalentlux cd / pi m^2 # luminance of a 1 lux surface |
| 2123 | equivalentphot cd / pi cm^2 # luminance of a 1 phot surface |
| 2124 | lambert cd / pi cm^2 |
| 2125 | footlambert cd / pi ft^2 |
| 2126 | |
| 2127 | # The bril is used to express "brilliance" of a source of light on a |
| 2128 | # logarithmic scale to correspond to subjective perception. An increase of 1 |
| 2129 | # bril means doubling the luminance. A luminance of 1 lambert is defined to |
| 2130 | # have a brilliance of 1 bril. |
| 2131 | |
| 2132 | bril(x) units=[1;lambert] 2^(x+-100) lamberts ;log2(bril/lambert)+100 |
| 2133 | |
| 2134 | # Some luminance data from the IES Lighting Handbook, 8th ed, 1993 |
| 2135 | |
| 2136 | sunlum 1.6e9 cd/m^2 # at zenith |
| 2137 | sunillum 100e3 lux # clear sky |
| 2138 | sunillum_o 10e3 lux # overcast sky |
| 2139 | sunlum_h 6e6 cd/m^2 # value at horizon |
| 2140 | skylum 8000 cd/m^2 # average, clear sky |
| 2141 | skylum_o 2000 cd/m^2 # average, overcast sky |
| 2142 | moonlum 2500 cd/m^2 |
| 2143 | |
| 2144 | # |
| 2145 | # Photographic Exposure Value |
| 2146 | # This section by Jeff Conrad (jeff_conrad@msn.com) |
| 2147 | # |
| 2148 | # The Additive system of Photographic EXposure (APEX) proposed in ASA |
| 2149 | # PH2.5-1960 was an attempt to simplify exposure determination for people who |
| 2150 | # relied on exposure tables rather than exposure meters. Shortly thereafter, |
| 2151 | # nearly all cameras incorporated exposure meters, so the APEX system never |
| 2152 | # caught on, but the concept of exposure value remains in use. Though given as |
| 2153 | # 'Ev' in ASA PH2.5-1960, it is now more commonly indicated by 'EV'. EV is |
| 2154 | # related to exposure parameters by |
| 2155 | # |
| 2156 | # A^2 LS ES |
| 2157 | # 2^EV = --- = -- = -- |
| 2158 | # t K C |
| 2159 | # |
| 2160 | # Where |
| 2161 | # A = Relative aperture (f-number) |
| 2162 | # t = Exposure time in seconds |
| 2163 | # L = Scene luminance in cd/m2 |
| 2164 | # E = Scene illuminance in lux |
| 2165 | # S = Arithmetic ISO speed |
| 2166 | # K = Reflected-light meter calibration constant |
| 2167 | # C = Incident-light meter calibration constant |
| 2168 | # |
| 2169 | # Strictly, an exposure value is a combination of aperture and exposure time, |
| 2170 | # but it's also commonly used to indicate luminance (or illuminance). |
| 2171 | # Conversion to luminance or illuminance units depends on the ISO speed and the |
| 2172 | # meter calibration constant. Common practice is to use an ISO speed of 100. |
| 2173 | # Calibration constants vary among camera and meter manufacturers: Canon, |
| 2174 | # Nikon, and Sekonic use a value of 12.5 for reflected-light meters, while |
| 2175 | # Kenko (formerly Minolta) and Pentax use a value of 14. Kenko and Sekonic use |
| 2176 | # a value of 250 for incident-light meters with flat receptors. |
| 2177 | # |
| 2178 | # The values for in-camera meters apply only averaging, weighted-averaging, or |
| 2179 | # spot metering--the multi-segment metering incorporated in most current |
| 2180 | # cameras uses proprietary algorithms that evaluate many factors related to the |
| 2181 | # luminance distribution of what is being metered; they are not amenable to |
| 2182 | # simple conversions, and are usually not disclosed by the manufacturers. |
| 2183 | |
| 2184 | s100 100 / lx s # ISO 100 speed |
| 2185 | iso100 s100 |
| 2186 | |
| 2187 | # Reflected-light meter calibration constant with ISO 100 speed |
| 2188 | |
| 2189 | k1250 12.5 (cd/m2) / lx s # For Canon, Nikon, and Sekonic |
| 2190 | k1400 14 (cd/m2) / lx s # For Kenko (Minolta) and Pentax |
| 2191 | |
| 2192 | # Incident-light meter calibration constant with ISO 100 film |
| 2193 | |
| 2194 | c250 250 lx / lx s # flat-disc receptor |
| 2195 | |
| 2196 | # Exposure value to scene luminance with ISO 100 imaging media |
| 2197 | |
| 2198 | # For Kenko (Minolta) or Pentax |
| 2199 | #ev100(x) units=[;cd/m^2] range=(0,) 2^x k1400 / s100; log2(ev100 s100/k1400) |
| 2200 | # For Canon, Nikon, or Sekonic |
| 2201 | ev100(x) units=[1;cd/m^2] range=(0,) 2^x k1250 / s100; log2(ev100 s100/k1250) |
| 2202 | EV100() ev100 |
| 2203 | |
| 2204 | # Exposure value to scene illuminance with ISO 100 imaging media |
| 2205 | |
| 2206 | iv100(x) units=[1;lx] range=(0,) 2^x c250 / s100; log2(iv100 s100 / c250) |
| 2207 | |
| 2208 | # Other Photographic Exposure Conversions |
| 2209 | # |
| 2210 | # As part of APEX, ASA PH2.5-1960 proposed several logarithmic quantities |
| 2211 | # related by |
| 2212 | # |
| 2213 | # Ev = Av + Tv = Bv + Sv |
| 2214 | # |
| 2215 | # where |
| 2216 | # Av = log2(A^2) Aperture value |
| 2217 | # Tv = log2(1/t) Time value |
| 2218 | # Sv = log2(N Sx) Speed value |
| 2219 | # Bv = log2(B S / K) Luminance ("brightness") value |
| 2220 | # Iv = log2(I S / C) Illuminance value |
| 2221 | # |
| 2222 | # and |
| 2223 | # A = Relative aperture (f-number) |
| 2224 | # t = Exposure time in seconds |
| 2225 | # Sx = Arithmetic ISO speed in 1/lux s |
| 2226 | # B = luminance in cd/m2 |
| 2227 | # I = luminance in lux |
| 2228 | |
| 2229 | # The constant N derives from the arcane relationship between arithmetic |
| 2230 | # and logarithmic speed given in ASA PH2.5-1960. That relationship |
| 2231 | # apparently was not obvious--so much so that it was thought necessary |
| 2232 | # to explain it in PH2.12-1961. The constant has had several values |
| 2233 | # over the years, usually without explanation for the changes. Although |
| 2234 | # APEX had little impact on consumer cameras, it has seen a partial |
| 2235 | # resurrection in the Exif standards published by the Camera & Imaging |
| 2236 | # Products Association of Japan. |
| 2237 | |
| 2238 | #N_apex 2^-1.75 lx s # precise value implied in ASA PH2.12-1961, |
| 2239 | # derived from ASA PH2.5-1960. |
| 2240 | #N_apex 0.30 lx s # rounded value in ASA PH2.5-1960, |
| 2241 | # ASA PH2.12-1961, and ANSI PH2.7-1986 |
| 2242 | #N_apex 0.3162 lx s # value in ANSI PH2.7-1973 |
| 2243 | N_exif 1|3.125 lx s # value in Exif 2.3 (2010), making Sv(5) = 100 |
| 2244 | K_apex1961 11.4 (cd/m2) / lx s # value in ASA PH2.12-1961 |
| 2245 | K_apex1971 12.5 (cd/m2) / lx s # value in ANSI PH3.49-1971; more common |
| 2246 | C_apex1961 224 lx / lx s # value in PH2.12-1961 (20.83 for I in |
| 2247 | # footcandles; flat sensor?) |
| 2248 | C_apex1971 322 lx / lx s # mean value in PH3.49-1971 (30 +/- 5 for I in |
| 2249 | # footcandles; hemispherical sensor?) |
| 2250 | N_speed N_exif |
| 2251 | K_lum K_apex1971 |
| 2252 | C_illum C_apex1961 |
| 2253 | |
| 2254 | # Units for Photographic Exposure Variables |
| 2255 | # |
| 2256 | # Practical photography sometimes pays scant attention to units for exposure |
| 2257 | # variables. In particular, the "speed" of the imaging medium is treated as if |
| 2258 | # it were dimensionless when it should have units of reciprocal lux seconds; |
| 2259 | # this practice works only because "speed" is almost invariably given in |
| 2260 | # accordance with international standards (or similar ones used by camera |
| 2261 | # manufacturers)--so the assumed units are invariant. In calculating |
| 2262 | # logarithmic quantities--especially the time value Tv and the exposure value |
| 2263 | # EV--the units for exposure time ("shutter speed") are often ignored; this |
| 2264 | # practice works only because the units of exposure time are assumed to be in |
| 2265 | # seconds, and the missing units that make the argument to the logarithmic |
| 2266 | # function dimensionless are silently provided. |
| 2267 | # |
| 2268 | # In keeping with common practice, the definitions that follow treat "speeds" |
| 2269 | # as dimensionless, so ISO 100 speed is given simply as '100'. When |
| 2270 | # calculating the logarithmic APEX quantities Av and Tv, the definitions |
| 2271 | # provide the missing units, so the times can be given with any appropriate |
| 2272 | # units. For example, giving an exposure time of 1 minute as either '1 min' or |
| 2273 | # '60 s' will result in Tv of -5.9068906. |
| 2274 | # |
| 2275 | # Exposure Value from f-number and Exposure Time |
| 2276 | # |
| 2277 | # Because nonlinear unit conversions only accept a single quantity, |
| 2278 | # there is no direct conversion from f-number and exposure time to |
| 2279 | # exposure value EV. But the EV can be obtained from a combination of |
| 2280 | # Av and Tv. For example, the "sunny 16" rule states that correct |
| 2281 | # exposure for a sunlit scene can achieved by using f/16 and an exposure |
| 2282 | # time equal to the reciprocal of the ISO speed in seconds; this can be |
| 2283 | # calculated as |
| 2284 | # |
| 2285 | # ~Av(16) + ~Tv(1|100 s), |
| 2286 | # |
| 2287 | # which gives 14.643856. These conversions may be combined with the |
| 2288 | # ev100 conversion: |
| 2289 | # |
| 2290 | # ev100(~Av(16) + ~Tv(1|100 s)) |
| 2291 | # |
| 2292 | # to yield the assumed average scene luminance of 3200 cd/m^2. |
| 2293 | |
| 2294 | # convert relative aperture (f-number) to aperture value |
| 2295 | Av(A) units=[1;1] domain=[-2,) range=[0.5,) 2^(A/2); 2 log2(Av) |
| 2296 | # convert exposure time to time value |
| 2297 | Tv(t) units=[1;s] range=(0,) 2^(-t) s; log2(s / Tv) |
| 2298 | # convert logarithmic speed Sv in ASA PH2.5-1960 to ASA/ISO arithmetic speed; |
| 2299 | # make arithmetic speed dimensionless |
| 2300 | # 'Sv' conflicts with the symbol for sievert; you can uncomment this function |
| 2301 | # definition if you don't need that symbol |
| 2302 | #Sv(S) units=[1;1] range=(0,) 2^S / (N_speed/lx s); log2((N_speed/lx s) Sv) |
| 2303 | Sval(S) units=[1;1] range=(0,) 2^S / (N_speed/lx s); log2((N_speed/lx s) Sval) |
| 2304 | |
| 2305 | # convert luminance value Bv in ASA PH2.12-1961 to luminance |
| 2306 | Bv(x) units=[1;cd/m^2] range=(0,) \ |
| 2307 | 2^x K_lum N_speed ; log2(Bv / (K_lum N_speed)) |
| 2308 | |
| 2309 | # convert illuminance value Iv in ASA PH2.12-1961 to illuminance |
| 2310 | Iv(x) units=[1;lx] range=(0,) \ |
| 2311 | 2^x C_illum N_speed ; log2(Iv / (C_illum N_speed)) |
| 2312 | |
| 2313 | # convert ASA/ISO arithmetic speed Sx to ASA logarithmic speed in |
| 2314 | # ASA PH2.5-1960; make arithmetic speed dimensionless |
| 2315 | Sx(S) units=[1;1] domain=(0,) \ |
| 2316 | log2((N_speed/lx s) S); 2^Sx / (N_speed/lx s) |
| 2317 | |
| 2318 | # convert DIN speed/ISO logarithmic speed in ISO 6:1993 to arithmetic speed |
| 2319 | # for convenience, speed is treated here as if it were dimensionless |
| 2320 | Sdeg(S) units=[1;1] range=(0,) 10^((S - 1) / 10) ; (1 + 10 log(Sdeg)) |
| 2321 | Sdin() Sdeg |
| 2322 | |
| 2323 | # Numerical Aperture and f-Number of a Lens |
| 2324 | # |
| 2325 | # The numerical aperture (NA) is given by |
| 2326 | # |
| 2327 | # NA = n sin(theta) |
| 2328 | # |
| 2329 | # where n is the index of refraction of the medium and theta is half |
| 2330 | # of the angle subtended by the aperture stop from a point in the image |
| 2331 | # or object plane. For a lens in air, n = 1, and |
| 2332 | # |
| 2333 | # NA = 0.5 / f-number |
| 2334 | # |
| 2335 | # convert NA to f-number |
| 2336 | numericalaperture(x) units=[1;1] domain=(0,1] range=[0.5,) \ |
| 2337 | 0.5 / x ; 0.5 / numericalaperture |
| 2338 | NA() numericalaperture |
| 2339 | # |
| 2340 | # convert f-number to itself; restrict values to those possible |
| 2341 | fnumber(x) units=[1;1] domain=[0.5,) range=[0.5,) x ; fnumber |
| 2342 | |
| 2343 | # Referenced Photographic Standards |
| 2344 | # |
| 2345 | # ASA PH-2.5-1960. USA Standard, Method for Determining (Monochrome, |
| 2346 | # Continuous-Tone) Speed of Photographic Negative Materials. |
| 2347 | # ASA PH2.12-1961. American Standard, General-Purpose Photographic |
| 2348 | # Exposure Meters (photoelectric type). |
| 2349 | # ANSI PH3.49-1971. American National Standard for general-purpose |
| 2350 | # photographic exposure meters (photoelectric type). |
| 2351 | # ANSI PH2.7-1973. American National Standard Photographic Exposure Guide. |
| 2352 | # ANSI PH2.7-1986. American National Standard for Photography -- |
| 2353 | # Photographic Exposure Guide. |
| 2354 | # CIPA DC-008-2010. Exchangeable image file format for digital still |
| 2355 | # cameras: Exif Version 2.3 |
| 2356 | # ISO 6:1993. International Standard, Photography -- Black-and-white |
| 2357 | # pictorial still camera negative film/process systems -- |
| 2358 | # Determination of ISO Speed. |
| 2359 | |
| 2360 | |
| 2361 | # |
| 2362 | # Astronomical time measurements |
| 2363 | # |
| 2364 | # Astronomical time measurement is a complicated matter. The length of the |
| 2365 | # true day at a given place can be 21 seconds less than 24 hours or 30 seconds |
| 2366 | # over 24 hours. The two main reasons for this are the varying speed of |
| 2367 | # Earth in its elliptical orbit and the fact that the Sun moves on the ecliptic |
| 2368 | # instead of along the celestial equator. To devise a workable system for time |
| 2369 | # measurement, Simon Newcomb (1835-1909) used a fictitious "mean Sun". |
| 2370 | # Consider a first fictitious Sun traveling along the ecliptic at a constant |
| 2371 | # speed and coinciding with the true Sun at perigee and apogee. Then |
| 2372 | # considering a second fictitious Sun traveling along the celestial equator at |
| 2373 | # a constant speed and coinciding with the first fictitious Sun at the |
| 2374 | # equinoxes. The second fictitious Sun is the "mean Sun". From this equations |
| 2375 | # can be written out to determine the length of the mean day, and the tropical |
| 2376 | # year. The length of the second was determined based on the tropical year |
| 2377 | # from such a calculation and was officially used from 1960-1967 until atomic |
| 2378 | # clocks replaced astronomical measurements for a standard of time. All of the |
| 2379 | # values below give the mean time for the specified interval. |
| 2380 | # |
| 2381 | # See "Mathematical Astronomy Morsels" by Jean Meeus for more details |
| 2382 | # and a description of how to compute the correction to mean time. |
| 2383 | # |
| 2384 | |
| 2385 | TIME second |
| 2386 | |
| 2387 | anomalisticyear 365.2596 days # The time between successive |
| 2388 | # perihelion passages of |
| 2389 | # Earth. |
| 2390 | siderealyear 365.256360417 day # The time for Earth to make |
| 2391 | # one revolution around the Sun |
| 2392 | # relative to the stars. |
| 2393 | tropicalyear 365.242198781 day # The time needed for the mean Sun |
| 2394 | # as defined above to increase |
| 2395 | # its longitude by 360 degrees. |
| 2396 | # Most references defined the |
| 2397 | # tropical year as the interval |
| 2398 | # between vernal equinoxes, but |
| 2399 | # this is misleading. The length |
| 2400 | # of the season changes over time |
| 2401 | # because of the eccentricity of |
| 2402 | # Earth's orbit. The time |
| 2403 | # between vernal equinoxes is |
| 2404 | # approximately 365.24237 days |
| 2405 | # around the year 2000. See |
| 2406 | # "Mathematical Astronomy |
| 2407 | # Morsels" for more details. |
| 2408 | eclipseyear 346.62 days # The line of nodes is the |
| 2409 | # intersection of the plane of |
| 2410 | # Earth's orbit around the Sun |
| 2411 | # with the plane of the Moon's |
| 2412 | # orbit around Earth. Eclipses |
| 2413 | # can only occur when the Moon |
| 2414 | # and Sun are close to this |
| 2415 | # line. The line rotates and |
| 2416 | # appearances of the Sun on the |
| 2417 | # line of nodes occur every |
| 2418 | # eclipse year. |
| 2419 | saros 223 synodicmonth # The Earth, Moon and Sun appear in |
| 2420 | # the same arrangement every |
| 2421 | # saros, so if an eclipse occurs, |
| 2422 | # then one saros later, a similar |
| 2423 | # eclipse will occur. (The saros |
| 2424 | # is close to 19 eclipse years.) |
| 2425 | # The eclipse will occur about |
| 2426 | # 120 degrees west of the |
| 2427 | # preceding one because the |
| 2428 | # saros is not an even number of |
| 2429 | # days. After 3 saros, an |
| 2430 | # eclipse will occur at |
| 2431 | # approximately the same place. |
| 2432 | solarday day # Time from noon to noon |
| 2433 | siderealday 86164.09054 s # The sidereal day is the interval |
| 2434 | siderealhour 1|24 siderealday # between two successive transits |
| 2435 | siderealminute 1|60 siderealhour # of a star over the meridian, |
| 2436 | siderealsecond 1|60 siderealminute # or the time required for |
| 2437 | # Earth to make one rotation |
| 2438 | # relative to the stars. Another |
| 2439 | # way to think about it is to |
| 2440 | # imagine looking down at the |
| 2441 | # solar system and noting when |
| 2442 | # Earth has made a rotation. |
| 2443 | # The more usual solar day is the |
| 2444 | # time required to make a |
| 2445 | # rotation relative to the Sun, |
| 2446 | # which means the same point on |
| 2447 | # Earth faces the Sun again. |
| 2448 | # Because Earth moves in its |
| 2449 | # orbit, it has to rotate a bit |
| 2450 | # more to face the Sun again, |
| 2451 | # hence the solar day is slightly |
| 2452 | # longer than the sidereal day. |
| 2453 | # The value given here is the |
| 2454 | # mean day length taken from |
| 2455 | # ssd.jpl.nasa.gov/astro_par.html |
| 2456 | # which in turn cites the |
| 2457 | # "Explanatory Supplement to the |
| 2458 | # Astronomical Almanac", 1992. |
| 2459 | anomalisticmonth 27.55454977 day # Time for the Moon to travel from |
| 2460 | # perigee to perigee |
| 2461 | nodicalmonth 27.2122199 day # The nodes are the points where |
| 2462 | draconicmonth nodicalmonth # an orbit crosses the ecliptic. |
| 2463 | draconiticmonth nodicalmonth # This is the time required to |
| 2464 | # travel from the ascending node |
| 2465 | # to the next ascending node. |
| 2466 | siderealmonth 27.321661 day # Time required for the Moon to |
| 2467 | # orbit the Earth |
| 2468 | lunarmonth 29 days + 12 hours + 44 minutes + 2.8 seconds |
| 2469 | # Mean time between full moons. |
| 2470 | synodicmonth lunarmonth # Full moons occur when the Sun |
| 2471 | lunation synodicmonth # and Moon are on opposite sides |
| 2472 | lune 1|30 lunation # of the Earth. Since the Earth |
| 2473 | lunour 1|24 lune # moves around the Sun, the Moon |
| 2474 | # has to move a bit further in its |
| 2475 | # orbit to return to the full moon |
| 2476 | # configuration. |
| 2477 | year tropicalyear |
| 2478 | yr year |
| 2479 | month 1|12 year |
| 2480 | mo month |
| 2481 | lustrum 5 years # The Lustrum was a Roman |
| 2482 | # purification ceremony that took |
| 2483 | # place every five years. |
| 2484 | # Classically educated Englishmen |
| 2485 | # used this term. |
| 2486 | decade 10 years |
| 2487 | century 100 years |
| 2488 | millennium 1000 years |
| 2489 | millennia millennium |
| 2490 | solaryear year |
| 2491 | lunaryear 12 lunarmonth |
| 2492 | calendaryear 365 day |
| 2493 | commonyear 365 day |
| 2494 | leapyear 366 day |
| 2495 | |
| 2496 | # The Julian year is The length of an average year over a 4-year cycle in the |
| 2497 | # Julian calendar. The calendar was proposed by Julius Caesar in 46 BCE and |
| 2498 | # took effect the following year. It has a normal year of 365 days and a leap |
| 2499 | # year of 366 days every four years. Though this calendar was used in |
| 2500 | # Europe for more than 1600 years, it drifts from the topical year by |
| 2501 | # about 1 day every 128 years, which became noticeable over its period |
| 2502 | # of use. |
| 2503 | |
| 2504 | # This growing discrepancy between the seasons and the calendar was perhaps |
| 2505 | # confusing but was also of concern to the Catholic Church because it led to a |
| 2506 | # shift in the date of Easter. To correct this discrepancy, Pope Gregory XIII |
| 2507 | # introduced the more accurate Gregorian calendar in 1582. The Gregorian year |
| 2508 | # is the length of an average year over a 400-year cycle in the Gregorian |
| 2509 | # calendar. Every year that is exactly divisible by four is a |
| 2510 | # leap year, except for years that are exactly divisible by 100, unless these |
| 2511 | # centurial years are exactly divisible by 400. This calendar was adopted by |
| 2512 | # many Catholic countries when it was proclaimed, but was not adopted by many |
| 2513 | # other countries until much later; Britain and the British Empire, including |
| 2514 | # what is now the eastern part of the United States, adopted it in 1752. See |
| 2515 | # https://en.wikipedia.org/wiki/List_of_adoption_dates_of_the_Gregorian_calendar_by_country |
| 2516 | # for additional details. |
| 2517 | |
| 2518 | julianyear 365.25 days |
| 2519 | gregorianyear 365.2425 days |
| 2520 | |
| 2521 | islamicyear 354 day # A year of 12 lunar months. They |
| 2522 | islamicleapyear 355 day # began counting on July 16, AD 622 |
| 2523 | # when Muhammad emigrated to Medina |
| 2524 | # (the year of the Hegira). They need |
| 2525 | # 11 leap days in 30 years to stay in |
| 2526 | # sync with the lunar year which is a |
| 2527 | # bit longer than the 29.5 days of the |
| 2528 | # average month. The months do not |
| 2529 | # keep to the same seasons, but |
| 2530 | # regress through the seasons every |
| 2531 | # 32.5 years. |
| 2532 | islamicmonth 1|12 islamicyear # They have 29 day and 30 day months. |
| 2533 | |
| 2534 | # The Hebrew year is also based on lunar months, but synchronized to the solar |
| 2535 | # calendar. The months vary irregularly between 29 and 30 days in length, and |
| 2536 | # the years likewise vary. The regular year is 353, 354, or 355 days long. To |
| 2537 | # keep up with the solar calendar, a leap month of 30 days is inserted every |
| 2538 | # 3rd, 6th, 8th, 11th, 14th, 17th, and 19th years of a 19 year cycle. This |
| 2539 | # gives leap years that last 383, 384, or 385 days. |
| 2540 | |
| 2541 | # |
| 2542 | # Planetary data from JPL's planet fact sheets. Each planet has its |
| 2543 | # own sheet at https://nssdc.gsfc.nasa.gov/planetary/factsheet/<name>fact.html |
| 2544 | # The source for data on the fact sheets is described at |
| 2545 | # https://nssdc.gsfc.nasa.gov/planetary/factsheet/fact_notes.html |
| 2546 | # and they also indicate that the values listed are not "official" values: |
| 2547 | # there is no single set of agreed upon values. |
| 2548 | |
| 2549 | # Sidereal days. The sidereal day is the time required for a planet to make a |
| 2550 | # revolution relative to the stars. This is the default day value. |
| 2551 | |
| 2552 | mercuryday mercuryday_sidereal |
| 2553 | venusday venusday_sidereal |
| 2554 | earthday earthday_sidereal |
| 2555 | marsday marsday_sidereal |
| 2556 | jupiterday jupiterday_sidereal |
| 2557 | saturnday saturnday_sidereal |
| 2558 | uranusday uranusday_sidereal |
| 2559 | neptuneday neptuneday_sidereal |
| 2560 | plutoday plutoday_sidereal |
| 2561 | |
| 2562 | mercuryday_sidereal 1407.6 hr # Mercury is in a 3:2 resonance lock |
| 2563 | # where it makes 3 rotations per 2 orbits |
| 2564 | # so 3 sidereal days = 2 years |
| 2565 | venusday_sidereal 5832.6 hr # Retrograde |
| 2566 | earthday_sidereal siderealday |
| 2567 | marsday_sidereal 24.6229 hr |
| 2568 | jupiterday_sidereal 9.9250 hr |
| 2569 | saturnday_sidereal 10.656 hr |
| 2570 | uranusday_sidereal 17.24 hr # Retrograde |
| 2571 | neptuneday_sidereal 16.11 hr |
| 2572 | plutoday_sidereal 153.2928 hr # Retrograde |
| 2573 | |
| 2574 | # In astronomy, an object's rotation is "prograde" if it rotates in |
| 2575 | # the same direction as the primary object it orbits. Prograde |
| 2576 | # rotation is the more common case: in Earth's solar system, Mercury, |
| 2577 | # Earth, Mars, Jupiter, Saturn, and Neptune have prograde rotation. |
| 2578 | # When an object rotates opposite the direction of its primary object, |
| 2579 | # the object's rotation is "retrograde". Venus, Uranus, and Pluto have |
| 2580 | # retrograde rotation. |
| 2581 | # |
| 2582 | # The solar (or synodic) day is the time from noon to noon on a planet. This |
| 2583 | # is different from the sidereal day because the planet has moved in its orbit, |
| 2584 | # so (if its rotation is prograde) it needs additional rotation to return to |
| 2585 | # the same orientation relative to the Sun. In one orbital period (a year), |
| 2586 | # this amounts to one additional complete rotation, so the number of sidereal |
| 2587 | # days in a year is one greater than the number of solar days. |
| 2588 | # |
| 2589 | # If the planet's rotation is retrograde, less rotation is needed to return to |
| 2590 | # the same orientation relative to the Sun, and the number of sidereal days in |
| 2591 | # a year is one fewer than the number of solar days. |
| 2592 | # |
| 2593 | # The solar day can be computed from the sidereal day in the typical prograde |
| 2594 | # case by: |
| 2595 | # solar_day = sidereal_day year / (year - sidereal_day) |
| 2596 | # If the planet's rotation is retrograde like Venus then the formula is |
| 2597 | # solar_day = sidereal_day year / (year + sidereal_day) |
| 2598 | # If the sidereal day and year are the same length then the same face of the |
| 2599 | # planet faces the Sun and there is no solar day. |
| 2600 | |
| 2601 | mercuryday_solar 4222.6 hr |
| 2602 | venusday_solar 2802.0 hr |
| 2603 | earthday_solar 24 hr |
| 2604 | marsday_solar 24.6597 hr |
| 2605 | jupiterday_solar 9.9259 hr |
| 2606 | saturnday_solar 10.656 hr |
| 2607 | uranusday_solar 17.24 hr |
| 2608 | neptuneday_solar 16.11 hr |
| 2609 | plutoday_solar 153.2820 hr |
| 2610 | |
| 2611 | # Sidereal years |
| 2612 | |
| 2613 | mercuryyear 87.969 day |
| 2614 | venusyear 224.701 day |
| 2615 | earthyear siderealyear |
| 2616 | marsyear 686.980 day |
| 2617 | jupiteryear 4332.589 day |
| 2618 | saturnyear 10759.22 day |
| 2619 | uranusyear 30685.4 day |
| 2620 | neptuneyear 60189 day |
| 2621 | plutoyear 90560 day |
| 2622 | |
| 2623 | # Equatorial radii for the planets from JPL fact sheets |
| 2624 | |
| 2625 | mercuryradius 2440.5 km |
| 2626 | venusradius 6051.8 km |
| 2627 | earthradius 6378.137 km |
| 2628 | marsradius 3396.2 km |
| 2629 | jupiterradius 71492 km # 1 bar level |
| 2630 | saturnradius 60268 km # 1 bar level |
| 2631 | uranusradius 25559 km # 1 bar level |
| 2632 | neptuneradius 24764 km # 1 bar level |
| 2633 | plutoradius 1188 km |
| 2634 | |
| 2635 | # Volumetric mean radii |
| 2636 | |
| 2637 | mercuryradius_mean 2440.5 km |
| 2638 | venusradius_mean 6051.8 km |
| 2639 | earthradius_mean 6371 km |
| 2640 | marsradius_mean 3389.5 km |
| 2641 | jupiterradius_mean 69911 km |
| 2642 | saturnradius_mean 58232 km |
| 2643 | uranusradius_mean 25362 km |
| 2644 | neptuneradius_mean 24622 km |
| 2645 | plutoradius_mean 1188 km |
| 2646 | |
| 2647 | # Polar radii |
| 2648 | |
| 2649 | mercuryradius_polar 2438.3 km |
| 2650 | venusradius_polar 6051.8 km |
| 2651 | marsradius_polar 3376.2 km |
| 2652 | jupiterradius_polar 66854 km |
| 2653 | saturnradius_polar 54364 km |
| 2654 | uranusradius_polar 24973 km |
| 2655 | neptuneradius_polar 24341 km |
| 2656 | plutoradius_polar 1188 km |
| 2657 | |
| 2658 | mercurysundist_min 46.000 Gm |
| 2659 | mercurysundist_max 69.818 Gm |
| 2660 | venussundist_min 107.480 Gm |
| 2661 | venussundist_max 108.941 Gm |
| 2662 | earthsundist_min sundist_min |
| 2663 | earthsundist_max sundist_max |
| 2664 | marssundist_min 206.650 Gm |
| 2665 | marssundist_max 249.261 Gm |
| 2666 | jupitersundist_min 740.595 Gm |
| 2667 | jupitersundist_max 816.363 Gm |
| 2668 | saturnsundist_min 1357.554 Gm |
| 2669 | saturnsundist_max 1506.527 Gm |
| 2670 | uranussundist_min 2732.696 Gm |
| 2671 | uranussundist_max 3001.390 Gm |
| 2672 | neptunesundist_min 4471.050 Gm |
| 2673 | neptunesundist_max 4558.857 Gm |
| 2674 | plutosundist_min 4434.987 Gm |
| 2675 | plutosundist_max 7304.326 Gm |
| 2676 | |
| 2677 | sundist 1.0000010178 au # mean Earth-Sun distance |
| 2678 | moondist 384400 km # mean Earth-Moon distance |
| 2679 | sundist_near 147.095 Gm # Earth-Sun distance at perihelion |
| 2680 | sundist_min sundist_near |
| 2681 | sundist_far 152.100 Gm # Earth-Sun distance at aphelion |
| 2682 | sundist_max sundist_far |
| 2683 | |
| 2684 | # The Earth-Moon distances at perigee and apogee are different for every |
| 2685 | # lunation. The values here are the extremes for 1500-2500 according to |
| 2686 | # Jean Meeus's Astronomical Algorithms (1991, 332). |
| 2687 | |
| 2688 | moondist_min 356371 km # minimum distance at perigee 1500-2500 |
| 2689 | moondist_max 406720 km # maximum distance at apogee 1500-2500 |
| 2690 | |
| 2691 | # Objects on Earth are charted relative to a perfect ellipsoid whose |
| 2692 | # dimensions are specified by different organizations. The ellipsoid is |
| 2693 | # specified by an equatorial radius and a flattening value which defines the |
| 2694 | # polar radius. |
| 2695 | |
| 2696 | earthflattening IERS_earthflattening |
| 2697 | earthradius_equatorial IERS_earthradius_equatorial |
| 2698 | earthradius_polar (1-earthflattening) earthradius_equatorial |
| 2699 | |
| 2700 | # The World Geodetic System maintains a standard, WGS84, which is used by the |
| 2701 | # the GPS system. This system uses a conventional ellipsoid that was fixed in |
| 2702 | # 1984 and has remained constant so that data collected at different times is |
| 2703 | # referenced to the same ellipsoid. https://epsg.io/4326 |
| 2704 | |
| 2705 | WGS84_earthflattening 1|298.257223563 |
| 2706 | WGS84_earthradius_equatorial 6378137 m |
| 2707 | WGS84_earthradius_polar (1-WGS84_earthflattening) WGS84_earthradius_equatorial |
| 2708 | |
| 2709 | # The International Earth Rotation Service (IERS) attempts to |
| 2710 | # maintain an accurate model of Earth, with updates to maintain the highest |
| 2711 | # possible accuracy, even though this makes it more difficult to relate geodetic |
| 2712 | # measurements made at different times. |
| 2713 | # IERS Conventions, Chapter 1, General definitions and numerical standards (16 November 2017) |
| 2714 | # https://iers-conventions.obspm.fr/content/chapter1/icc1.pdf |
| 2715 | |
| 2716 | IERS_earthflattening 1|298.25642 |
| 2717 | IERS_earthradius_equatorial 6378136.6 m |
| 2718 | IERS_earthradius_polar (1-IERS_earthflattening) IERS_earthradius_equatorial |
| 2719 | |
| 2720 | |
| 2721 | landarea 148.847e6 km^2 |
| 2722 | oceanarea 361.254e6 km^2 |
| 2723 | |
| 2724 | moonradius 1738 km # mean value |
| 2725 | sunradius 6.96e8 m |
| 2726 | |
| 2727 | # Many astronomical values can be measured most accurately in a system of units |
| 2728 | # using the astronomical unit and the mass of the Sun as base units. The |
| 2729 | # uncertainty in the gravitational constant makes conversion to SI units |
| 2730 | # significantly less accurate. |
| 2731 | |
| 2732 | # The astronomical unit was defined to be the length of the of the semimajor |
| 2733 | # axis of a massless object with the same year as Earth. With such a |
| 2734 | # definition in force, and with the mass of the Sun set equal to one, Kepler's |
| 2735 | # third law can be used to solve for the value of the gravitational constant. |
| 2736 | |
| 2737 | # Kepler's third law says that (2 pi / T)^2 a^3 = G M where T is the orbital |
| 2738 | # period, a is the size of the semimajor axis, G is the gravitational constant |
| 2739 | # and M is the mass. With M = 1 and T and a chosen for Earth's orbit, we |
| 2740 | # find sqrt(G) = (2 pi / T) sqrt(AU^3). This constant is called the Gaussian |
| 2741 | # gravitational constant, apparently because Gauss originally did the |
| 2742 | # calculations. However, when the original calculation was done, the value |
| 2743 | # for the length of Earth's year was inaccurate. The value used is called |
| 2744 | # the Gaussian year. Changing the astronomical unit to bring it into |
| 2745 | # agreement with more accurate values for the year would have invalidated a |
| 2746 | # lot of previous work, so instead the astronomical unit has been kept equal |
| 2747 | # to this original value. This is accomplished by using a standard value for |
| 2748 | # the Gaussian gravitational constant. This constant is called k. |
| 2749 | |
| 2750 | gauss_k 0.01720209895 # This beast has dimensions of |
| 2751 | # au^(3|2) / day and is exact. |
| 2752 | gaussianyear (2 pi / gauss_k) days # Year that corresponds to the Gaussian |
| 2753 | # gravitational constant. This is a |
| 2754 | # fictional year, and doesn't |
| 2755 | # correspond to any celestial event. |
| 2756 | astronomicalunit 149597870700 m # IAU definition from 2012, exact |
| 2757 | au astronomicalunit # ephemeris for the above described |
| 2758 | # astronomical unit. (See the NASA |
| 2759 | # site listed above.) |
| 2760 | GMsun 132712440041.279419 km^3 / s^2 # heliocentric gravitational constant |
| 2761 | solarmass GMsun/G # is known more accurately than G. |
| 2762 | sunmass solarmass # Estimated from DE440 |
| 2763 | |
| 2764 | |
| 2765 | # The following are masses for planetary systems, not just the planet itself, |
| 2766 | # except for the case of Earth, where the Moon is excluded. Masses are |
| 2767 | # relative to G because they are known much more accurately than G. |
| 2768 | # |
| 2769 | # See https://ssd.jpl.nasa.gov/astro_par.html. Values are from |
| 2770 | # the DE440 Ephemeris: https://ssd.jpl.nasa.gov/doc/Park.2021.AJ.DE440.pdf |
| 2771 | |
| 2772 | mercurymass 22031.868551 km^3 / s^2 G |
| 2773 | venusmass 324858.592000 km^3 / s^2 G |
| 2774 | marsmass 42828.375816 km^3 / s^2 G |
| 2775 | jupitermass 126712764.100000 km^3 / s^2 G |
| 2776 | saturnmass 37940584.841800 km^3 / s^2 G |
| 2777 | uranusmass 5794556.400000 km^3 / s^2 G |
| 2778 | neptunemass 6836527.100580 km^3 / s^2 G |
| 2779 | plutomass 975.500000 km^3 / s^2 G |
| 2780 | ceresmass 62.62890 km^3 / s^2 G |
| 2781 | vestamass 17.288245 km^3 / s^2 G |
| 2782 | |
| 2783 | earthmass 398600.435507 km^3 / s^2 G # Earth alone |
| 2784 | moonmass 4902.800118 km^3 / s^2 G |
| 2785 | moonearthmassratio moonmass/earthmass |
| 2786 | earthmoonmass earthmass+moonmass |
| 2787 | |
| 2788 | moongravity 1.62 m/s^2 |
| 2789 | |
| 2790 | # Earth gravity values at the equator and poles. These values are |
| 2791 | # obtained from the WGS84 model. |
| 2792 | |
| 2793 | gravity_equatorial 9.7803263359 m / s^2 |
| 2794 | gravity_polar 9.8321849378 m / s^2 |
| 2795 | |
| 2796 | # The Hubble constant gives the speed at which distance galaxies are moving |
| 2797 | # away from Earth according to v = H0*d, where H0 is the hubble constant |
| 2798 | # and d is the distance to the galaxy. |
| 2799 | |
| 2800 | hubble 70 km/s/Mpc # approximate |
| 2801 | H0 hubble |
| 2802 | |
| 2803 | # Parallax is the angular difference between the topocentric (on Earth's |
| 2804 | # surface) and geocentric (at Earth's center) direction toward a celestial body |
| 2805 | # when the body is at a given altitude. When the body is on the horizon, the |
| 2806 | # parallax is the horizontal parallax; when the body is on the horizon and the |
| 2807 | # observer is on the equator, the parallax is the equatorial horizontal |
| 2808 | # parallax. When the body is at zenith, the parallax is zero. |
| 2809 | |
| 2810 | lunarparallax asin(earthradius_equatorial / moondist) # Moon equatorial |
| 2811 | moonhp lunarparallax # horizontal parallax |
| 2812 | # at mean distance |
| 2813 | |
| 2814 | # Light from celestial objects is attenuated by passage through Earth's |
| 2815 | # atmosphere. A body near the horizon passes through much more air than an |
| 2816 | # object at zenith, and is consequently less bright. Air mass is the ratio of |
| 2817 | # the length of the optical path at a given altitude (angle above the horizon) |
| 2818 | # to the length at zenith. Air mass at zenith is by definition unity; at the |
| 2819 | # horizon, air mass is approximately 38, though the latter value can vary |
| 2820 | # considerably with atmospheric conditions. The general formula is # E = E0 |
| 2821 | # exp(-c X), where E0 is the value outside Earth's atmosphere, E is the value |
| 2822 | # seen by an observer, X is the air mass and c is the extinction coefficient. |
| 2823 | # A common value for c in reasonably clear air is 0.21, but values can be |
| 2824 | # considerably greater in urban areas. Apparent altitude is that perceived by |
| 2825 | # an observer; it includes the effect of atmospheric refraction. There is no |
| 2826 | # shortage of formulas for air mass |
| 2827 | # (https://en.wikipedia.org/wiki/Air_mass_(astronomy)); all are subject to |
| 2828 | # variations in local atmospheric conditions. The formula used here is simple |
| 2829 | # and is in good agreement with rigorously calculated values under standard |
| 2830 | # conditions. |
| 2831 | # |
| 2832 | # Extraterrestrial illuminance or luminance of an object at a given altitude |
| 2833 | # determined with vmag() or SB_xxx() below can be multiplied by |
| 2834 | # atm_transmission() or atm_transmissionz() to estimate the terrestrial value. |
| 2835 | # |
| 2836 | # Kasten and Young (1989) air mass formula. alt is apparent altitude |
| 2837 | # Reference: |
| 2838 | # Kasten, F., and A.T. Young. 1989. "Revised Optical Air Mass Tables |
| 2839 | # and Approximation Formula." Applied Optics. Vol. 28, 4735-4738. |
| 2840 | # Bibcode:1989ApOpt..28.4735K. doi:10.1364/AO.28.004735. |
| 2841 | |
| 2842 | airmass(alt) units=[degree;1] domain=[0,90] noerror \ |
| 2843 | 1 / (sin(alt) + 0.50572 (alt / degree + 6.07995)^-1.6364) |
| 2844 | |
| 2845 | # zenith is apparent zenith angle (zenith = 90 deg - alt) |
| 2846 | airmassz(zenith) units=[degree;1] domain=[0,90] noerror \ |
| 2847 | 1 / (cos(zenith) + 0.50572 (96.07995 - zenith / degree)^-1.6364) |
| 2848 | |
| 2849 | # For reasonably clear air at sea level; values may need adjustment for |
| 2850 | # elevation and local atmospheric conditions |
| 2851 | # for scotopic vision (510 nm), appropriate for the dark-adapted eye |
| 2852 | # extinction_coeff 0.26 |
| 2853 | # for photopic vision, appropriate for observing brighter objects such |
| 2854 | # as the full moon |
| 2855 | extinction_coeff 0.21 |
| 2856 | |
| 2857 | atm_transmission(alt) units=[degree;1] domain=[0,90] noerror \ |
| 2858 | exp(-extinction_coeff airmass(alt)) |
| 2859 | |
| 2860 | # in terms of zenith angle (zenith = 90 deg - alt) |
| 2861 | atm_transmissionz(zenith) units=[degree;1] domain=[0,90] noerror \ |
| 2862 | exp(-extinction_coeff airmassz(zenith)) |
| 2863 | |
| 2864 | # Moon and Sun data at mean distances |
| 2865 | moonvmag -12.74 # Moon apparent visual magnitude at mean distance |
| 2866 | sunvmag -26.74 # Sun apparent visual magnitude at mean distance |
| 2867 | moonsd asin(moonradius / moondist) # Moon angular semidiameter at mean distance |
| 2868 | sunsd asin(sunradius / sundist) # Sun angular semidiameter at mean distance |
| 2869 | |
| 2870 | # Visual magnitude of star or other celestial object. The system of stellar |
| 2871 | # magnitudes, developed in ancient Greece, assigned magnitudes from 1 |
| 2872 | # (brightest) to 6 (faintest visible to the naked eye). In 1856, British |
| 2873 | # astronomer Norman Pogson made the system precise, with a magnitude 1 object |
| 2874 | # 100 times as bright as a magnitude 6 object, and each magnitude differing |
| 2875 | # from the next by a constant ratio; the ratio, sometimes known as Pogson's |
| 2876 | # ratio, is thus 100^0.2, or approximately 2.5119. The logarithm of 100^0.2 is |
| 2877 | # 0.4, hence the common use of powers of 10 and base-10 logarithms. |
| 2878 | # |
| 2879 | # Reference: |
| 2880 | # Allen, C.W. 1976. Astrophysical Quantities, 3rd ed. 1973, reprinted |
| 2881 | # with corrections, 1976. London: Athlone. |
| 2882 | # |
| 2883 | # The function argument is the (dimensionless) visual magnitude; reference |
| 2884 | # illuminance of 2.54e-6 lx is from Allen (2000, 21), and is for outside |
| 2885 | # Earth's atmosphere. Illuminance values can be adjusted to terrestrial values |
| 2886 | # by multiplying by one of the atm_transmission functions above. |
| 2887 | |
| 2888 | # Illuminance from apparent visual magnitude |
| 2889 | vmag(mag) units=[1;lx] domain=[,] range=(0,] \ |
| 2890 | 2.54e-6 lx 10^(-0.4 mag); -2.5 log(vmag / (2.54e-6 lx)) |
| 2891 | |
| 2892 | # Surface brightness of a celestial object of a given visual magnitude |
| 2893 | # is a logarithmic measure of the luminance the object would have if its |
| 2894 | # light were emitted by an object of specified solid angle; it is |
| 2895 | # expressed in magnitudes per solid angle. Surface brightness can be |
| 2896 | # obtained from the visual magnitude by |
| 2897 | # S = m + 2.5 log(pi pi k a b), |
| 2898 | # where k is the phase (fraction illuminated), a is the equatorial |
| 2899 | # radius, and b is the polar radius. For 100% illumination (e.g., full |
| 2900 | # moon), this is often simplified to |
| 2901 | # S = m + 2.5 log(pi k s^2), |
| 2902 | # where s is the object's angular semidiameter; the units of s determine |
| 2903 | # the units of solid angle. The visual magnitude and semidiameter must |
| 2904 | # be appropriate for the object's distance; for other than 100% |
| 2905 | # illumination, the visual magnitude must be appropriate for the phase. |
| 2906 | # Luminance values are for outside Earth's atmosphere; they can be |
| 2907 | # adjusted to terrestrial values by multiplying by one of the atm_transmission |
| 2908 | # functions above. |
| 2909 | |
| 2910 | # luminance from surface brightness in magnitudes per square degree |
| 2911 | SB_degree(sb) units=[1;cd/m^2] domain=[,] range=(0,] \ |
| 2912 | vmag(sb) / squaredegree ; \ |
| 2913 | ~vmag(SB_degree squaredegree) |
| 2914 | |
| 2915 | # luminance from surface brightness in magnitudes per square minute |
| 2916 | SB_minute(sb) units=[1;cd/m^2] domain=[,] range=(0,] \ |
| 2917 | vmag(sb) / squareminute ; \ |
| 2918 | ~vmag(SB_minute squareminute) |
| 2919 | |
| 2920 | # luminance from surface brightness in magnitudes per square second |
| 2921 | SB_second(sb) units=[1;cd/m^2] domain=[,] range=(0,] \ |
| 2922 | vmag(sb) / squaresecond ; \ |
| 2923 | ~vmag(SB_second squaresecond) |
| 2924 | |
| 2925 | # luminance from surface brightness in magnitudes per steradian |
| 2926 | SB_sr(sb) units=[1;cd/m^2] domain=[,] range=(0,] \ |
| 2927 | vmag(sb) / sr ; \ |
| 2928 | ~vmag(SB_sr sr) |
| 2929 | |
| 2930 | SB() SB_second |
| 2931 | SB_sec() SB_second |
| 2932 | SB_min() SB_minute |
| 2933 | SB_deg() SB_degree |
| 2934 | |
| 2935 | # The brightness of one tenth-magnitude star per square degree outside |
| 2936 | # Earth's atmosphere; often used for night sky brightness. |
| 2937 | S10 SB_degree(10) |
| 2938 | |
| 2939 | # Examples for magnitude and surface brightness functions |
| 2940 | # Sun illuminance from visual magnitude |
| 2941 | # You have: sunvmag |
| 2942 | # You want: |
| 2943 | # Definition: -26.74 = -26.74 |
| 2944 | # You have: vmag(sunvmag) |
| 2945 | # You want: lx |
| 2946 | # * 126134.45 |
| 2947 | # / 7.9280482e-06 |
| 2948 | # |
| 2949 | # Moon surface brightness from visual magnitude and semidiameter at 100% |
| 2950 | # illumination (full moon): |
| 2951 | # You have: moonvmag |
| 2952 | # You want: |
| 2953 | # Definition: -12.74 = -12.74 |
| 2954 | # You have: moonsd |
| 2955 | # You want: arcsec |
| 2956 | # * 932.59484 |
| 2957 | # / 0.001072277 |
| 2958 | # You have: moonvmag + 2.5 log(pi 932.59484^2) |
| 2959 | # You want: |
| 2960 | # Definition: 3.3513397 |
| 2961 | # |
| 2962 | # Similar example with specific data obtained from another source (JPL |
| 2963 | # Horizons, https://ssd.jpl.nasa.gov/horizons.cgi); semidiameter is in |
| 2964 | # arcseconds |
| 2965 | # |
| 2966 | # You have: -12.9 + 2.5 log(pi 2023.201|2^2) |
| 2967 | # You want: |
| 2968 | # Definition: 3.3679199 |
| 2969 | # You have: SB_second(-12.9 + 2.5 log(pi 2023.201|2^2)) |
| 2970 | # You want: |
| 2971 | # Definition: 4858.6547 cd / m^2 |
| 2972 | # |
| 2973 | # If surface brightness is provided by another source (e.g., Horizons), |
| 2974 | # it can simply be used directly: |
| 2975 | # You have: SB_second(3.3679199) |
| 2976 | # You want: cd/m^2 |
| 2977 | # * 4858.6546 |
| 2978 | # / 0.0002058183 |
| 2979 | # The illuminance and luminance values are extraterrestrial (outside |
| 2980 | # Earth's atmosphere). The values at Earth's surface are less than these |
| 2981 | # because of atmospheric extinction. For example, in the last example |
| 2982 | # above, if the Moon were at an altitude of 55 degrees, the terrestrial |
| 2983 | # luminance could be calculated with |
| 2984 | # You have: SB_second(3.3679199) |
| 2985 | # You want: cd/m^2 |
| 2986 | # * 4858.6546 |
| 2987 | # / 0.0002058183 |
| 2988 | # You have: _ atm_transmission(55 deg) |
| 2989 | # You want: cd/m^2 |
| 2990 | # * 3760.6356 |
| 2991 | # / 0.0002659125 |
| 2992 | # If desired, photographic exposure can be determined with EV100(), |
| 2993 | # leading to acceptable combinations of aperture and exposure time. |
| 2994 | # For the example above, but with the Moon at 10 degrees, |
| 2995 | # You have: SB_second(3.3679199) atm_transmission(10 deg) |
| 2996 | # You want: EV100 |
| 2997 | # 13.553962 |
| 2998 | |
| 2999 | # |
| 3000 | # The Hartree system of atomic units, derived from fundamental units |
| 3001 | # of mass (of the electron), action (Planck's constant), charge, and |
| 3002 | # the Coulomb constant. This system is used in the fields of physical |
| 3003 | # chemistry and condensed matter physics. |
| 3004 | # |
| 3005 | |
| 3006 | # Fundamental units |
| 3007 | |
| 3008 | atomicmass electronmass |
| 3009 | atomiccharge e |
| 3010 | atomicaction hbar |
| 3011 | atomicenergy hartree |
| 3012 | |
| 3013 | # Derived units |
| 3014 | |
| 3015 | atomicvelocity sqrt(atomicenergy / atomicmass) |
| 3016 | atomictime atomicaction / atomicenergy |
| 3017 | atomiclength atomicvelocity atomictime |
| 3018 | atomicforce atomicenergy / atomiclength |
| 3019 | atomicmomentum atomicenergy / atomicvelocity |
| 3020 | atomiccurrent atomiccharge / atomictime |
| 3021 | atomicpotential atomicenergy / atomiccharge # electrical potential |
| 3022 | atomicvolt atomicpotential |
| 3023 | atomicEfield atomicpotential / atomiclength |
| 3024 | atomicBfield atomicEfield / atomicvelocity |
| 3025 | atomictemperature atomicenergy / boltzmann |
| 3026 | |
| 3027 | # |
| 3028 | # In Hartree units, m_e = hbar = e = coulombconst = bohrradius = alpha*c = 1 |
| 3029 | # |
| 3030 | |
| 3031 | !var UNITS_SYSTEM hartree |
| 3032 | !message Hartree units selected |
| 3033 | !prompt (hartree) |
| 3034 | +hartree 1 |
| 3035 | +kg 1/electronmass_SI |
| 3036 | +K k_SI / hbar_SI s |
| 3037 | +m alpha c_SI electronmass_SI / hbar_SI |
| 3038 | +s alpha c_SI m |
| 3039 | +A 1 / s e_SI |
| 3040 | !endvar |
| 3041 | |
| 3042 | # |
| 3043 | # These thermal units treat entropy as charge, from [5] |
| 3044 | # |
| 3045 | |
| 3046 | thermalcoulomb J/K # entropy |
| 3047 | thermalampere W/K # entropy flow |
| 3048 | thermalfarad J/K^2 |
| 3049 | thermalohm K^2/W # thermal resistance |
| 3050 | fourier thermalohm |
| 3051 | thermalhenry J K^2/W^2 # thermal inductance |
| 3052 | thermalvolt K # thermal potential difference |
| 3053 | |
| 3054 | |
| 3055 | # |
| 3056 | # United States units |
| 3057 | # |
| 3058 | |
| 3059 | # linear measure |
| 3060 | |
| 3061 | # The US Metric Law of 1866 legalized the metric system in the USA and |
| 3062 | # defined the meter in terms of the British system with the exact |
| 3063 | # 1 meter = 39.37 inches. On April 5, 1893 Thomas Corwin Mendenhall, |
| 3064 | # Superintendent of Weights and Measures, decided, in what has become |
| 3065 | # known as the "Mendenhall Order" that the meter and kilogram would be the |
| 3066 | # fundamental standards in the USA. The definition from 1866 was turned |
| 3067 | # around to give an exact definition of the yard as 3600|3937 meters This |
| 3068 | # definition was used until July of 1959 when the definition was changed |
| 3069 | # to bring the US and other English-speaking countries into agreement; the |
| 3070 | # Canadian value of 1 yard = 0.9144 meter (exactly) was chosen because it |
| 3071 | # was approximately halfway between the British and US values; it had the |
| 3072 | # added advantage of making 1 inch = 25.4 mm (exactly). Since 1959, the |
| 3073 | # "international" foot has been exactly 0.3048 meters. At the same time, |
| 3074 | # it was decided that any data expressed in feet derived from geodetic |
| 3075 | # surveys within the US would continue to use the old definition and call |
| 3076 | # the old unit the "survey foot." |
| 3077 | # |
| 3078 | # Until 1 January 2023, the US continued to define the statute |
| 3079 | # mile, furlong, chain, rod, link, and fathom in terms of the US survey |
| 3080 | # foot. Since then, use of the US survey foot has been officially |
| 3081 | # deprecated, with its use limited to historical and legacy applications. |
| 3082 | # These units are now defined in terms of the international foot. |
| 3083 | # |
| 3084 | # Sources: |
| 3085 | # NIST Special Publication 447, Sects. 5, 7, and 8. |
| 3086 | # NIST Handbook 44, 2024 ed., Appendix C. |
| 3087 | # Canadian Journal of Physics, 1959, 37:(1) 84, 10.1139/p59-014. |
| 3088 | |
| 3089 | inch 2.54 cm # Exact, international inch (1959) |
| 3090 | in inch |
| 3091 | foot 12 inch |
| 3092 | feet foot |
| 3093 | ft foot |
| 3094 | yard 3 ft |
| 3095 | yd yard |
| 3096 | mile 5280 ft # The mile was enlarged from 5000 ft |
| 3097 | # to this number in order to make |
| 3098 | # it an even number of furlongs. |
| 3099 | # (The Roman mile is 5000 romanfeet.) |
| 3100 | line 1|12 inch # Also defined as '.1 in' or as '1e-8 Wb' |
| 3101 | rod 16.5 ft |
| 3102 | pole rod |
| 3103 | perch rod |
| 3104 | furlong 40 rod # From "furrow long" |
| 3105 | statutemile mile |
| 3106 | league 3 mile # Intended to be an hour's walk |
| 3107 | |
| 3108 | # surveyor's measure |
| 3109 | # The US survey foot is officially deprecated as of 1 January 2023 |
| 3110 | US 1200|3937 m/ft # These four values will convert |
| 3111 | US- US # international measures to |
| 3112 | survey- US # US Survey measures |
| 3113 | geodetic- US |
| 3114 | int 3937|1200 ft/m # Convert US Survey measures to |
| 3115 | int- int # international measures |
| 3116 | |
| 3117 | # values based on the US survey foot are deprecated as of 1 January 2023 |
| 3118 | surveyorschain 66 surveyft |
| 3119 | surveychain surveyorschain |
| 3120 | surveyorspole 1|4 surveyorschain |
| 3121 | surveyorslink 1|100 surveyorschain |
| 3122 | USacre 10 surveychain^2 |
| 3123 | USacrefoot USacre surveyfoot |
| 3124 | |
| 3125 | chain 66 ft |
| 3126 | link 1|100 chain |
| 3127 | ch chain |
| 3128 | intacre 10 chain^2 # Acre based on international ft |
| 3129 | intacrefoot acre foot |
| 3130 | acrefoot intacrefoot |
| 3131 | acre intacre |
| 3132 | ac acre |
| 3133 | section mile^2 |
| 3134 | township 36 section |
| 3135 | homestead 160 acre # Area of land granted by the 1862 Homestead |
| 3136 | # Act of the United States Congress |
| 3137 | gunterschain surveyorschain |
| 3138 | |
| 3139 | engineerschain 100 ft |
| 3140 | engineerslink 1|100 engineerschain |
| 3141 | ramsdenschain engineerschain |
| 3142 | ramsdenslink engineerslink |
| 3143 | |
| 3144 | gurleychain 33 feet # Andrew Ellicott chain is the |
| 3145 | gurleylink 1|50 gurleychain # same length |
| 3146 | |
| 3147 | wingchain 66 feet # Chain from 1664, introduced by |
| 3148 | winglink 1|80 wingchain # Vincent Wing, also found in a |
| 3149 | # 33 foot length with 40 links. |
| 3150 | # early US length standards |
| 3151 | |
| 3152 | # The US has had four standards for the yard: one by Troughton of London |
| 3153 | # (1815); bronze yard #11 (1856); the Mendhall yard (1893), consistent |
| 3154 | # with the definition of the meter in the metric joint resolution of |
| 3155 | # Congress in 1866, but defining the yard in terms of the meter; and the |
| 3156 | # international yard (1959), which standardized definitions for Australia, |
| 3157 | # Canada, New Zealand, South Africa, the UK, and the US. |
| 3158 | # Sources: Pat Naughtin (2009), Which Inch?: |
| 3159 | # https://metricationmatters.org/docs/WhichInch.pdf, |
| 3160 | # Lewis E. Barbrow and Lewis V. Judson (1976). NBS Special |
| 3161 | # Publication 447, Weights and Measures Standards of the United States: A |
| 3162 | # Brief History. |
| 3163 | |
| 3164 | troughtonyard 914.42190 mm |
| 3165 | bronzeyard11 914.39980 mm |
| 3166 | mendenhallyard surveyyard |
| 3167 | internationalyard yard |
| 3168 | |
| 3169 | # nautical measure |
| 3170 | |
| 3171 | fathom 6 ft # Originally defined as the distance from |
| 3172 | # fingertip to fingertip with arms fully |
| 3173 | # extended. |
| 3174 | nauticalmile 1852 m # Supposed to be one minute of latitude at |
| 3175 | # the equator. That value is about 1855 m. |
| 3176 | # Early estimates of Earth's circumference |
| 3177 | # were a bit off. The value of 1852 m was |
| 3178 | # made the international standard in 1929. |
| 3179 | # The US did not accept this value until |
| 3180 | # 1954. The UK switched in 1970. |
| 3181 | |
| 3182 | # The cable is used for depth in water and has a wide range of definitions |
| 3183 | |
| 3184 | intcable 1|10 nauticalmile # international cable |
| 3185 | uscable 120 fathom # value after 1 January 2023 |
| 3186 | surveycable 120 USfathom # value before 1 January 2023 |
| 3187 | UScable surveycable |
| 3188 | cableslength cable |
| 3189 | cablelength cable |
| 3190 | navycablelength cable |
| 3191 | brcable 1|10 brnauticalmile |
| 3192 | admiraltycable brcable |
| 3193 | |
| 3194 | marineleague 3 nauticalmile |
| 3195 | geographicalmile brnauticalmile |
| 3196 | knot nauticalmile / hr |
| 3197 | click km # US military slang |
| 3198 | klick click |
| 3199 | |
| 3200 | # Avoirdupois weight |
| 3201 | |
| 3202 | pound 0.45359237 kg # Exact, International Pound (1959) |
| 3203 | lb pound # From the Latin libra |
| 3204 | grain 1|7000 pound # The grain is the same in all three |
| 3205 | # weight systems. It was originally |
| 3206 | # defined as the weight of a barley |
| 3207 | # corn taken from the middle of the |
| 3208 | # ear. |
| 3209 | ounce 1|16 pound |
| 3210 | oz ounce |
| 3211 | dram 1|16 ounce |
| 3212 | dr dram |
| 3213 | ushundredweight 100 pounds |
| 3214 | cwt hundredweight |
| 3215 | shorthundredweight ushundredweight |
| 3216 | uston shortton |
| 3217 | shortton 2000 lb |
| 3218 | quarterweight 1|4 uston |
| 3219 | shortquarterweight 1|4 shortton |
| 3220 | shortquarter shortquarterweight |
| 3221 | |
| 3222 | # Troy Weight. In 1828 the troy pound was made the first United States |
| 3223 | # standard weight. It was to be used to regulate coinage. |
| 3224 | |
| 3225 | troypound 5760 grain |
| 3226 | troyounce 1|12 troypound |
| 3227 | ozt troyounce |
| 3228 | pennyweight 1|20 troyounce # Abbreviated "d" in reference to a |
| 3229 | dwt pennyweight # Frankish coin called the "denier" |
| 3230 | # minted in the late 700's. There |
| 3231 | # were 240 deniers to the pound. |
| 3232 | assayton mg ton / troyounce # mg / assayton = troyounce / ton |
| 3233 | usassayton mg uston / troyounce |
| 3234 | brassayton mg brton / troyounce |
| 3235 | fineounce troyounce # A troy ounce of 99.5% pure gold |
| 3236 | |
| 3237 | # Some other jewelers units |
| 3238 | |
| 3239 | metriccarat 0.2 gram # Defined in 1907 |
| 3240 | metricgrain 50 mg |
| 3241 | carat metriccarat |
| 3242 | ct carat |
| 3243 | jewelerspoint 1|100 carat |
| 3244 | silversmithpoint 1|4000 inch |
| 3245 | momme 3.75 grams # Traditional Japanese unit based |
| 3246 | # on the chinese mace. It is used for |
| 3247 | # pearls in modern times and also for |
| 3248 | # silk density. The definition here |
| 3249 | # was adopted in 1891. |
| 3250 | # Apothecaries' weight |
| 3251 | |
| 3252 | appound troypound |
| 3253 | apounce troyounce |
| 3254 | apdram 1|8 apounce |
| 3255 | apscruple 1|3 apdram |
| 3256 | |
| 3257 | # Liquid measure |
| 3258 | |
| 3259 | usgallon 231 in^3 # US liquid measure is derived from |
| 3260 | gal gallon # the British wine gallon of 1707. |
| 3261 | quart 1|4 gallon # See the "winegallon" entry below |
| 3262 | pint 1|2 quart # more historical information. |
| 3263 | gill 1|4 pint |
| 3264 | usquart 1|4 usgallon |
| 3265 | uspint 1|2 usquart |
| 3266 | usgill 1|4 uspint |
| 3267 | usfluidounce 1|16 uspint |
| 3268 | fluiddram 1|8 usfloz |
| 3269 | minimvolume 1|60 fluiddram |
| 3270 | qt quart |
| 3271 | pt pint |
| 3272 | floz fluidounce |
| 3273 | usfloz usfluidounce |
| 3274 | fldr fluiddram |
| 3275 | liquidbarrel 31.5 usgallon |
| 3276 | usbeerbarrel 2 beerkegs |
| 3277 | beerkeg 15.5 usgallon # Various among brewers |
| 3278 | ponykeg 1|2 beerkeg |
| 3279 | winekeg 12 usgallon |
| 3280 | petroleumbarrel 42 usgallon # Originated in Pennsylvania oil |
| 3281 | barrel petroleumbarrel # fields, from the winetierce |
| 3282 | bbl barrel |
| 3283 | ushogshead 2 liquidbarrel |
| 3284 | usfirkin 9 usgallon |
| 3285 | |
| 3286 | # Dry measures: The Winchester Bushel was defined by William III in 1702 and |
| 3287 | # legally adopted in the US in 1836. |
| 3288 | |
| 3289 | usbushel 2150.42 in^3 # Volume of 8 inch cylinder with 18.5 |
| 3290 | bu bushel # inch diameter (rounded) |
| 3291 | peck 1|4 bushel |
| 3292 | uspeck 1|4 usbushel |
| 3293 | brpeck 1|4 brbushel |
| 3294 | pk peck |
| 3295 | drygallon 1|2 uspeck |
| 3296 | dryquart 1|4 drygallon |
| 3297 | drypint 1|2 dryquart |
| 3298 | drybarrel 7056 in^3 # Used in US for fruits, vegetables, |
| 3299 | # and other dry commodities except for |
| 3300 | # cranberries. |
| 3301 | cranberrybarrel 5826 in^3 # US cranberry barrel |
| 3302 | heapedbushel 1.278 usbushel# The following explanation for this |
| 3303 | # value was provided by Wendy Krieger |
| 3304 | # <os2fan2@yahoo.com> based on |
| 3305 | # guesswork. The cylindrical vessel is |
| 3306 | # 18.5 inches in diameter and 1|2 inch |
| 3307 | # thick. A heaped bushel includes the |
| 3308 | # contents of this cylinder plus a heap |
| 3309 | # on top. The heap is a cone 19.5 |
| 3310 | # inches in diameter and 6 inches |
| 3311 | # high. With these values, the volume |
| 3312 | # of the bushel is 684.5 pi in^3 and |
| 3313 | # the heap occupies 190.125 pi in^3. |
| 3314 | # Therefore, the heaped bushel is |
| 3315 | # 874.625|684.5 bushels. This value is |
| 3316 | # approximately 1.2777575 and it rounds |
| 3317 | # to the value listed for the size of |
| 3318 | # the heaped bushel. Sometimes the |
| 3319 | # heaped bushel is reported as 1.25 |
| 3320 | # bushels. This same explanation gives |
| 3321 | # that value if the heap is taken to |
| 3322 | # have an 18.5 inch diameter. |
| 3323 | |
| 3324 | # Grain measures. The bushel as it is used by farmers in the USA is actually |
| 3325 | # a measure of mass which varies for different commodities. Canada uses the |
| 3326 | # same bushel masses for most commodities, but not for oats. |
| 3327 | |
| 3328 | wheatbushel 60 lb |
| 3329 | soybeanbushel 60 lb |
| 3330 | cornbushel 56 lb |
| 3331 | ryebushel 56 lb |
| 3332 | barleybushel 48 lb |
| 3333 | oatbushel 32 lb |
| 3334 | ricebushel 45 lb |
| 3335 | canada_oatbushel 34 lb |
| 3336 | |
| 3337 | # Wine and Spirits measure |
| 3338 | |
| 3339 | ponyvolume 1 usfloz |
| 3340 | jigger 1.5 usfloz # Can vary between 1 and 2 usfloz |
| 3341 | shot jigger # Sometimes 1 usfloz |
| 3342 | eushot 25 ml # EU standard spirits measure |
| 3343 | fifth 1|5 usgallon |
| 3344 | winebottle 750 ml # US industry standard, 1979 |
| 3345 | winesplit 1|4 winebottle |
| 3346 | magnum 1.5 liter # Standardized in 1979, but given |
| 3347 | # as 2 qt in some references |
| 3348 | metrictenth 375 ml |
| 3349 | metricfifth 750 ml |
| 3350 | metricquart 1 liter |
| 3351 | |
| 3352 | # Old British bottle size |
| 3353 | |
| 3354 | reputedquart 1|6 brgallon |
| 3355 | reputedpint 1|2 reputedquart |
| 3356 | brwinebottle reputedquart # Very close to 1|5 winegallon |
| 3357 | |
| 3358 | # French champagne bottle sizes |
| 3359 | |
| 3360 | split 200 ml |
| 3361 | jeroboam 2 magnum |
| 3362 | rehoboam 3 magnum |
| 3363 | methuselah 4 magnum |
| 3364 | imperialbottle 4 magnum |
| 3365 | salmanazar 6 magnum |
| 3366 | balthazar 8 magnum |
| 3367 | nebuchadnezzar 10 magnum |
| 3368 | solomon 12 magnum |
| 3369 | melchior 12 magnum |
| 3370 | sovereign 17.5 magnum |
| 3371 | primat 18 magnum |
| 3372 | goliath 18 magnum |
| 3373 | melchizedek 20 magnum |
| 3374 | midas 20 magnum |
| 3375 | |
| 3376 | # The wine glass doesn't seem to have an official standard, but the same value |
| 3377 | # is suggested by several sources in the US. |
| 3378 | |
| 3379 | wineglass 150 mL |
| 3380 | |
| 3381 | # In the UK, serving size offerings legally mandated by The Weights and |
| 3382 | # Measures (Specified Quantities) (Unwrapped Bread and Intoxicating |
| 3383 | # Liquor) Order 2011, effective 1st October 2011. The quantities--not |
| 3384 | # the names--are mandated. Lawful size offerings are these or multiples |
| 3385 | # thereof, but other sizes can be provided at the express request of a |
| 3386 | # buyer. |
| 3387 | |
| 3388 | smallwineglass 125 mL |
| 3389 | mediumwineglass 175 mL |
| 3390 | |
| 3391 | # Values vary considerably among countries and even more so in practice. The |
| 3392 | # "standard" US value gives 5 glasses per standard 750 ml bottle. Old practice |
| 3393 | # in the UK was 125 ml per glass, or 6 glasses per bottle. Some sources suggest |
| 3394 | # a more recent common value of 250 ml per glass, or 3 glasses per |
| 3395 | # bottle; as a multiple of 125 ml, this would be a lawful serving size offering. |
| 3396 | # |
| 3397 | # The value refers to the size of the serving, not the total volume of the |
| 3398 | # glass, which is typically not filled above the height of its greatest |
| 3399 | # diameter. |
| 3400 | # |
| 3401 | # A unit of alcohol is a specified amount of pure ethyl alcohol, expressed as a |
| 3402 | # mass or volumetric equivalent. Many countries use the same concept but use |
| 3403 | # different terms. "Alcohol unit" is used officially in the UK; the US, Canada, |
| 3404 | # and Australia use "standard drink." Values vary considerably among |
| 3405 | # countries. The UK value of 8 g is nominally the amount of alcohol that a |
| 3406 | # typical adult can metabolize in one hour. |
| 3407 | |
| 3408 | alcoholunitus 14 g / ethanoldensity |
| 3409 | alcoholunitca 13.6 g / ethanoldensity |
| 3410 | alcoholunituk 8 g / ethanoldensity |
| 3411 | alcoholunitau 10 g / ethanoldensity |
| 3412 | |
| 3413 | # Common serving sizes have roughly equivalent amounts of alcohol, as |
| 3414 | # illustrated by US examples for wine (12% Alcohol By Volume), beer (5% ABV), |
| 3415 | # and spirits (80 proof). |
| 3416 | # |
| 3417 | # alcoholunitus / 12% = 147.8 mL, close to the "standard" serving of 150 mL. |
| 3418 | # alcoholunitus / 5% = 11.995346 floz, close to a standard 12 floz bottle or can |
| 3419 | # alcoholunitus / 80 proof = 1.4994182 floz, close to a standard "shot" or jigger |
| 3420 | |
| 3421 | # https://www.rethinkingdrinking.niaaa.nih.gov/ |
| 3422 | # https://www.cdc.gov/alcohol/faqs.htm |
| 3423 | # https://www.canada.ca/en/health-canada/services/substance-use/alcohol/low-risk-alcohol-drinking-guidelines |
| 3424 | # https://www.drinkaware.co.uk/ |
| 3425 | # https://www.drinkaware.co.uk/facts/alcoholic-drinks-and-units |
| 3426 | # https://www.gov.uk/government/uploads/system/uploads/attachment_data/file/545937/UK_CMOs__report.pdf |
| 3427 | # https://adf.org.au/reducing-risk/alcohol/alcohol-guidelines/ |
| 3428 | # https://www.health.gov.au/topics/alcohol/about-alcohol/standard-drinks-guide |
| 3429 | # https://en.wikipedia.org/wiki/Unit_of_alcohol |
| 3430 | # https://en.wikipedia.org/wiki/Standard_drink |
| 3431 | |
| 3432 | # Coffee |
| 3433 | # |
| 3434 | # The recommended ratio of coffee to water. Values vary considerably; |
| 3435 | # one is from the Specialty Coffee Association of America: Brewing Best Practices |
| 3436 | # https://sca.coffee/research/protocols-best-practices |
| 3437 | |
| 3438 | coffeeratio 55 g/L # +/- 10% |
| 3439 | |
| 3440 | # other recommendations are more loose, e.g., |
| 3441 | # http://www.ncausa.org/About-Coffee/How-to-Brew-Coffee |
| 3442 | |
| 3443 | |
| 3444 | # |
| 3445 | # Water is "hard" if it contains various minerals, especially calcium |
| 3446 | # carbonate. |
| 3447 | # |
| 3448 | |
| 3449 | clarkdegree grains/brgallon # Content by weigh of calcium carbonate |
| 3450 | gpg grains/usgallon # Divide by water's density to convert to |
| 3451 | # a dimensionless concentration measure |
| 3452 | # |
| 3453 | # Shoe measures |
| 3454 | # |
| 3455 | |
| 3456 | shoeiron 1|48 inch # Used to measure leather in soles |
| 3457 | shoeounce 1|64 inch # Used to measure non-sole shoe leather |
| 3458 | |
| 3459 | # USA shoe sizes. These express the length of the shoe or the length |
| 3460 | # of the "last", the form that the shoe is made on. But note that |
| 3461 | # this only captures the length. It appears that widths change 1/4 |
| 3462 | # inch for each letter within the same size, and if you change the |
| 3463 | # length by half a size then the width changes between 1/8 inch and |
| 3464 | # 1/4 inch. But this may not be standard. If you know better, please |
| 3465 | # contact me. |
| 3466 | |
| 3467 | shoesize_delta 1|3 inch # USA shoe sizes differ by this amount |
| 3468 | shoe_men0 8.25 inch |
| 3469 | shoe_women0 (7+11|12) inch |
| 3470 | shoe_boys0 (3+11|12) inch |
| 3471 | shoe_girls0 (3+7|12) inch |
| 3472 | |
| 3473 | shoesize_men(n) units=[1;inch] shoe_men0 + n shoesize_delta ; \ |
| 3474 | (shoesize_men+(-shoe_men0))/shoesize_delta |
| 3475 | shoesize_women(n) units=[1;inch] shoe_women0 + n shoesize_delta ; \ |
| 3476 | (shoesize_women+(-shoe_women0))/shoesize_delta |
| 3477 | shoesize_boys(n) units=[1;inch] shoe_boys0 + n shoesize_delta ; \ |
| 3478 | (shoesize_boys+(-shoe_boys0))/shoesize_delta |
| 3479 | shoesize_girls(n) units=[1;inch] shoe_girls0 + n shoesize_delta ; \ |
| 3480 | (shoesize_girls+(-shoe_girls0))/shoesize_delta |
| 3481 | |
| 3482 | # European shoe size. According to |
| 3483 | # http://www.shoeline.com/footnotes/shoeterm.shtml |
| 3484 | # shoe sizes in Europe are measured with Paris points which simply measure |
| 3485 | # the length of the shoe. |
| 3486 | |
| 3487 | europeshoesize 2|3 cm |
| 3488 | |
| 3489 | # |
| 3490 | # USA slang units |
| 3491 | # |
| 3492 | |
| 3493 | buck US$ |
| 3494 | fin 5 US$ |
| 3495 | sawbuck 10 US$ |
| 3496 | usgrand 1000 US$ |
| 3497 | greenback US$ |
| 3498 | key kg # usually of marijuana, 60's |
| 3499 | lid 1 oz # Another 60's weed unit |
| 3500 | footballfield usfootballfield |
| 3501 | usfootballfield 100 yards |
| 3502 | canadafootballfield 110 yards # And 65 yards wide |
| 3503 | marathon 26 miles + 385 yards |
| 3504 | |
| 3505 | # |
| 3506 | # British |
| 3507 | # |
| 3508 | |
| 3509 | # The length measure in the UK was defined by a bronze bar manufactured in |
| 3510 | # 1844. Various conversions were sanctioned for convenience at different |
| 3511 | # times, which makes conversions before 1963 a confusing matter. Apparently |
| 3512 | # previous conversions were never explicitly revoked. Four different |
| 3513 | # conversion factors appear below. Multiply them times an imperial length |
| 3514 | # units as desired. The Weights and Measures Act of 1963 switched the UK away |
| 3515 | # from their bronze standard and onto a definition of the yard in terms of the |
| 3516 | # meter. This happened after an international agreement in 1959 to align the |
| 3517 | # world's measurement systems. |
| 3518 | |
| 3519 | UK UKlength_SJJ |
| 3520 | UK- UK |
| 3521 | british- UK |
| 3522 | |
| 3523 | UKlength_B 0.9143992 meter / yard # Benoit found the yard to be |
| 3524 | # 0.9143992 m at a weights and |
| 3525 | # measures conference around |
| 3526 | # 1896. Legally sanctioned |
| 3527 | # in 1898. |
| 3528 | UKlength_SJJ 0.91439841 meter / yard # In 1922, Seers, Jolly and |
| 3529 | # Johnson found the yard to be |
| 3530 | # 0.91439841 meters. |
| 3531 | # Used starting in the 1930's. |
| 3532 | UKlength_K meter / 39.37079 inch # In 1816 Kater found this ratio |
| 3533 | # for the meter and inch. This |
| 3534 | # value was used as the legal |
| 3535 | # conversion ratio when the |
| 3536 | # metric system was legalized |
| 3537 | # for contract in 1864. |
| 3538 | UKlength_C meter / 1.09362311 yard # In 1866 Clarke found the meter |
| 3539 | # to be 1.09362311 yards. This |
| 3540 | # conversion was legalized |
| 3541 | # around 1878. |
| 3542 | brnauticalmile 6080 ft # Used until 1970 when the UK |
| 3543 | brknot brnauticalmile / hr # switched to the international |
| 3544 | admiraltymile brnauticalmile # nautical mile. |
| 3545 | admiraltyknot brknot |
| 3546 | seamile 6000 ft |
| 3547 | shackle 15 fathoms # Adopted 1949 by British navy |
| 3548 | |
| 3549 | # British Imperial weight is mostly the same as US weight. A few extra |
| 3550 | # units are added here. |
| 3551 | |
| 3552 | clove 7 lb |
| 3553 | stone 14 lb |
| 3554 | tod 28 lb |
| 3555 | brquarterweight 1|4 brhundredweight |
| 3556 | brhundredweight 8 stone |
| 3557 | longhundredweight brhundredweight |
| 3558 | longton 20 brhundredweight |
| 3559 | brton longton |
| 3560 | |
| 3561 | # British Imperial volume measures |
| 3562 | |
| 3563 | brminim 1|60 brdram |
| 3564 | brscruple 1|3 brdram |
| 3565 | fluidscruple brscruple |
| 3566 | brdram 1|8 brfloz |
| 3567 | brfluidounce 1|20 brpint |
| 3568 | brfloz brfluidounce |
| 3569 | brgill 1|4 brpint |
| 3570 | brpint 1|2 brquart |
| 3571 | brquart 1|4 brgallon |
| 3572 | brgallon 4.54609 l # The British Imperial gallon was |
| 3573 | # defined in 1824 to be the volume of |
| 3574 | # water which weighed 10 pounds at 62 |
| 3575 | # deg F with a pressure of 30 inHg. |
| 3576 | # It was also defined as 277.274 in^3, |
| 3577 | # Which is slightly in error. In |
| 3578 | # 1963 it was defined to be the volume |
| 3579 | # occupied by 10 pounds of distilled |
| 3580 | # water of density 0.998859 g/ml weighed |
| 3581 | # in air of density 0.001217 g/ml |
| 3582 | # against weights of density 8.136 g/ml. |
| 3583 | # This gives a value of approximately |
| 3584 | # 4.5459645 liters, but the old liter |
| 3585 | # was in force at this time. In 1976 |
| 3586 | # the definition was changed to exactly |
| 3587 | # 4.54609 liters using the new |
| 3588 | # definition of the liter (1 dm^3). |
| 3589 | brbarrel 36 brgallon # Used for beer |
| 3590 | brbushel 8 brgallon |
| 3591 | brheapedbushel 1.278 brbushel |
| 3592 | brquarter 8 brbushel |
| 3593 | brchaldron 36 brbushel |
| 3594 | |
| 3595 | # Obscure British volume measures. These units are generally traditional |
| 3596 | # measures whose definitions have fluctuated over the years. Often they |
| 3597 | # depended on the quantity being measured. They are given here in terms of |
| 3598 | # British Imperial measures. For example, the puncheon may have historically |
| 3599 | # been defined relative to the wine gallon or beer gallon or ale gallon |
| 3600 | # rather than the British Imperial gallon. |
| 3601 | |
| 3602 | bag 4 brbushel |
| 3603 | bucket 4 brgallon |
| 3604 | kilderkin 2 brfirkin |
| 3605 | last 40 brbushel |
| 3606 | noggin brgill |
| 3607 | pottle 0.5 brgallon |
| 3608 | pin 4.5 brgallon |
| 3609 | puncheon 72 brgallon |
| 3610 | seam 8 brbushel |
| 3611 | coomb 4 brbushel |
| 3612 | boll 6 brbushel |
| 3613 | firlot 1|4 boll |
| 3614 | brfirkin 9 brgallon # Used for ale and beer |
| 3615 | cran 37.5 brgallon # measures herring, about 750 fish |
| 3616 | brwinehogshead 52.5 brgallon # This value is approximately equal |
| 3617 | brhogshead brwinehogshead # to the old wine hogshead of 63 |
| 3618 | # wine gallons. This adjustment |
| 3619 | # is listed in the OED and in |
| 3620 | # "The Weights and Measures of |
| 3621 | # England" by R. D. Connor |
| 3622 | brbeerhogshead 54 brgallon |
| 3623 | brbeerbutt 2 brbeerhogshead |
| 3624 | registerton 100 ft^3 # Used for internal capacity of ships |
| 3625 | shippington 40 ft^3 # Used for ship's cargo freight or timber |
| 3626 | brshippington 42 ft^3 # |
| 3627 | freightton shippington # Both register ton and shipping ton derive |
| 3628 | # from the "tun cask" of wine. |
| 3629 | displacementton 35 ft^3 # Approximate volume of a longton weight of |
| 3630 | # sea water. Measures water displaced by |
| 3631 | # ships. |
| 3632 | waterton 224 brgallon |
| 3633 | strike 70.5 l # 16th century unit, sometimes |
| 3634 | # defined as .5, 2, or 4 bushels |
| 3635 | # depending on the location. It |
| 3636 | # probably doesn't make a lot of |
| 3637 | # sense to define in terms of imperial |
| 3638 | # bushels. Zupko gives a value of |
| 3639 | # 2 Winchester grain bushels or about |
| 3640 | # 70.5 liters. |
| 3641 | amber 4 brbushel# Used for dry and liquid capacity [18] |
| 3642 | |
| 3643 | # British volume measures with "imperial" |
| 3644 | |
| 3645 | imperialminim brminim |
| 3646 | imperialscruple brscruple |
| 3647 | imperialdram brdram |
| 3648 | imperialfluidounce brfluidounce |
| 3649 | imperialfloz brfloz |
| 3650 | imperialgill brgill |
| 3651 | imperialpint brpint |
| 3652 | imperialquart brquart |
| 3653 | imperialgallon brgallon |
| 3654 | imperialbarrel brbarrel |
| 3655 | imperialbushel brbushel |
| 3656 | imperialheapedbushel brheapedbushel |
| 3657 | imperialquarter brquarter |
| 3658 | imperialchaldron brchaldron |
| 3659 | imperialwinehogshead brwinehogshead |
| 3660 | imperialhogshead brhogshead |
| 3661 | imperialbeerhogshead brbeerhogshead |
| 3662 | imperialbeerbutt brbeerbutt |
| 3663 | imperialfirkin brfirkin |
| 3664 | |
| 3665 | # obscure British lengths |
| 3666 | |
| 3667 | barleycorn 1|3 UKinch # Given in Realm of Measure as the |
| 3668 | # difference between successive shoe sizes |
| 3669 | nail 1|16 UKyard # Originally the width of the thumbnail, |
| 3670 | # or 1|16 ft. This took on the general |
| 3671 | # meaning of 1|16 and settled on the |
| 3672 | # nail of a yard or 1|16 yards as its |
| 3673 | # final value. [12] |
| 3674 | UKpole 16.5 UKft # This was 15 Saxon feet, the Saxon |
| 3675 | rope 20 UKft # foot (aka northern foot) being longer |
| 3676 | englishell 45 UKinch |
| 3677 | flemishell 27 UKinch |
| 3678 | ell englishell # supposed to be measure from elbow to |
| 3679 | # fingertips |
| 3680 | span 9 UKinch # supposed to be distance from thumb |
| 3681 | # to pinky with full hand extension |
| 3682 | goad 4.5 UKft # used for cloth, possibly named after the |
| 3683 | # stick used for prodding animals. |
| 3684 | |
| 3685 | # misc obscure British units |
| 3686 | |
| 3687 | hide 120 acre # English unit of land area dating to the 7th |
| 3688 | # century, originally the amount of land |
| 3689 | # that a single plowman could cultivate, |
| 3690 | # which varied from 60-180 acres regionally. |
| 3691 | # Standardized at Normon conquest. |
| 3692 | virgate 1|4 hide |
| 3693 | nook 1|2 virgate |
| 3694 | rood furlong rod # Area of a strip a rod by a furlong |
| 3695 | englishcarat troyounce/151.5 # Originally intended to be 4 grain |
| 3696 | # but this value ended up being |
| 3697 | # used in the London diamond market |
| 3698 | mancus 2 oz |
| 3699 | mast 2.5 lb |
| 3700 | nailkeg 100 lbs |
| 3701 | basebox 31360 in^2 # Used in metal plating |
| 3702 | |
| 3703 | # alternate spellings |
| 3704 | |
| 3705 | gramme gram |
| 3706 | litre liter |
| 3707 | dioptre diopter |
| 3708 | sulphur sulfur |
| 3709 | |
| 3710 | # |
| 3711 | # Units derived the human body (may not be very accurate) |
| 3712 | # |
| 3713 | |
| 3714 | geometricpace 5 ft # distance between points where the same |
| 3715 | # foot hits the ground |
| 3716 | pace 2.5 ft # distance between points where alternate |
| 3717 | # feet touch the ground |
| 3718 | USmilitarypace 30 in # United States official military pace |
| 3719 | USdoubletimepace 36 in # United States official doubletime pace |
| 3720 | fingerbreadth 7|8 in # The finger is defined as either the width |
| 3721 | fingerlength 4.5 in # or length of the finger |
| 3722 | finger fingerbreadth |
| 3723 | palmwidth hand # The palm is a unit defined as either the width |
| 3724 | palmlength 8 in # or the length of the hand |
| 3725 | hand 4 inch # width of hand |
| 3726 | shaftment 6 inch # Distance from tip of outstretched thumb to the |
| 3727 | # opposite side of the palm of the hand. The |
| 3728 | # ending -ment is from the old English word |
| 3729 | # for hand. [18] |
| 3730 | smoot 5 ft + 7 in # Created as part of an MIT fraternity prank. |
| 3731 | # In 1958 Oliver Smoot was used to measure |
| 3732 | # the length of the Harvard Bridge, which was |
| 3733 | # marked off in Smoot lengths. These |
| 3734 | # markings have been maintained on the bridge |
| 3735 | # since then and repainted by subsequent |
| 3736 | # incoming fraternity members. During a |
| 3737 | # bridge renovation the new sidewalk was |
| 3738 | # scored every Smoot rather than at the |
| 3739 | # customary 6 ft spacing. |
| 3740 | tomcruise 5 ft + 7.75 in # Height of Tom Cruise |
| 3741 | |
| 3742 | # |
| 3743 | # Cooking measures |
| 3744 | # |
| 3745 | |
| 3746 | # Common abbreviations |
| 3747 | |
| 3748 | tbl tablespoon |
| 3749 | tbsp tablespoon |
| 3750 | tblsp tablespoon |
| 3751 | Tb tablespoon |
| 3752 | tsp teaspoon |
| 3753 | saltspoon 1|4 tsp |
| 3754 | |
| 3755 | # US measures |
| 3756 | |
| 3757 | uscup 8 usfloz |
| 3758 | ustablespoon 1|16 uscup |
| 3759 | usteaspoon 1|3 ustablespoon |
| 3760 | ustbl ustablespoon |
| 3761 | ustbsp ustablespoon |
| 3762 | ustblsp ustablespoon |
| 3763 | ustsp usteaspoon |
| 3764 | metriccup 250 ml |
| 3765 | stickbutter 1|4 lb # Butter in the USA is sold in one |
| 3766 | # pound packages that contain four |
| 3767 | # individually wrapped pieces. The |
| 3768 | # pieces are marked into tablespoons, |
| 3769 | # making it possible to measure out |
| 3770 | # butter by volume by slicing the |
| 3771 | # butter. |
| 3772 | |
| 3773 | legalcup 240 ml # The cup used on nutrition labeling |
| 3774 | legaltablespoon 1|16 legalcup |
| 3775 | legaltbsp legaltablespoon |
| 3776 | |
| 3777 | # Scoop size. Ice cream scoops in the US are marked with numbers |
| 3778 | # indicating the number of scoops required to fill a US quart. |
| 3779 | |
| 3780 | scoop(n) units=[1;cup] domain=[4,100] range=[0.04,1] \ |
| 3781 | 32 usfloz / n ; 32 usfloz / scoop |
| 3782 | |
| 3783 | |
| 3784 | # US can sizes. |
| 3785 | |
| 3786 | number1can 10 usfloz |
| 3787 | number2can 19 usfloz |
| 3788 | number2.5can 3.5 uscups |
| 3789 | number3can 4 uscups |
| 3790 | number5can 7 uscups |
| 3791 | number10can 105 usfloz |
| 3792 | |
| 3793 | # British measures |
| 3794 | |
| 3795 | brcup 1|2 brpint |
| 3796 | brteacup 1|3 brpint |
| 3797 | brtablespoon 15 ml # Also 5|8 brfloz, approx 17.7 ml |
| 3798 | brteaspoon 1|3 brtablespoon # Also 1|4 brtablespoon |
| 3799 | brdessertspoon 2 brteaspoon |
| 3800 | dessertspoon brdessertspoon |
| 3801 | dsp dessertspoon |
| 3802 | brtsp brteaspoon |
| 3803 | brtbl brtablespoon |
| 3804 | brtbsp brtablespoon |
| 3805 | brtblsp brtablespoon |
| 3806 | |
| 3807 | # Australian |
| 3808 | |
| 3809 | australiatablespoon 20 ml |
| 3810 | austbl australiatablespoon |
| 3811 | austbsp australiatablespoon |
| 3812 | austblsp australiatablespoon |
| 3813 | australiateaspoon 1|4 australiatablespoon |
| 3814 | austsp australiateaspoon |
| 3815 | |
| 3816 | # Italian |
| 3817 | |
| 3818 | etto 100 g # Used for buying items like meat and |
| 3819 | etti etto # cheese. |
| 3820 | |
| 3821 | # Chinese |
| 3822 | |
| 3823 | catty 0.5 kg |
| 3824 | oldcatty 4|3 lbs # Before metric conversion. |
| 3825 | tael 1|16 oldcatty # Should the tael be defined both ways? |
| 3826 | mace 0.1 tael |
| 3827 | oldpicul 100 oldcatty |
| 3828 | picul 100 catty # Chinese usage |
| 3829 | |
| 3830 | # Indian |
| 3831 | |
| 3832 | seer 14400 grain # British Colonial standard |
| 3833 | ser seer |
| 3834 | maund 40 seer |
| 3835 | pakistanseer 1 kg |
| 3836 | pakistanmaund 40 pakistanseer |
| 3837 | chittak 1|16 seer |
| 3838 | tola 1|5 chittak |
| 3839 | ollock 1|4 liter # Is this right? |
| 3840 | |
| 3841 | # Japanese |
| 3842 | |
| 3843 | japancup 200 ml |
| 3844 | |
| 3845 | # densities of cooking ingredients from The Cake Bible by Rose Levy Beranbaum |
| 3846 | # so you can convert '2 cups sugar' to grams, for example, or in the other |
| 3847 | # direction grams could be converted to 'cup flour_scooped'. |
| 3848 | |
| 3849 | butter 8 oz/uscup |
| 3850 | butter_clarified 6.8 oz/uscup |
| 3851 | cocoa_butter 9 oz/uscup |
| 3852 | shortening 6.75 oz/uscup # vegetable shortening |
| 3853 | oil 7.5 oz/uscup |
| 3854 | cakeflour_sifted 3.5 oz/uscup # The density of flour depends on the |
| 3855 | cakeflour_spooned 4 oz/uscup # measuring method. "Scooped", or |
| 3856 | cakeflour_scooped 4.5 oz/uscup # "dip and sweep" refers to dipping a |
| 3857 | flour_sifted 4 oz/uscup # measure into a bin, and then sweeping |
| 3858 | flour_spooned 4.25 oz/uscup # the excess off the top. "Spooned" |
| 3859 | flour_scooped 5 oz/uscup # means to lightly spoon into a measure |
| 3860 | breadflour_sifted 4.25 oz/uscup # and then sweep the top. Sifted means |
| 3861 | breadflour_spooned 4.5 oz/uscup # sifting the flour directly into a |
| 3862 | breadflour_scooped 5.5 oz/uscup # measure and then sweeping the top. |
| 3863 | cornstarch 120 grams/uscup |
| 3864 | dutchcocoa_sifted 75 g/uscup # These are for Dutch processed cocoa |
| 3865 | dutchcocoa_spooned 92 g/uscup |
| 3866 | dutchcocoa_scooped 95 g/uscup |
| 3867 | cocoa_sifted 75 g/uscup # These are for nonalkalized cocoa |
| 3868 | cocoa_spooned 82 g/uscup |
| 3869 | cocoa_scooped 95 g/uscup |
| 3870 | heavycream 232 g/uscup |
| 3871 | milk 242 g/uscup |
| 3872 | sourcream 242 g/uscup |
| 3873 | molasses 11.25 oz/uscup |
| 3874 | cornsyrup 11.5 oz/uscup |
| 3875 | honey 11.75 oz/uscup |
| 3876 | sugar 200 g/uscup |
| 3877 | powdered_sugar 4 oz/uscup |
| 3878 | brownsugar_light 217 g/uscup # packed |
| 3879 | brownsugar_dark 239 g/uscup |
| 3880 | |
| 3881 | baking_powder 4.6 grams / ustsp |
| 3882 | salt 6 g / ustsp |
| 3883 | koshersalt 2.8 g / ustsp # Diamond Crystal kosher salt |
| 3884 | koshersalt_morton 4.8 g / ustsp # Morton kosher salt |
| 3885 | # Values are from the nutrition info |
| 3886 | # on the packages |
| 3887 | |
| 3888 | |
| 3889 | # Egg weights and volumes for a USA large egg |
| 3890 | |
| 3891 | egg 50 grams # without shell |
| 3892 | eggwhite 30 grams |
| 3893 | eggyolk 18.6 grams |
| 3894 | eggvolume 3 ustablespoons + 1|2 ustsp |
| 3895 | eggwhitevolume 2 ustablespoons |
| 3896 | eggyolkvolume 3.5 ustsp |
| 3897 | |
| 3898 | # Alcohol density |
| 3899 | |
| 3900 | ethanoldensity 0.7893 g/cm^3 # From CRC Handbook, 91st Edition |
| 3901 | alcoholdensity ethanoldensity |
| 3902 | |
| 3903 | # |
| 3904 | # Density measures. Density has traditionally been measured on a variety of |
| 3905 | # bizarre nonlinear scales. |
| 3906 | # |
| 3907 | |
| 3908 | # Density of a sugar syrup is frequently measured in candy making procedures. |
| 3909 | # In the USA the boiling point of the syrup is measured. Some recipes instead |
| 3910 | # specify the density using degrees Baume. Conversion between degrees Baume |
| 3911 | # and the boiling point measure has proved elusive. This table appeared in one |
| 3912 | # text, and provides a fragmentary relationship to the concentration. |
| 3913 | # |
| 3914 | # temp(C) conc (%) |
| 3915 | # 100 30 |
| 3916 | # 101 40 |
| 3917 | # 102 50 |
| 3918 | # 103 60 |
| 3919 | # 106 70 |
| 3920 | # 112 80 |
| 3921 | # 123 90 |
| 3922 | # 140 95 |
| 3923 | # 151 97 |
| 3924 | # 160 98.2 |
| 3925 | # 166 99.5 |
| 3926 | # 171 99.6 |
| 3927 | # |
| 3928 | # The best source identified to date came from "Boiling point elevation of |
| 3929 | # technical sugarcane solutions and its use in automatic pan boiling" by |
| 3930 | # Michael Saska. International Sugar Journal, 2002, 104, 1247, pp 500-507. |
| 3931 | # |
| 3932 | # But I'm using equation (3) which is credited to Starzak and Peacock, |
| 3933 | # "Water activity coefficient in aqueous solutions of sucrose--A comprehensive |
| 3934 | # data analysis. Zuckerindustrie, 122, 380-387. (I couldn't find this |
| 3935 | # document.) |
| 3936 | # |
| 3937 | # Note that the range of validity is uncertain, but answers are in agreement |
| 3938 | # with the above table all the way to 99.6. |
| 3939 | # |
| 3940 | # The original equation has a parameter for the boiling point of water, which |
| 3941 | # of course varies with altitude. It also includes various other model |
| 3942 | # parameters. The input is the molar concentration of sucrose in the solution, |
| 3943 | # (moles sucrose) / (total moles). |
| 3944 | # |
| 3945 | # Bsp 3797.06 degC |
| 3946 | # Csp 226.28 degC |
| 3947 | # QQ -17638 J/mol |
| 3948 | # asp -1.0038 |
| 3949 | # bsp -0.24653 |
| 3950 | # tbw 100 degC # boiling point of water |
| 3951 | # sugar_bpe_orig(x) ((1-QQ/R Bsp * x^2 (1+asp x + bsp x^2) (tbw + Csp) \ |
| 3952 | # /(tbw+stdtemp)) / (1+(tbw + Csp)/Bsp *ln(1-x))-1) * (tbw + Csp) |
| 3953 | # |
| 3954 | # To convert mass concentration (brix) to molar concentration |
| 3955 | # |
| 3956 | # sc(x) (x / 342.3) / (( x/342.3) + (100-x)/18.02); \ |
| 3957 | # 100 sc 342.3|18.02 / (sc (342.3|18.02-1)+1) |
| 3958 | # |
| 3959 | # Here is a simplified version of this equation where the temperature of boiling |
| 3960 | # water has been fixed at 100 degrees Celsius and the argument is now the |
| 3961 | # concentration (brix). |
| 3962 | # |
| 3963 | # sugar_bpe(x) ((1+ 0.48851085 * sc(x)^2 (1+ -1.0038 sc(x) + -0.24653 sc(x)^2)) \ |
| 3964 | # / (1+0.08592964 ln(1-sc(x)))-1) 326.28 K |
| 3965 | # |
| 3966 | # |
| 3967 | # The formula is not invertible, so to implement it in units we unfortunately |
| 3968 | # must turn it into a table. |
| 3969 | |
| 3970 | # This table gives the boiling point elevation as a function of the sugar syrup |
| 3971 | # concentration expressed as a percentage. |
| 3972 | |
| 3973 | sugar_conc_bpe[K] \ |
| 3974 | 0 0.0000 5 0.0788 10 0.1690 15 0.2729 20 0.3936 25 0.5351 \ |
| 3975 | 30 0.7027 35 0.9036 40 1.1475 42 1.2599 44 1.3825 46 1.5165 \ |
| 3976 | 48 1.6634 50 1.8249 52 2.0031 54 2.2005 56 2.4200 58 2.6651 \ |
| 3977 | 60 2.9400 61 3.0902 62 3.2499 63 3.4198 64 3.6010 65 3.7944 \ |
| 3978 | 66 4.0012 67 4.2227 68 4.4603 69 4.7156 70 4.9905 71 5.2870 \ |
| 3979 | 72 5.6075 73 5.9546 74 6.3316 75 6.7417 76 7.1892 77 7.6786 \ |
| 3980 | 78.0 8.2155 79.0 8.8061 80.0 9.4578 80.5 9.8092 81.0 10.1793 \ |
| 3981 | 81.5 10.5693 82.0 10.9807 82.5 11.4152 83.0 11.8743 83.5 12.3601 \ |
| 3982 | 84.0 12.8744 84.5 13.4197 85.0 13.9982 85.5 14.6128 86.0 15.2663 \ |
| 3983 | 86.5 15.9620 87.0 16.7033 87.5 17.4943 88.0 18.3391 88.5 19.2424 \ |
| 3984 | 89.0 20.2092 89.5 21.2452 90.0 22.3564 90.5 23.5493 91.0 24.8309 \ |
| 3985 | 91.5 26.2086 92.0 27.6903 92.5 29.2839 93.0 30.9972 93.5 32.8374 \ |
| 3986 | 94.0 34.8104 94.5 36.9195 95.0 39.1636 95.5 41.5348 96.0 44.0142 \ |
| 3987 | 96.5 46.5668 97.0 49.1350 97.5 51.6347 98.0 53.9681 98.1 54.4091 \ |
| 3988 | 98.2 54.8423 98.3 55.2692 98.4 55.6928 98.5 56.1174 98.6 56.5497 \ |
| 3989 | 98.7 56.9999 98.8 57.4828 98.9 58.0206 99.0 58.6455 99.1 59.4062 \ |
| 3990 | 99.2 60.3763 99.3 61.6706 99.4 63.4751 99.5 66.1062 99.6 70.1448 \ |
| 3991 | 99.7 76.7867 |
| 3992 | |
| 3993 | # Using the brix table we can use this to produce a mapping from boiling point |
| 3994 | # to density which makes all of the units interconvertible. Because the brix |
| 3995 | # table stops at 95 this approach works up to a boiling point elevation of 39 K |
| 3996 | # or a boiling point of 139 C / 282 F, which is the "soft crack" stage in candy |
| 3997 | # making. The "hard crack" stage continues up to 310 F. |
| 3998 | |
| 3999 | # Boiling point elevation |
| 4000 | sugar_bpe(T) units=[K;g/cm^3] domain=[0,39.1636] range=[0.99717,1.5144619] \ |
| 4001 | brix(~sugar_conc_bpe(T)); sugar_conc_bpe(~brix(sugar_bpe)) |
| 4002 | # Absolute boiling point (produces an absolute temperature) |
| 4003 | sugar_bp(T) units=[K;g/cm^3] domain=[373.15,412.3136] \ |
| 4004 | range=[0.99717,1.5144619] \ |
| 4005 | brix(~sugar_conc_bpe(T-tempC(100))) ;\ |
| 4006 | sugar_conc_bpe(~brix(sugar_bp))+tempC(100) |
| 4007 | |
| 4008 | # In practice dealing with the absolute temperature is annoying because it is |
| 4009 | # not possible to convert to a nested function, so you're stuck retyping the |
| 4010 | # absolute temperature in Kelvins to convert to celsius or Fahrenheit. To |
| 4011 | # prevent this we supply definitions that build in the temperature conversion |
| 4012 | # and produce results in the Fahrenheit and Celsius scales. So using these |
| 4013 | # measures, to convert 46 degrees Baume to a Fahrenheit boiling point: |
| 4014 | # |
| 4015 | # You have: baume(45) |
| 4016 | # You want: sugar_bpF |
| 4017 | # 239.05647 |
| 4018 | # |
| 4019 | sugar_bpF(T) units=[1;g/cm^3] domain=[212,282.49448] range=[0.99717,1.5144619]\ |
| 4020 | brix(~sugar_conc_bpe(tempF(T)+-tempC(100))) ;\ |
| 4021 | ~tempF(sugar_conc_bpe(~brix(sugar_bpF))+tempC(100)) |
| 4022 | sugar_bpC(T) units=[1;g/cm^3] domain=[100,139.1636] range=[0.99717,1.5144619]\ |
| 4023 | brix(~sugar_conc_bpe(tempC(T)+-tempC(100))) ;\ |
| 4024 | ~tempC(sugar_conc_bpe(~brix(sugar_bpC))+tempC(100)) |
| 4025 | |
| 4026 | # Degrees Baume is used in European recipes to specify the density of a sugar |
| 4027 | # syrup. An entirely different definition is used for densities below |
| 4028 | # 1 g/cm^3. An arbitrary constant appears in the definition. This value is |
| 4029 | # equal to 145 in the US, but was according to [], the old scale used in |
| 4030 | # Holland had a value of 144, and the new scale or Gerlach scale used 146.78. |
| 4031 | |
| 4032 | baumeconst 145 # US value |
| 4033 | baume(d) units=[1;g/cm^3] domain=[0,145) range=[1,) \ |
| 4034 | (baumeconst/(baumeconst+-d)) g/cm^3 ; \ |
| 4035 | (baume+((-g)/cm^3)) baumeconst / baume |
| 4036 | |
| 4037 | # It's not clear if this value was ever used with negative degrees. |
| 4038 | twaddell(x) units=[1;g/cm^3] domain=[-200,) range=[0,) \ |
| 4039 | (1 + 0.005 x) g / cm^3 ; \ |
| 4040 | 200 (twaddell / (g/cm^3) +- 1) |
| 4041 | |
| 4042 | # The degree quevenne is a unit for measuring the density of milk. |
| 4043 | # Similarly it's unclear if negative values were allowed here. |
| 4044 | quevenne(x) units=[1;g/cm^3] domain=[-1000,) range=[0,) \ |
| 4045 | (1 + 0.001 x) g / cm^3 ; \ |
| 4046 | 1000 (quevenne / (g/cm^3) +- 1) |
| 4047 | |
| 4048 | # Degrees brix measures sugar concentration by weigh as a percentage, so a |
| 4049 | # solution that is 3 degrees brix is 3% sugar by weight. This unit was named |
| 4050 | # after Adolf Brix who invented a hydrometer that read this percentage |
| 4051 | # directly. This data is from Table 114 of NIST Circular 440, "Polarimetry, |
| 4052 | # Saccharimetry and the Sugars". It gives apparent specific gravity at 20 |
| 4053 | # degrees Celsius of various sugar concentrations. As rendered below this |
| 4054 | # data is converted to apparent density at 20 degrees Celsius using the |
| 4055 | # density figure for water given in the same NIST reference. They use the |
| 4056 | # word "apparent" to refer to measurements being made in air with brass |
| 4057 | # weights rather than vacuum. |
| 4058 | |
| 4059 | brix[0.99717g/cm^3]\ |
| 4060 | 0 1.00000 1 1.00390 2 1.00780 3 1.01173 4 1.01569 5 1.01968 \ |
| 4061 | 6 1.02369 7 1.02773 8 1.03180 9 1.03590 10 1.04003 11 1.04418 \ |
| 4062 | 12 1.04837 13 1.05259 14 1.05683 15 1.06111 16 1.06542 17 1.06976 \ |
| 4063 | 18 1.07413 19 1.07853 20 1.08297 21 1.08744 22 1.09194 23 1.09647 \ |
| 4064 | 24 1.10104 25 1.10564 26 1.11027 27 1.11493 28 1.11963 29 1.12436 \ |
| 4065 | 30 1.12913 31 1.13394 32 1.13877 33 1.14364 34 1.14855 35 1.15350 \ |
| 4066 | 36 1.15847 37 1.16349 38 1.16853 39 1.17362 40 1.17874 41 1.18390 \ |
| 4067 | 42 1.18910 43 1.19434 44 1.19961 45 1.20491 46 1.21026 47 1.21564 \ |
| 4068 | 48 1.22106 49 1.22652 50 1.23202 51 1.23756 52 1.24313 53 1.24874 \ |
| 4069 | 54 1.25439 55 1.26007 56 1.26580 57 1.27156 58 1.27736 59 1.28320 \ |
| 4070 | 60 1.28909 61 1.29498 62 1.30093 63 1.30694 64 1.31297 65 1.31905 \ |
| 4071 | 66 1.32516 67 1.33129 68 1.33748 69 1.34371 70 1.34997 71 1.35627 \ |
| 4072 | 72 1.36261 73 1.36900 74 1.37541 75 1.38187 76 1.38835 77 1.39489 \ |
| 4073 | 78 1.40146 79 1.40806 80 1.41471 81 1.42138 82 1.42810 83 1.43486 \ |
| 4074 | 84 1.44165 85 1.44848 86 1.45535 87 1.46225 88 1.46919 89 1.47616 \ |
| 4075 | 90 1.48317 91 1.49022 92 1.49730 93 1.50442 94 1.51157 95 1.51876 |
| 4076 | |
| 4077 | # Density measure invented by the American Petroleum Institute. Lighter |
| 4078 | # petroleum products are more valuable, and they get a higher API degree. |
| 4079 | # |
| 4080 | # The intervals of range and domain should be open rather than closed. |
| 4081 | # |
| 4082 | apidegree(x) units=[1;g/cm^3] domain=[-131.5,) range=[0,) \ |
| 4083 | 141.5 g/cm^3 / (x+131.5) ; \ |
| 4084 | 141.5 (g/cm^3) / apidegree + (-131.5) |
| 4085 | # |
| 4086 | # Average densities of various woods (dried) |
| 4087 | # Data from The Wood Database https://www.wood-database.com |
| 4088 | # |
| 4089 | |
| 4090 | # North American Hardwoods |
| 4091 | |
| 4092 | wood_cherry 35 lb/ft^3 |
| 4093 | wood_redoak 44 lb/ft^3 |
| 4094 | wood_whiteoak 47 lb/ft^3 |
| 4095 | wood_blackwalnut 38 lb/ft^3 |
| 4096 | wood_walnut wood_blackwalnut |
| 4097 | wood_birch 43 lb/ft^3 |
| 4098 | wood_hardmaple 44 lb/ft^3 |
| 4099 | |
| 4100 | wood_bigleafmaple 34 lb/ft^3 |
| 4101 | wood_boxeldermaple 30 lb/ft^3 |
| 4102 | wood_redmaple 38 lb/ft^3 |
| 4103 | wood_silvermaple 33 lb/ft^3 |
| 4104 | wood_stripedmaple 32 lb/ft^3 |
| 4105 | wood_softmaple (wood_bigleafmaple \ |
| 4106 | + wood_boxeldermaple \ |
| 4107 | + wood_redmaple \ |
| 4108 | + wood_silvermaple \ |
| 4109 | + wood_stripedmaple) / 5 |
| 4110 | wood_poplar 29 lb/ft^3 |
| 4111 | wood_beech 45 lb/ft^3 |
| 4112 | |
| 4113 | # North American Softwoods |
| 4114 | |
| 4115 | wood_jeffreypine 28 lb/ft^3 |
| 4116 | wood_ocotepine 44 lb/ft^3 |
| 4117 | wood_ponderosapine 28 lb/ft^3 |
| 4118 | |
| 4119 | wood_loblollypine 35 lb/ft^3 |
| 4120 | wood_longleafpine 41 lb/ft^3 |
| 4121 | wood_shortleafpine 35 lb/ft^3 |
| 4122 | wood_slashpine 41 lb/ft^3 |
| 4123 | wood_yellowpine (wood_loblollypine \ |
| 4124 | + wood_longleafpine \ |
| 4125 | + wood_shortleafpine \ |
| 4126 | + wood_slashpine) / 4 |
| 4127 | wood_redpine 34 lb/ft^3 |
| 4128 | |
| 4129 | wood_easternwhitepine 25 lb/ft^3 |
| 4130 | wood_westernwhitepine 27 lb/ft^3 |
| 4131 | wood_whitepine (wood_easternwhitepine + wood_westernwhitepine) / 2 |
| 4132 | |
| 4133 | wood_douglasfir 32 lb/ft^3 |
| 4134 | |
| 4135 | wood_blackspruce 28 lb/ft^3 |
| 4136 | wood_engelmannspruce 24 lb/ft^3 |
| 4137 | wood_redspruce 27 lb/ft^3 |
| 4138 | wood_sitkaspruce 27 lb/ft^3 |
| 4139 | wood_whitespruce 27 lb/ft^3 |
| 4140 | wood_spruce (wood_blackspruce \ |
| 4141 | + wood_engelmannspruce \ |
| 4142 | + wood_redspruce \ |
| 4143 | + wood_sitkaspruce \ |
| 4144 | + wood_whitespruce) / 5 |
| 4145 | |
| 4146 | # Other woods |
| 4147 | |
| 4148 | wood_basswood 26 lb/ft^3 |
| 4149 | wood_balsa 9 lb/ft^3 |
| 4150 | wood_ebony_gaboon 60 lb/ft^3 |
| 4151 | wood_ebony_macassar 70 lb/ft^3 |
| 4152 | wood_mahogany 37 lb/ft^3 # True (Honduran) mahogany, |
| 4153 | # Swietenia macrophylla |
| 4154 | wood_teak 41 lb/ft^3 |
| 4155 | wood_rosewood_brazilian 52 lb/ft^3 |
| 4156 | wood_rosewood_honduran 64 lb/ft^3 |
| 4157 | wood_rosewood_indian 52 lb/ft^3 |
| 4158 | wood_cocobolo 69 lb/ft^3 |
| 4159 | wood_bubinga 56 lb/ft^3 |
| 4160 | wood_zebrawood 50 lb/ft^3 |
| 4161 | wood_koa 38 lb/ft^3 |
| 4162 | wood_snakewood 75.7 lb/ft^3 |
| 4163 | wood_lignumvitae 78.5 lb/ft^3 |
| 4164 | wood_blackwood 79.3 lb/ft^3 |
| 4165 | wood_blackironwood 84.5 lb/ft^3 # Krugiodendron ferreum, listed |
| 4166 | # in database as the heaviest wood |
| 4167 | |
| 4168 | # |
| 4169 | # Modulus of elasticity of selected woods. |
| 4170 | # Data from The Wood Database https://www.wood-database.com |
| 4171 | # |
| 4172 | |
| 4173 | # North American Hardwoods |
| 4174 | |
| 4175 | wood_mod_beech 1.720e6 lbf/in^2 |
| 4176 | wood_mod_birchyellow 2.010e6 lbf/in^2 |
| 4177 | wood_mod_birch wood_mod_birchyellow |
| 4178 | wood_mod_cherry 1.490e6 lbf/in^2 |
| 4179 | wood_mod_hardmaple 1.830e6 lbf/in^2 |
| 4180 | |
| 4181 | wood_mod_bigleafmaple 1.450e6 lbf/in^2 |
| 4182 | wood_mod_boxeldermaple 1.050e6 lbf/in^2 |
| 4183 | wood_mod_redmaple 1.640e6 lbf/in^2 |
| 4184 | wood_mod_silvermaple 1.140e6 lbf/in^2 |
| 4185 | wood_mod_softmaple (wood_mod_bigleafmaple \ |
| 4186 | + wood_mod_boxeldermaple \ |
| 4187 | + wood_mod_redmaple \ |
| 4188 | + wood_mod_silvermaple) / 4 |
| 4189 | |
| 4190 | wood_mod_redoak 1.761e6 lbf/in^2 |
| 4191 | wood_mod_whiteoak 1.762e6 lbf/in^2 |
| 4192 | wood_mod_poplar 1.580e6 lbf/in^2 |
| 4193 | wood_mod_blackwalnut 1.680e6 lbf/in^2 |
| 4194 | wood_mod_walnut wood_mod_blackwalnut |
| 4195 | |
| 4196 | # North American Softwoods |
| 4197 | |
| 4198 | wood_mod_jeffreypine 1.240e6 lbf/in^2 |
| 4199 | wood_mod_ocotepine 2.209e6 lbf/in^2 |
| 4200 | wood_mod_ponderosapine 1.290e6 lbf/in^2 |
| 4201 | |
| 4202 | wood_mod_loblollypine 1.790e6 lbf/in^2 |
| 4203 | wood_mod_longleafpine 1.980e6 lbf/in^2 |
| 4204 | wood_mod_shortleafpine 1.750e6 lbf/in^2 |
| 4205 | wood_mod_slashpine 1.980e6 lbf/in^2 |
| 4206 | wood_mod_yellowpine (wood_mod_loblollypine \ |
| 4207 | + wood_mod_longleafpine \ |
| 4208 | + wood_mod_shortleafpine \ |
| 4209 | + wood_mod_slashpine) / 4 |
| 4210 | |
| 4211 | wood_mod_redpine 1.630e6 lbf/in^2 |
| 4212 | |
| 4213 | wood_mod_easternwhitepine 1.240e6 lbf/in^2 |
| 4214 | wood_mod_westernwhitepine 1.460e6 lbf/in^2 |
| 4215 | wood_mod_whitepine (wood_mod_easternwhitepine + \ |
| 4216 | wood_mod_westernwhitepine) / 2 |
| 4217 | |
| 4218 | wood_mod_douglasfir 1.765e6 lbf/in^2 |
| 4219 | |
| 4220 | wood_mod_blackspruce 1.523e6 lbf/in^2 |
| 4221 | wood_mod_englemannspruce 1.369e6 lbf/in^2 |
| 4222 | wood_mod_redspruce 1.560e6 lbf/in^2 |
| 4223 | wood_mod_sitkaspruce 1.600e6 lbf/in^2 |
| 4224 | wood_mod_whitespruce 1.315e6 lbf/in^2 |
| 4225 | wood_mod_spruce (wood_mod_blackspruce \ |
| 4226 | + wood_mod_englemannspruce \ |
| 4227 | + wood_mod_redspruce + wood_mod_sitkaspruce \ |
| 4228 | + wood_mod_whitespruce) / 5 |
| 4229 | |
| 4230 | # Other woods |
| 4231 | |
| 4232 | wood_mod_balsa 0.538e6 lbf/in^2 |
| 4233 | wood_mod_basswood 1.460e6 lbf/in^2 |
| 4234 | wood_mod_blackwood 2.603e6 lbf/in^2 # African, Dalbergia melanoxylon |
| 4235 | wood_mod_bubinga 2.670e6 lbf/in^2 |
| 4236 | wood_mod_cocobolo 2.712e6 lbf/in^2 |
| 4237 | wood_mod_ebony_gaboon 2.449e6 lbf/in^2 |
| 4238 | wood_mod_ebony_macassar 2.515e6 lbf/in^2 |
| 4239 | wood_mod_blackironwood 2.966e6 lbf/in^2 # Krugiodendron ferreum |
| 4240 | wood_mod_koa 1.503e6 lbf/in^2 |
| 4241 | wood_mod_lignumvitae 2.043e6 lbf/in^2 |
| 4242 | wood_mod_mahogany 1.458e6 lbf/in^2 # True (Honduran) mahogany, |
| 4243 | # Swietenia macrophylla |
| 4244 | wood_mod_rosewood_brazilian 2.020e6 lbf/in^2 |
| 4245 | wood_mod_rosewood_honduran 3.190e6 lbf/in^2 |
| 4246 | wood_mod_rosewood_indian 1.668e6 lbf/in^2 |
| 4247 | wood_mod_snakewood 3.364e6 lbf/in^2 |
| 4248 | wood_mod_teak 1.781e6 lbf/in^2 |
| 4249 | wood_mod_zebrawood 2.374e6 lbf/in^2 |
| 4250 | |
| 4251 | # |
| 4252 | # Area of countries and other regions. This is the "total area" which |
| 4253 | # includes land and water areas within international boundaries and |
| 4254 | # coastlines. Data from January, 2019. |
| 4255 | # |
| 4256 | # except as noted, sources are |
| 4257 | # https://en.wikipedia.org/wiki/List_of_countries_and_dependencies_by_area |
| 4258 | # US Central Intelligence Agency: The World Factbook |
| 4259 | # https://www.cia.gov/the-world-factbook/ |
| 4260 | |
| 4261 | area_russia 17098246 km^2 |
| 4262 | area_antarctica 14000000 km^2 |
| 4263 | # area_canada is covered below as sum of province and territory areas |
| 4264 | area_china 9596961 km^2 |
| 4265 | # area_unitedstates is covered below as sum of state areas |
| 4266 | # includes only the 50 states and District of Columbia |
| 4267 | area_us area_unitedstates |
| 4268 | area_brazil 8515767 km^2 |
| 4269 | area_australia 7692024 km^2 |
| 4270 | # area_europeanunion is covered below as sum of member areas |
| 4271 | area_india 3287263 km^2 |
| 4272 | area_argentina 2780400 km^2 |
| 4273 | area_kazakhstan 2724900 km^2 |
| 4274 | area_algeria 2381741 km^2 |
| 4275 | area_drcongo 2344858 km^2 |
| 4276 | area_greenland 2166086 km^2 |
| 4277 | area_saudiarabia 2149690 km^2 |
| 4278 | area_mexico 1964375 km^2 |
| 4279 | area_indonesia 1910931 km^2 |
| 4280 | area_sudan 1861484 km^2 |
| 4281 | area_libya 1759540 km^2 |
| 4282 | area_iran 1648195 km^2 |
| 4283 | area_mongolia 1564110 km^2 |
| 4284 | area_peru 1285216 km^2 |
| 4285 | area_chad 1284000 km^2 |
| 4286 | area_niger 1267000 km^2 |
| 4287 | area_angola 1246700 km^2 |
| 4288 | area_mali 1240192 km^2 |
| 4289 | area_southafrica 1221037 km^2 |
| 4290 | area_colombia 1141748 km^2 |
| 4291 | area_ethiopia 1104300 km^2 |
| 4292 | area_bolivia 1098581 km^2 |
| 4293 | area_mauritania 1030700 km^2 |
| 4294 | area_egypt 1002450 km^2 |
| 4295 | area_tanzania 945087 km^2 |
| 4296 | area_nigeria 923768 km^2 |
| 4297 | area_venezuela 916445 km^2 |
| 4298 | area_pakistan 881912 km^2 |
| 4299 | area_namibia 825615 km^2 |
| 4300 | area_mozambique 801590 km^2 |
| 4301 | area_turkey 783562 km^2 |
| 4302 | area_chile 756102 km^2 |
| 4303 | area_zambia 752612 km^2 |
| 4304 | area_myanmar 676578 km^2 |
| 4305 | area_burma area_myanmar |
| 4306 | area_afghanistan 652230 km^2 |
| 4307 | area_southsudan 644329 km^2 |
| 4308 | area_france 640679 km^2 |
| 4309 | area_somalia 637657 km^2 |
| 4310 | area_centralafrica 622984 km^2 |
| 4311 | area_ukraine 603500 km^2 |
| 4312 | area_crimea 27000 km^2 # occupied by Russia; included in |
| 4313 | # (Encyclopedia Britannica) |
| 4314 | area_madagascar 587041 km^2 |
| 4315 | area_botswana 581730 km^2 |
| 4316 | area_kenya 580367 km^2 |
| 4317 | area_yemen 527968 km^2 |
| 4318 | area_thailand 513120 km^2 |
| 4319 | area_spain 505992 km^2 |
| 4320 | area_turkmenistan 488100 km^2 |
| 4321 | area_cameroon 475422 km^2 |
| 4322 | area_papuanewguinea 462840 km^2 |
| 4323 | area_sweden 450295 km^2 |
| 4324 | area_uzbekistan 447400 km^2 |
| 4325 | area_morocco 446550 km^2 |
| 4326 | area_iraq 438317 km^2 |
| 4327 | area_paraguay 406752 km^2 |
| 4328 | area_zimbabwe 390757 km^2 |
| 4329 | area_japan 377973 km^2 |
| 4330 | area_germany 357114 km^2 |
| 4331 | area_congorepublic 342000 km^2 |
| 4332 | area_finland 338424 km^2 |
| 4333 | area_vietnam 331212 km^2 |
| 4334 | area_malaysia 330803 km^2 |
| 4335 | area_norway 323802 km^2 |
| 4336 | area_ivorycoast 322463 km^2 |
| 4337 | area_poland 312696 km^2 |
| 4338 | area_oman 309500 km^2 |
| 4339 | area_italy 301339 km^2 |
| 4340 | area_philippines 300000 km^2 |
| 4341 | area_ecuador 276841 km^2 |
| 4342 | area_burkinafaso 274222 km^2 |
| 4343 | area_newzealand 270467 km^2 |
| 4344 | area_gabon 267668 km^2 |
| 4345 | area_westernsahara 266000 km^2 |
| 4346 | area_guinea 245857 km^2 |
| 4347 | # area_unitedkingdom is covered below |
| 4348 | area_uganda 241550 km^2 |
| 4349 | area_ghana 238533 km^2 |
| 4350 | area_romania 238397 km^2 |
| 4351 | area_laos 236800 km^2 |
| 4352 | area_guyana 214969 km^2 |
| 4353 | area_belarus 207600 km^2 |
| 4354 | area_kyrgyzstan 199951 km^2 |
| 4355 | area_senegal 196722 km^2 |
| 4356 | area_syria 185180 km^2 |
| 4357 | area_golanheights 1150 km^2 # occupied by Israel; included in |
| 4358 | # Syria (Encyclopedia Britannica) |
| 4359 | area_cambodia 181035 km^2 |
| 4360 | area_uruguay 176215 km^2 |
| 4361 | area_somaliland 176120 km^2 |
| 4362 | area_suriname 163820 km^2 |
| 4363 | area_tunisia 163610 km^2 |
| 4364 | area_bangladesh 147570 km^2 |
| 4365 | area_nepal 147181 km^2 |
| 4366 | area_tajikistan 143100 km^2 |
| 4367 | area_greece 131990 km^2 |
| 4368 | area_nicaragua 130373 km^2 |
| 4369 | area_northkorea 120540 km^2 |
| 4370 | area_malawi 118484 km^2 |
| 4371 | area_eritrea 117600 km^2 |
| 4372 | area_benin 114763 km^2 |
| 4373 | area_honduras 112492 km^2 |
| 4374 | area_liberia 111369 km^2 |
| 4375 | area_bulgaria 110879 km^2 |
| 4376 | area_cuba 109884 km^2 |
| 4377 | area_guatemala 108889 km^2 |
| 4378 | area_iceland 103000 km^2 |
| 4379 | area_southkorea 100210 km^2 |
| 4380 | area_hungary 93028 km^2 |
| 4381 | area_portugal 92090 km^2 |
| 4382 | area_jordan 89342 km^2 |
| 4383 | area_serbia 88361 km^2 |
| 4384 | area_azerbaijan 86600 km^2 |
| 4385 | area_austria 83871 km^2 |
| 4386 | area_uae 83600 km^2 |
| 4387 | area_czechia 78865 km^2 |
| 4388 | area_czechrepublic area_czechia |
| 4389 | area_panama 75417 km^2 |
| 4390 | area_sierraleone 71740 km^2 |
| 4391 | area_ireland 70273 km^2 |
| 4392 | area_georgia 69700 km^2 |
| 4393 | area_srilanka 65610 km^2 |
| 4394 | area_lithuania 65300 km^2 |
| 4395 | area_latvia 64559 km^2 |
| 4396 | area_togo 56785 km^2 |
| 4397 | area_croatia 56594 km^2 |
| 4398 | area_bosnia 51209 km^2 |
| 4399 | area_costarica 51100 km^2 |
| 4400 | area_slovakia 49037 km^2 |
| 4401 | area_dominicanrepublic 48671 km^2 |
| 4402 | area_estonia 45227 km^2 |
| 4403 | area_denmark 43094 km^2 |
| 4404 | area_netherlands 41850 km^2 |
| 4405 | area_switzerland 41284 km^2 |
| 4406 | area_bhutan 38394 km^2 |
| 4407 | area_taiwan 36193 km^2 |
| 4408 | area_guineabissau 36125 km^2 |
| 4409 | area_moldova 33846 km^2 |
| 4410 | area_belgium 30528 km^2 |
| 4411 | area_lesotho 30355 km^2 |
| 4412 | area_armenia 29743 km^2 |
| 4413 | area_solomonislands 28896 km^2 |
| 4414 | area_albania 28748 km^2 |
| 4415 | area_equitorialguinea 28051 km^2 |
| 4416 | area_burundi 27834 km^2 |
| 4417 | area_haiti 27750 km^2 |
| 4418 | area_rwanda 26338 km^2 |
| 4419 | area_northmacedonia 25713 km^2 |
| 4420 | area_djibouti 23200 km^2 |
| 4421 | area_belize 22966 km^2 |
| 4422 | area_elsalvador 21041 km^2 |
| 4423 | area_israel 20770 km^2 |
| 4424 | area_slovenia 20273 km^2 |
| 4425 | area_fiji 18272 km^2 |
| 4426 | area_kuwait 17818 km^2 |
| 4427 | area_eswatini 17364 km^2 |
| 4428 | area_easttimor 14919 km^2 |
| 4429 | area_bahamas 13943 km^2 |
| 4430 | area_montenegro 13812 km^2 |
| 4431 | area_vanatu 12189 km^2 |
| 4432 | area_qatar 11586 km^2 |
| 4433 | area_gambia 11295 km^2 |
| 4434 | area_jamaica 10991 km^2 |
| 4435 | area_kosovo 10887 km^2 |
| 4436 | area_lebanon 10452 km^2 |
| 4437 | area_cyprus 9251 km^2 |
| 4438 | area_puertorico 9104 km^2 # United States territory; not included |
| 4439 | # in United States area |
| 4440 | area_westbank 5860 km^2 # (CIA World Factbook) |
| 4441 | area_hongkong 2755 km^2 |
| 4442 | area_luxembourg 2586 km^2 |
| 4443 | area_singapore 716 km^2 |
| 4444 | area_gazastrip 360 km^2 # (CIA World Factbook) |
| 4445 | area_malta 316 km^2 # smallest EU country |
| 4446 | area_liechtenstein 160 km^2 |
| 4447 | area_monaco 2.02 km^2 |
| 4448 | area_vaticancity 0.44 km^2 |
| 4449 | |
| 4450 | # Members as of 1 Feb 2020 |
| 4451 | area_europeanunion area_austria + area_belgium + area_bulgaria \ |
| 4452 | + area_croatia + area_cyprus + area_czechia + area_denmark \ |
| 4453 | + area_estonia + area_finland + area_france + area_germany \ |
| 4454 | + area_greece + area_hungary + area_ireland + area_italy \ |
| 4455 | + area_latvia + area_lithuania + area_luxembourg \ |
| 4456 | + area_malta + area_netherlands + area_poland \ |
| 4457 | + area_portugal + area_romania + area_slovakia \ |
| 4458 | + area_slovenia + area_spain + area_sweden |
| 4459 | area_eu area_europeanunion |
| 4460 | |
| 4461 | # |
| 4462 | # Areas of the individual US states |
| 4463 | # |
| 4464 | # https://en.wikipedia.org/wiki/List_of_U.S._states_and_territories_by_area |
| 4465 | # |
| 4466 | # United States Summary: 2010, Population and Housing Unit Counts, Table 18, p. 41 |
| 4467 | # Issued September 2012 |
| 4468 | |
| 4469 | area_alaska 1723336.8 km^2 |
| 4470 | area_texas 695661.6 km^2 |
| 4471 | area_california 423967.4 km^2 |
| 4472 | area_montana 380831.1 km^2 |
| 4473 | area_newmexico 314917.4 km^2 |
| 4474 | area_arizona 295233.5 km^2 |
| 4475 | area_nevada 286379.7 km^2 |
| 4476 | area_colorado 269601.4 km^2 |
| 4477 | area_oregon 254799.2 km^2 |
| 4478 | area_wyoming 253334.5 km^2 |
| 4479 | area_michigan 250486.8 km^2 |
| 4480 | area_minnesota 225162.8 km^2 |
| 4481 | area_utah 219881.9 km^2 |
| 4482 | area_idaho 216442.6 km^2 |
| 4483 | area_kansas 213100.0 km^2 |
| 4484 | area_nebraska 200329.9 km^2 |
| 4485 | area_southdakota 199728.7 km^2 |
| 4486 | area_washington 184660.8 km^2 |
| 4487 | area_northdakota 183107.8 km^2 |
| 4488 | area_oklahoma 181037.2 km^2 |
| 4489 | area_missouri 180540.3 km^2 |
| 4490 | area_florida 170311.7 km^2 |
| 4491 | area_wisconsin 169634.8 km^2 |
| 4492 | area_georgia_us 153910.4 km^2 |
| 4493 | area_illinois 149995.4 km^2 |
| 4494 | area_iowa 145745.9 km^2 |
| 4495 | area_newyork 141296.7 km^2 |
| 4496 | area_northcarolina 139391.0 km^2 |
| 4497 | area_arkansas 137731.8 km^2 |
| 4498 | area_alabama 135767.4 km^2 |
| 4499 | area_louisiana 135658.7 km^2 |
| 4500 | area_mississippi 125437.7 km^2 |
| 4501 | area_pennsylvania 119280.2 km^2 |
| 4502 | area_ohio 116097.7 km^2 |
| 4503 | area_virginia 110786.6 km^2 |
| 4504 | area_tennessee 109153.1 km^2 |
| 4505 | area_kentucky 104655.7 km^2 |
| 4506 | area_indiana 94326.2 km^2 |
| 4507 | area_maine 91633.1 km^2 |
| 4508 | area_southcarolina 82932.7 km^2 |
| 4509 | area_westvirginia 62755.5 km^2 |
| 4510 | area_maryland 32131.2 km^2 |
| 4511 | area_hawaii 28313.0 km^2 |
| 4512 | area_massachusetts 27335.7 km^2 |
| 4513 | area_vermont 24906.3 km^2 |
| 4514 | area_newhampshire 24214.2 km^2 |
| 4515 | area_newjersey 22591.4 km^2 |
| 4516 | area_connecticut 14357.4 km^2 |
| 4517 | area_delaware 6445.8 km^2 |
| 4518 | area_rhodeisland 4001.2 km^2 |
| 4519 | area_districtofcolumbia 177.0 km^2 |
| 4520 | |
| 4521 | area_unitedstates area_alabama + area_alaska + area_arizona \ |
| 4522 | + area_arkansas + area_california + area_colorado \ |
| 4523 | + area_connecticut + area_delaware \ |
| 4524 | + area_districtofcolumbia + area_florida \ |
| 4525 | + area_georgia_us + area_hawaii + area_idaho \ |
| 4526 | + area_illinois + area_indiana + area_iowa \ |
| 4527 | + area_kansas + area_kentucky + area_louisiana \ |
| 4528 | + area_maine + area_maryland + area_massachusetts \ |
| 4529 | + area_michigan + area_minnesota + area_mississippi \ |
| 4530 | + area_missouri + area_montana + area_nebraska \ |
| 4531 | + area_nevada + area_newhampshire + area_newjersey \ |
| 4532 | + area_newmexico + area_newyork + area_northcarolina \ |
| 4533 | + area_northdakota + area_ohio + area_oklahoma \ |
| 4534 | + area_oregon + area_pennsylvania + area_rhodeisland \ |
| 4535 | + area_southcarolina + area_southdakota \ |
| 4536 | + area_tennessee + area_texas + area_utah \ |
| 4537 | + area_vermont + area_virginia + area_washington \ |
| 4538 | + area_westvirginia + area_wisconsin + area_wyoming |
| 4539 | |
| 4540 | # Total area of Canadian province and territories |
| 4541 | # |
| 4542 | # Statistics Canada, "Land and freshwater area, by province and territory", |
| 4543 | # 2016-10-07: |
| 4544 | # |
| 4545 | # https://www150.statcan.gc.ca/n1/pub/11-402-x/2012000/chap/geo/tbl/tbl06-eng.htm |
| 4546 | |
| 4547 | area_ontario 1076395 km^2 # confederated 1867-Jul-01 |
| 4548 | area_quebec 1542056 km^2 # confederated 1867-Jul-01 |
| 4549 | area_novascotia 55284 km^2 # confederated 1867-Jul-01 |
| 4550 | area_newbrunswick 72908 km^2 # confederated 1867-Jul-01 |
| 4551 | area_canada_original area_ontario + area_quebec + area_novascotia \ |
| 4552 | + area_newbrunswick |
| 4553 | area_manitoba 647797 km^2 # confederated 1870-Jul-15 |
| 4554 | area_britishcolumbia 944735 km^2 # confederated 1871-Jul-20 |
| 4555 | area_princeedwardisland 5660 km^2 # confederated 1873-Jul-01 |
| 4556 | area_canada_additional area_manitoba + area_britishcolumbia \ |
| 4557 | + area_princeedwardisland |
| 4558 | area_alberta 661848 km^2 # confederated 1905-Sep-01 |
| 4559 | area_saskatchewan 651036 km^2 # confederated 1905-Sep-01 |
| 4560 | area_newfoundlandandlabrador 405212 km^2 # confederated 1949-Mar-31 |
| 4561 | area_canada_recent area_alberta + area_saskatchewan \ |
| 4562 | + area_newfoundlandandlabrador |
| 4563 | area_canada_provinces area_canada_original + area_canada_additional \ |
| 4564 | + area_canada_recent |
| 4565 | area_northwestterritories 1346106 km^2 # NT confederated 1870-Jul-15 |
| 4566 | area_yukon 482443 km^2 # YT confederated 1898-Jun-13 |
| 4567 | area_nunavut 2093190 km^2 # NU confederated 1999-Apr-01 |
| 4568 | area_canada_territories area_northwestterritories + area_yukon \ |
| 4569 | + area_nunavut |
| 4570 | area_canada area_canada_provinces + area_canada_territories |
| 4571 | |
| 4572 | # area-uk-countries.units - UK country (/province) total areas |
| 4573 | # https://en.wikipedia.org/wiki/Countries_of_the_United_Kingdom#Statistics |
| 4574 | # GB is official UK country code for some purposes but internally is a Kingdom |
| 4575 | # |
| 4576 | # areas from A Beginners Guide to UK Geography 2019 v1.0, Office for National Statistics |
| 4577 | # England: country; 0927-Jul-12 united; 1603-Mar-24 union of crowns |
| 4578 | area_england 132947.76 km^2 |
| 4579 | # |
| 4580 | # Wales: 1282 conquered; 1535 union; principality until 2011 |
| 4581 | area_wales 21224.48 km^2 |
| 4582 | # |
| 4583 | # England and Wales: nation; 1535 union |
| 4584 | area_englandwales area_england + area_wales |
| 4585 | # |
| 4586 | # Scotland: country; ~900 united; 1603-Mar-24 union of crowns |
| 4587 | area_scotland 80226.36 km^2 |
| 4588 | # |
| 4589 | # Great Britain: kingdom; excludes NI; |
| 4590 | # 1707 Treaty and Acts of Union: union of parliaments |
| 4591 | area_greatbritain area_england + area_wales + area_scotland |
| 4592 | area_gb area_greatbritain |
| 4593 | # |
| 4594 | # Northern Ireland: province; Ireland: 1177 Henry II lordship; |
| 4595 | # 1542 Henry VIII kingdom; 1652 Cromwell commonwealth; |
| 4596 | # 1691 William III kingdom; 1800 Acts of Union: UK of GB & Ireland; |
| 4597 | # 1921 Irish Free State independent of UK |
| 4598 | area_northernireland 14133.38 km^2 |
| 4599 | # |
| 4600 | # United Kingdom of GB & NI: 1800 Acts of Union: UK of GB & Ireland; |
| 4601 | # 1921 Irish Free State independent of UK |
| 4602 | area_unitedkingdom area_greatbritain + area_northernireland |
| 4603 | area_uk area_unitedkingdom |
| 4604 | |
| 4605 | # |
| 4606 | # Units derived from imperial system |
| 4607 | # |
| 4608 | |
| 4609 | ouncedal oz ft / s^2 # force which accelerates an ounce |
| 4610 | # at 1 ft/s^2 |
| 4611 | poundal lb ft / s^2 # same thing for a pound |
| 4612 | tondal longton ft / s^2 # and for a ton |
| 4613 | pdl poundal |
| 4614 | osi ounce force / inch^2 # used in aviation |
| 4615 | psi pound force / inch^2 |
| 4616 | psia psi # absolute pressure |
| 4617 | # Note that gauge pressure can be given |
| 4618 | # using the gaugepressure() and |
| 4619 | # psig() nonlinear unit definitions |
| 4620 | tsi ton force / inch^2 |
| 4621 | reyn psi sec |
| 4622 | slug lbf s^2 / ft |
| 4623 | slugf slug force |
| 4624 | slinch lbf s^2 / inch # Mass unit derived from inch second |
| 4625 | slinchf slinch force # pound-force system. Used in space |
| 4626 | # applications where in/sec^2 was a |
| 4627 | # natural acceleration measure. |
| 4628 | geepound slug |
| 4629 | lbf lb force |
| 4630 | tonf ton force |
| 4631 | lbm lb |
| 4632 | kip 1000 lbf # from kilopound |
| 4633 | ksi kip / in^2 |
| 4634 | mil 0.001 inch |
| 4635 | thou 0.001 inch |
| 4636 | tenth 0.0001 inch # one tenth of one thousandth of an inch |
| 4637 | millionth 1e-6 inch # one millionth of an inch |
| 4638 | circularinch 1|4 pi in^2 # area of a one-inch diameter circle |
| 4639 | circleinch circularinch # A circle with diameter d inches has |
| 4640 | # an area of d^2 circularinches |
| 4641 | cylinderinch circleinch inch # Cylinder h inch tall, d inches diameter |
| 4642 | # has volume d^2 h cylinder inches |
| 4643 | circularmil 1|4 pi mil^2 # area of one-mil diameter circle |
| 4644 | cmil circularmil |
| 4645 | cental 100 pound |
| 4646 | centner cental |
| 4647 | |
| 4648 | # Shotgun gauge measures the inside diameter of the barrel by counting |
| 4649 | # the number of spherical lead balls you can make to fit that barrel |
| 4650 | # using a pound of lead. Equivalently, this means that an n gauge gun |
| 4651 | # has a bore diameter that fits a ball of lead that weighs 1|n pounds |
| 4652 | |
| 4653 | shotgungauge(ga) units=[1;m] domain=(0,] range=(0,] \ |
| 4654 | 2 ~spherevol(1 pound / ga leaddensity) ; \ |
| 4655 | 1 pound / leaddensity spherevol(shotgungauge/2) |
| 4656 | shotgunga() shotgungauge |
| 4657 | caliber 0.01 inch # for measuring bullets |
| 4658 | |
| 4659 | duty ft lbf |
| 4660 | celo ft / s^2 |
| 4661 | jerk ft / s^3 |
| 4662 | australiapoint 0.01 inch # The "point" is used to measure rainfall |
| 4663 | # in Australia |
| 4664 | sabin ft^2 # Measure of sound absorption equal to the |
| 4665 | # absorbing power of one square foot of |
| 4666 | # a perfectly absorbing material. The |
| 4667 | # sound absorptivity of an object is the |
| 4668 | # area times a dimensionless |
| 4669 | # absorptivity coefficient. |
| 4670 | standardgauge 4 ft + 8.5 in # Standard width between railroad track |
| 4671 | flag 5 ft^2 # Construction term referring to sidewalk. |
| 4672 | rollwallpaper 30 ft^2 # Area of roll of wall paper |
| 4673 | fillpower in^3 / ounce # Density of down at standard pressure. |
| 4674 | # The best down has 750-800 fillpower. |
| 4675 | pinlength 1|16 inch # A #17 pin is 17/16 in long in the USA. |
| 4676 | buttonline 1|40 inch # The line was used in 19th century USA |
| 4677 | # to measure width of buttons. |
| 4678 | beespace 1|4 inch # Bees will fill any space that is smaller |
| 4679 | # than the bee space and leave open |
| 4680 | # spaces that are larger. The size of |
| 4681 | # the space varies with species. |
| 4682 | diamond 8|5 ft # Marking on US tape measures that is |
| 4683 | # useful to carpenters who wish to place |
| 4684 | # five studs in an 8 ft distance. Note |
| 4685 | # that the numbers appear in red every |
| 4686 | # 16 inches as well, giving six |
| 4687 | # divisions in 8 feet. |
| 4688 | retmaunit 1.75 in # Height of rack mountable equipment. |
| 4689 | U retmaunit # Equipment should be 1|32 inch narrower |
| 4690 | RU U # than its U measurement indicates to |
| 4691 | # allow for clearance, so 4U=(6+31|32)in |
| 4692 | # RETMA stands for the former name of |
| 4693 | # the standardizing organization, Radio |
| 4694 | # Electronics Television Manufacturers |
| 4695 | # Association. This organization is now |
| 4696 | # called the Electronic Industries |
| 4697 | # Alliance (EIA) and the rack standard |
| 4698 | # is specified in EIA RS-310-D. |
| 4699 | count per pound # For measuring the size of shrimp |
| 4700 | flightlevel 100 ft # Flight levels are used to ensure safe |
| 4701 | FL flightlevel # vertical separation between aircraft |
| 4702 | # despite variations in local air |
| 4703 | # pressure. Flight levels define |
| 4704 | # altitudes based on a standard air |
| 4705 | # pressure so that altimeter calibration |
| 4706 | # is not needed. This means that |
| 4707 | # aircraft at separated flight levels |
| 4708 | # are guaranteed to be separated. |
| 4709 | # Hence the definition of 100 feet is |
| 4710 | # a nominal, not true, measure. |
| 4711 | # Customarily written with no space in |
| 4712 | # the form FL290, which will not work in |
| 4713 | # units. But note "FL 290" will work. |
| 4714 | |
| 4715 | # |
| 4716 | # Other units of work, energy, power, etc |
| 4717 | # |
| 4718 | |
| 4719 | # Calorie: approximate energy to raise a gram of water one degree celsius |
| 4720 | |
| 4721 | calorie cal_th # Default is the thermochemical calorie |
| 4722 | cal calorie |
| 4723 | calorie_th 4.184 J # Thermochemical calorie, defined in 1930 |
| 4724 | thermcalorie calorie_th # by Frederick Rossini as 4.1833 J to |
| 4725 | cal_th calorie_th # avoid difficulties associated with the |
| 4726 | # uncertainty in the heat capacity of |
| 4727 | # water. In 1948 the value of the joule |
| 4728 | # was changed, so the thermochemical |
| 4729 | # calorie was redefined to 4.184 J. |
| 4730 | # This kept the energy measured by this |
| 4731 | # unit the same. |
| 4732 | calorie_IT 4.1868 J # International (Steam) Table calorie, |
| 4733 | cal_IT calorie_IT # defined in 1929 as watt-hour/860 or |
| 4734 | # equivalently 180|43 joules. At this |
| 4735 | # time the international joule had a |
| 4736 | # different value than the modern joule, |
| 4737 | # and the values were different in the |
| 4738 | # USA and in Europe. In 1956 at the |
| 4739 | # Fifth International Conference on |
| 4740 | # Properties of Steam the exact |
| 4741 | # definition given here was adopted. |
| 4742 | calorie_15 4.18580 J # Energy to go from 14.5 to 15.5 degC |
| 4743 | cal_15 calorie_15 |
| 4744 | calorie_fifteen cal_15 |
| 4745 | calorie_20 4.18190 J # Energy to go from 19.5 to 20.5 degC |
| 4746 | cal_20 calorie_20 |
| 4747 | calorie_twenty calorie_20 |
| 4748 | calorie_4 4.204 J # Energy to go from 3.5 to 4.5 degC |
| 4749 | cal_4 calorie_4 |
| 4750 | calorie_four calorie_4 |
| 4751 | cal_mean 4.19002 J # 1|100 energy to go from 0 to 100 degC |
| 4752 | Calorie kilocalorie # the food Calorie |
| 4753 | thermie 1e6 cal_15 # Heat required to raise the |
| 4754 | # temperature of a tonne of |
| 4755 | # water from 14.5 to 15.5 degC. |
| 4756 | |
| 4757 | # btu definitions: energy to raise a pound of water 1 degF |
| 4758 | |
| 4759 | btu btu_IT # International Table BTU is the default |
| 4760 | britishthermalunit btu |
| 4761 | btu_IT cal_IT lb degF / gram K |
| 4762 | btu_th cal_th lb degF / gram K |
| 4763 | btu_mean cal_mean lb degF / gram K |
| 4764 | btu_15 cal_15 lb degF / gram K |
| 4765 | btu_ISO 1055.06 J # Exact, rounded ISO definition based |
| 4766 | # on the IT calorie |
| 4767 | quad quadrillion btu |
| 4768 | |
| 4769 | ECtherm 1e5 btu_ISO # Exact definition |
| 4770 | UStherm 1.054804e8 J # Exact definition |
| 4771 | therm UStherm |
| 4772 | |
| 4773 | # Water latent heat from [23] |
| 4774 | |
| 4775 | water_fusion_heat 6.01 kJ/mol / (18.015 g/mol) # At 0 deg C |
| 4776 | water_vaporization_heat 2256.4 J/g # At saturation, 100 deg C, 101.42 kPa |
| 4777 | |
| 4778 | # Specific heat capacities of various substances |
| 4779 | # |
| 4780 | # SPECFIC_HEAT ENERGY / MASS / TEMPERATURE_DIFFERENCE |
| 4781 | # SPECFIC_HEAT_CAPACITY ENERGY / MASS / TEMPERATURE_DIFFERENCE |
| 4782 | |
| 4783 | specificheat_water calorie / g K |
| 4784 | water_specificheat specificheat_water |
| 4785 | # Values from www.engineeringtoolbox.com/specific-heat-metals-d_152.html |
| 4786 | specificheat_aluminum 0.91 J/g K |
| 4787 | specificheat_antimony 0.21 J/g K |
| 4788 | specificheat_barium 0.20 J/g K |
| 4789 | specificheat_beryllium 1.83 J/g K |
| 4790 | specificheat_bismuth 0.13 J/g K |
| 4791 | specificheat_cadmium 0.23 J/g K |
| 4792 | specificheat_cesium 0.24 J/g K |
| 4793 | specificheat_chromium 0.46 J/g K |
| 4794 | specificheat_cobalt 0.42 J/g K |
| 4795 | specificheat_copper 0.39 J/g K |
| 4796 | specificheat_gallium 0.37 J/g K |
| 4797 | specificheat_germanium 0.32 J/g K |
| 4798 | specificheat_gold 0.13 J/g K |
| 4799 | specificheat_hafnium 0.14 J/g K |
| 4800 | specificheat_indium 0.24 J/g K |
| 4801 | specificheat_iridium 0.13 J/g K |
| 4802 | specificheat_iron 0.45 J/g K |
| 4803 | specificheat_lanthanum 0.195 J/g K |
| 4804 | specificheat_lead 0.13 J/g K |
| 4805 | specificheat_lithium 3.57 J/g K |
| 4806 | specificheat_lutetium 0.15 J/g K |
| 4807 | specificheat_magnesium 1.05 J/g K |
| 4808 | specificheat_manganese 0.48 J/g K |
| 4809 | specificheat_mercury 0.14 J/g K |
| 4810 | specificheat_molybdenum 0.25 J/g K |
| 4811 | specificheat_nickel 0.44 J/g K |
| 4812 | specificheat_osmium 0.13 J/g K |
| 4813 | specificheat_palladium 0.24 J/g K |
| 4814 | specificheat_platinum 0.13 J/g K |
| 4815 | specificheat_plutonum 0.13 J/g K |
| 4816 | specificheat_potassium 0.75 J/g K |
| 4817 | specificheat_rhenium 0.14 J/g K |
| 4818 | specificheat_rhodium 0.24 J/g K |
| 4819 | specificheat_rubidium 0.36 J/g K |
| 4820 | specificheat_ruthenium 0.24 J/g K |
| 4821 | specificheat_scandium 0.57 J/g K |
| 4822 | specificheat_selenium 0.32 J/g K |
| 4823 | specificheat_silicon 0.71 J/g K |
| 4824 | specificheat_silver 0.23 J/g K |
| 4825 | specificheat_sodium 1.21 J/g K |
| 4826 | specificheat_strontium 0.30 J/g K |
| 4827 | specificheat_tantalum 0.14 J/g K |
| 4828 | specificheat_thallium 0.13 J/g K |
| 4829 | specificheat_thorium 0.13 J/g K |
| 4830 | specificheat_tin 0.21 J/g K |
| 4831 | specificheat_titanium 0.54 J/g K |
| 4832 | specificheat_tungsten 0.13 J/g K |
| 4833 | specificheat_uranium 0.12 J/g K |
| 4834 | specificheat_vanadium 0.39 J/g K |
| 4835 | specificheat_yttrium 0.30 J/g K |
| 4836 | specificheat_zinc 0.39 J/g K |
| 4837 | specificheat_zirconium 0.27 J/g K |
| 4838 | specificheat_ethanol 2.3 J/g K |
| 4839 | specificheat_ammonia 4.6 J/g K |
| 4840 | specificheat_freon 0.91 J/g K # R-12 at 0 degrees Fahrenheit |
| 4841 | specificheat_gasoline 2.22 J/g K |
| 4842 | specificheat_iodine 2.15 J/g K |
| 4843 | specificheat_oliveoil 1.97 J/g K |
| 4844 | |
| 4845 | # en.wikipedia.org/wiki/Heat_capacity#Table_of_specific_heat_capacities |
| 4846 | specificheat_hydrogen 14.3 J/g K |
| 4847 | specificheat_helium 5.1932 J/g K |
| 4848 | specificheat_argon 0.5203 J/g K |
| 4849 | specificheat_tissue 3.5 J/g K |
| 4850 | specificheat_diamond 0.5091 J/g K |
| 4851 | specificheat_granite 0.79 J/g K |
| 4852 | specificheat_graphite 0.71 J/g K |
| 4853 | specificheat_ice 2.11 J/g K |
| 4854 | specificheat_asphalt 0.92 J/g K |
| 4855 | specificheat_brick 0.84 J/g K |
| 4856 | specificheat_concrete 0.88 J/g K |
| 4857 | specificheat_glass_silica 0.84 J/g K |
| 4858 | specificheat_glass_flint 0.503 J/g K |
| 4859 | specificheat_glass_pyrex 0.753 J/g K |
| 4860 | specificheat_gypsum 1.09 J/g K |
| 4861 | specificheat_marble 0.88 J/g K |
| 4862 | specificheat_sand 0.835 J/g K |
| 4863 | specificheat_soil 0.835 J/g K |
| 4864 | specificheat_wood 1.7 J/g K |
| 4865 | |
| 4866 | specificheat_sucrose 1.244 J/g K #www.sugartech.co.za/heatcapacity/index.php |
| 4867 | |
| 4868 | |
| 4869 | # Energy densities of various fuels |
| 4870 | # |
| 4871 | # Most of these fuels have varying compositions or qualities and hence their |
| 4872 | # actual energy densities vary. These numbers are hence only approximate. |
| 4873 | # |
| 4874 | # E1. http://www.aps.org/policy/reports/popa-reports/energy/units.cfm |
| 4875 | # E2. https://web.archive.org/web/20100825042309/http://www.ior.com.au/ecflist.html |
| 4876 | |
| 4877 | tonoil 1e10 cal_IT # Ton oil equivalent. A conventional |
| 4878 | # value for the energy released by |
| 4879 | toe tonoil # burning one metric ton of oil. [18,E1] |
| 4880 | # Note that energy per mass of petroleum |
| 4881 | # products is fairly constant. |
| 4882 | # Variations in volumetric energy |
| 4883 | # density result from variations in the |
| 4884 | # density (kg/m^3) of different fuels. |
| 4885 | # This definition is given by the |
| 4886 | # IEA/OECD. |
| 4887 | toncoal 7e9 cal_IT # Energy in metric ton coal from [18]. |
| 4888 | # This is a nominal value which |
| 4889 | # is close to the heat content |
| 4890 | # of coal used in the 1950's |
| 4891 | barreloil 5.8 Mbtu # Conventional value for barrel of crude |
| 4892 | # oil [E1]. Actual range is 5.6 - 6.3. |
| 4893 | naturalgas_HHV 1027 btu/ft3 # Energy content of natural gas. HHV |
| 4894 | naturalgas_LHV 930 btu/ft3 # is for Higher Heating Value and |
| 4895 | naturalgas naturalgas_HHV # includes energy from condensation |
| 4896 | # combustion products. LHV is for Lower |
| 4897 | # Heating Value and excludes these. |
| 4898 | # American publications typically report |
| 4899 | # HHV whereas European ones report LHV. |
| 4900 | charcoal 30 GJ/tonne |
| 4901 | woodenergy_dry 20 GJ/tonne # HHV, a cord weights about a tonne |
| 4902 | woodenergy_airdry 15 GJ/tonne # 20% moisture content |
| 4903 | coal_bituminous 27 GJ / tonne |
| 4904 | coal_lignite 15 GJ / tonne |
| 4905 | coal_US 22 GJ / uston # Average for US coal (short ton), 1995 |
| 4906 | ethanol_HHV 84000 btu/usgallon |
| 4907 | ethanol_LHV 75700 btu/usgallon |
| 4908 | diesel 130500 btu/usgallon |
| 4909 | gasoline_LHV 115000 btu/usgallon |
| 4910 | gasoline_HHV 125000 btu/usgallon |
| 4911 | gasoline gasoline_HHV |
| 4912 | heating 37.3 MJ/liter |
| 4913 | fueloil 39.7 MJ/liter # low sulphur |
| 4914 | propane 93.3 MJ/m^3 |
| 4915 | butane 124 MJ/m^3 |
| 4916 | |
| 4917 | # The US EPA defines a "miles per gallon equivalent" for alternative |
| 4918 | # energy vehicles: |
| 4919 | |
| 4920 | mpg_e miles / gallon gasoline_LHV |
| 4921 | MPGe mpg_e |
| 4922 | |
| 4923 | # These values give total energy from uranium fission. Actual efficiency |
| 4924 | # of nuclear power plants is around 30%-40%. Note also that some reactors |
| 4925 | # use enriched uranium around 3% U-235. Uranium during processing or use |
| 4926 | # may be in a compound of uranium oxide or uranium hexafluoride, in which |
| 4927 | # case the energy density would be lower depending on how much uranium is |
| 4928 | # in the compound. |
| 4929 | |
| 4930 | uranium_pure 200 MeV avogadro / (235.0439299 g/mol) # Pure U-235 |
| 4931 | uranium_natural 0.7% uranium_pure # Natural uranium: 0.7% U-235 |
| 4932 | |
| 4933 | # Celsius heat unit: energy to raise a pound of water 1 degC |
| 4934 | |
| 4935 | celsiusheatunit cal lb degC / gram K |
| 4936 | chu celsiusheatunit |
| 4937 | |
| 4938 | # "Apparent" average power in an AC circuit, the product of rms voltage |
| 4939 | # and rms current, equal to the true power in watts when voltage and |
| 4940 | # current are in phase. In a DC circuit, always equal to the true power. |
| 4941 | |
| 4942 | VA volt ampere |
| 4943 | |
| 4944 | kWh kilowatt hour |
| 4945 | |
| 4946 | # The horsepower is supposedly the power of one horse pulling. Obviously |
| 4947 | # different people had different horses. |
| 4948 | |
| 4949 | horsepower 550 foot pound force / sec # Invented by James Watt |
| 4950 | mechanicalhorsepower horsepower |
| 4951 | hp horsepower |
| 4952 | metrichorsepower 75 kilogram force meter / sec # PS=Pferdestaerke in |
| 4953 | electrichorsepower 746 W # Germany |
| 4954 | boilerhorsepower 9809.50 W |
| 4955 | waterhorsepower 746.043 W |
| 4956 | brhorsepower horsepower # Value corrected Dec, 2019. Was 745.7 W. |
| 4957 | donkeypower 250 W |
| 4958 | chevalvapeur metrichorsepower |
| 4959 | |
| 4960 | # |
| 4961 | # Heat Transfer |
| 4962 | # |
| 4963 | # Thermal conductivity, K, measures the rate of heat transfer across |
| 4964 | # a material. The heat transferred is |
| 4965 | # Q = K dT A t / L |
| 4966 | # where dT is the temperature difference across the material, A is the |
| 4967 | # cross sectional area, t is the time, and L is the length (thickness). |
| 4968 | # Thermal conductivity is a material property. |
| 4969 | |
| 4970 | THERMAL_CONDUCTIVITY POWER / AREA (TEMPERATURE_DIFFERENCE/LENGTH) |
| 4971 | THERMAL_RESISTIVITY 1/THERMAL_CONDUCTIVITY |
| 4972 | |
| 4973 | # Thermal conductance is the rate at which heat flows across a given |
| 4974 | # object, so the area and thickness have been fixed. It depends on |
| 4975 | # the size of the object and is hence not a material property. |
| 4976 | |
| 4977 | THERMAL_CONDUCTANCE POWER / TEMPERATURE_DIFFERENCE |
| 4978 | THERMAL_RESISTANCE 1/THERMAL_CONDUCTANCE |
| 4979 | |
| 4980 | # Thermal admittance is the rate of heat flow per area across an |
| 4981 | # object whose thickness has been fixed. Its reciprocal, thermal |
| 4982 | # insulation, is used to for measuring the heat transfer per area |
| 4983 | # of sheets of insulation or cloth that are of specified thickness. |
| 4984 | |
| 4985 | THERMAL_ADMITTANCE THERMAL_CONDUCTIVITY / LENGTH |
| 4986 | THERMAL_INSULANCE THERMAL_RESISTIVITY LENGTH |
| 4987 | THERMAL_INSULATION THERMAL_RESISTIVITY LENGTH |
| 4988 | |
| 4989 | Rvalue degF ft^2 hr / btu |
| 4990 | Uvalue 1/Rvalue |
| 4991 | europeanUvalue watt / m^2 K |
| 4992 | RSI degC m^2 / W |
| 4993 | clo 0.155 degC m^2 / W # Supposed to be the insulance |
| 4994 | # required to keep a resting person |
| 4995 | # comfortable indoors. The value |
| 4996 | # given is from NIST and the CRC, |
| 4997 | # but [5] gives a slightly different |
| 4998 | # value of 0.875 ft^2 degF hr / btu. |
| 4999 | tog 0.1 degC m^2 / W # Also used for clothing. |
| 5000 | |
| 5001 | |
| 5002 | # Thermal Conductivity of a few materials |
| 5003 | |
| 5004 | diamond_natural_thermal_conductivity 2200 W / m K |
| 5005 | diamond_synthetic_thermal_conductivity 3320 W / m K # 99% pure C12 |
| 5006 | silver_thermal_conductivity 406 W / m K |
| 5007 | aluminum_thermal_conductivity 205 W / m K |
| 5008 | copper_thermal_conductivity 385 W / m K |
| 5009 | gold_thermal_conductivity 314 W / m K |
| 5010 | iron_thermal_conductivity 79.5 W / m K |
| 5011 | stainless_304_thermal_conductivity 15.5 W / m K # average value |
| 5012 | |
| 5013 | # The bel was defined by engineers of Bell Laboratories to describe the |
| 5014 | # reduction in audio level over a length of one mile. It was originally |
| 5015 | # called the transmission unit (TU) but was renamed around 1923 to honor |
| 5016 | # Alexander Graham Bell. The bel proved inconveniently large so the decibel |
| 5017 | # has become more common. The decibel is dimensionless since it reports a |
| 5018 | # ratio, but it is used in various contexts to report a signal's power |
| 5019 | # relative to some reference level. |
| 5020 | |
| 5021 | bel(x) units=[1;1] range=(0,) 10^(x); log(bel) # Basic bel definition |
| 5022 | decibel(x) units=[1;1] range=(0,) 10^(x/10); 10 log(decibel) # Basic decibel |
| 5023 | dB() decibel # Abbreviation |
| 5024 | dBW(x) units=[1;W] range=(0,) dB(x) W ; ~dB(dBW/W) # Reference = 1 W |
| 5025 | dBk(x) units=[1;W] range=(0,) dB(x) kW ; ~dB(dBk/kW) # Reference = 1 kW |
| 5026 | dBf(x) units=[1;W] range=(0,) dB(x) fW ; ~dB(dBf/fW) # Reference = 1 fW |
| 5027 | dBm(x) units=[1;W] range=(0,) dB(x) mW ; ~dB(dBm/mW) # Reference = 1 mW |
| 5028 | dBmW(x) units=[1;W] range=(0,) dBm(x) ; ~dBm(dBmW) # Reference = 1 mW |
| 5029 | dBJ(x) units=[1;J] range=(0,) dB(x) J; ~dB(dBJ/J) # Energy relative |
| 5030 | # to 1 joule. Used for power spectral |
| 5031 | # density since W/Hz = J |
| 5032 | |
| 5033 | |
| 5034 | # When used to measure amplitude, voltage, or current the signal is squared |
| 5035 | # because power is proportional to the square of these measures. The root |
| 5036 | # mean square (RMS) voltage is typically used with these units. |
| 5037 | |
| 5038 | dB_amplitude(x) units=[1;1] dB(0.5 x) ; ~dB(dB_amplitude^2) |
| 5039 | dBV(x) units=[1;V] range=(0,) dB(0.5 x) V;~dB(dBV^2 / V^2) # Reference = 1 V |
| 5040 | dBmV(x) units=[1;V] range=(0,) dB(0.5 x) mV;~dB(dBmV^2/mV^2)# Reference = 1 mV |
| 5041 | dBuV(x) units=[1;V] range=(0,) dB(0.5 x) microV ; ~dB(dBuV^2 / microV^2) |
| 5042 | # Reference = 1 microvolt |
| 5043 | |
| 5044 | # Here are dB measurements for current. Be aware that dbA is also |
| 5045 | # a unit for frequency weighted sound pressure. |
| 5046 | dBA(x) units=[1;A] range=(0,) dB(0.5 x) A;~dB(dBA^2 / A^2) # Reference = 1 A |
| 5047 | dBmA(x) units=[1;A] range=(0,) dB(0.5 x) mA;~dB(dBmA^2/mA^2)# Reference = 1 mA |
| 5048 | dBuA(x) units=[1;A] range=(0,) dB(0.5 x) microA ; ~dB(dBuA^2 / microA^2) |
| 5049 | # Reference = 1 microamp |
| 5050 | |
| 5051 | # Referenced to the voltage that causes 1 mW dissipation in a 600 ohm load. |
| 5052 | # Originally defined as dBv but changed to prevent confusion with dBV. |
| 5053 | # The "u" is for unloaded. |
| 5054 | dBu(x) units=[1;V] range=(0,) dB(0.5 x) sqrt(mW 600 ohm) ; \ |
| 5055 | ~dB(dBu^2 / mW 600 ohm) |
| 5056 | dBv(x) units=[1;V] range=(0,) dBu(x) ; ~dBu(dBv) # Synonym for dBu |
| 5057 | |
| 5058 | # Measurements for sound in air, referenced to the threshold of human hearing |
| 5059 | # Note that sound in other media typically uses 1 micropascal as a reference |
| 5060 | # for sound pressure. Units dBA, dBB, dBC, refer to different frequency |
| 5061 | # weightings meant to approximate the human ear's response. |
| 5062 | |
| 5063 | # sound pressure level |
| 5064 | dBSPL(x) units=[1;Pa] range=(0,) dB(0.5 x) 20 microPa ; \ |
| 5065 | ~dB(dBSPL^2 / (20 microPa)^2) |
| 5066 | # sound intensity level |
| 5067 | dBSIL(x) units=[1;W/m^2] range=(0,) dB(x) 1e-12 W/m^2; \ |
| 5068 | ~dB(dBSIL / (1e-12 W/m^2)) |
| 5069 | # sound power level (The W in SWL is for the reference power, 1 W.) |
| 5070 | dBSWL(x) units=[1;W] range=(0,) dB(x) 1e-12 W; ~dB(dBSWL/1e-12 W) |
| 5071 | |
| 5072 | # The neper is another similar logarithmic unit. Note that the neper |
| 5073 | # is defined based on the ratio of amplitudes rather than the power |
| 5074 | # ratio like the decibel. This means that if the data is power, and |
| 5075 | # you convert to nepers you should take the square root of the data |
| 5076 | # to convert to amplitude. If you want to convert nepers to a power |
| 5077 | # measurement you need to square the resulting output. |
| 5078 | |
| 5079 | neper(x) units=[1;1] range=(0,) exp(x); ln(neper) |
| 5080 | centineper(x) units=[1;1] range=(0,) exp(x/100); 100 ln(centineper) |
| 5081 | Np() neper |
| 5082 | cNp() centineper |
| 5083 | Np_power(x) units=[1;1] Np(2 x) ; ~Np(Np_power)/2 |
| 5084 | |
| 5085 | # Misc other measures |
| 5086 | |
| 5087 | ENTROPY ENERGY / TEMPERATURE |
| 5088 | clausius 1e3 cal/K # A unit of physical entropy |
| 5089 | langley thermcalorie/cm^2 # Used in radiation theory |
| 5090 | poncelet 100 kg force m / s |
| 5091 | tonrefrigeration uston 144 btu / lb day # One ton refrigeration is |
| 5092 | # the rate of heat extraction required |
| 5093 | # turn one ton of water to ice in |
| 5094 | # a day. Ice is defined to have a |
| 5095 | # latent heat of 144 btu/lb. |
| 5096 | tonref tonrefrigeration |
| 5097 | refrigeration tonref / ton |
| 5098 | frigorie 1000 cal_15 # Used in refrigeration engineering. |
| 5099 | airwatt 8.5 (ft^3/min) inH2O # Measure of vacuum power as |
| 5100 | # pressure times air flow. |
| 5101 | |
| 5102 | # The unit "tnt" is defined so that you can write "tons tnt". The |
| 5103 | # question of which ton, exactly, is intended. The answer is that |
| 5104 | # nobody knows: |
| 5105 | # |
| 5106 | # Quoting the footnote from page 13 of |
| 5107 | # The Effects of Nuclear Weapons, 3rd ed. |
| 5108 | # https://www.fourmilab.ch/etexts/www/effects/eonw_1.pdf |
| 5109 | # |
| 5110 | # The majority of the experimental and theoretical values of the |
| 5111 | # explosive energy released by TNT range from 900 to 1,100 calories per |
| 5112 | # gram. At one time, there was some uncertainty as to whether the term |
| 5113 | # "kiloton" of TNT referred to a short kiloton (2*10^6 pounds), a metric |
| 5114 | # kiloton (2.205*10^6 pounds), or a long kiloton (2.24*10^6 pounds). In |
| 5115 | # order to avoid ambiguity, it was agreed that the term "kiloton" would |
| 5116 | # refer to the release of 10^12 calories of explosive energy. This is |
| 5117 | # equivalent to 1 short kiloton of TNT if the energy release is 1,102 |
| 5118 | # calories per gram or to 1 long kiloton if the energy is 984 calories |
| 5119 | # per gram of TNT. |
| 5120 | # |
| 5121 | # It is therefore not well-defined how much energy a "gram of tnt" is, |
| 5122 | # though this term does appear in some references. |
| 5123 | |
| 5124 | tnt 1e9 cal_th / ton # Defined exact value |
| 5125 | |
| 5126 | # Nuclear weapon yields |
| 5127 | |
| 5128 | davycrocket 10 ton tnt # lightest US tactical nuclear weapon |
| 5129 | hiroshima 15.5 kiloton tnt # Uranium-235 fission bomb |
| 5130 | nagasaki 21 kiloton tnt # Plutonium-239 fission bomb |
| 5131 | fatman nagasaki |
| 5132 | littleboy hiroshima |
| 5133 | ivyking 500 kiloton tnt # most powerful fission bomb |
| 5134 | castlebravo 15 megaton tnt # most powerful US test |
| 5135 | tsarbomba 50 megaton tnt # most powerful test ever: USSR, |
| 5136 | # 30 October 1961 |
| 5137 | b53bomb 9 megaton tnt |
| 5138 | # http://rarehistoricalphotos.com/gadget-first-atomic-bomb/ |
| 5139 | trinity 18 kiloton tnt # July 16, 1945 |
| 5140 | gadget trinity |
| 5141 | |
| 5142 | # |
| 5143 | # Permeability: The permeability or permeance, n, of a substance determines |
| 5144 | # how fast vapor flows through the substance. The formula W = n A dP |
| 5145 | # holds where W is the rate of flow (in mass/time), n is the permeability, |
| 5146 | # A is the area of the flow path, and dP is the vapor pressure difference. |
| 5147 | # |
| 5148 | |
| 5149 | perm_0C grain / hr ft^2 inHg |
| 5150 | perm_zero perm_0C |
| 5151 | perm_0 perm_0C |
| 5152 | perm perm_0C |
| 5153 | perm_23C grain / hr ft^2 in Hg23C |
| 5154 | perm_twentythree perm_23C |
| 5155 | |
| 5156 | # |
| 5157 | # Counting measures |
| 5158 | # |
| 5159 | |
| 5160 | pair 2 |
| 5161 | brace 2 |
| 5162 | nest 3 # often used for items like bowls that |
| 5163 | # nest together |
| 5164 | hattrick 3 # Used in sports, especially cricket and ice |
| 5165 | # hockey to report the number of goals. |
| 5166 | dicker 10 |
| 5167 | dozen 12 |
| 5168 | bakersdozen 13 |
| 5169 | score 20 |
| 5170 | flock 40 |
| 5171 | timer 40 |
| 5172 | shock 60 |
| 5173 | toncount 100 # Used in sports in the UK |
| 5174 | longhundred 120 # From a germanic counting system |
| 5175 | gross 144 |
| 5176 | greatgross 12 gross |
| 5177 | tithe 1|10 # From Anglo-Saxon word for tenth |
| 5178 | |
| 5179 | # Paper counting measure |
| 5180 | |
| 5181 | shortquire 24 |
| 5182 | quire 25 |
| 5183 | shortream 480 |
| 5184 | ream 500 |
| 5185 | perfectream 516 |
| 5186 | bundle 2 reams |
| 5187 | bale 5 bundles |
| 5188 | |
| 5189 | # |
| 5190 | # Paper measures |
| 5191 | # |
| 5192 | |
| 5193 | # USA paper sizes |
| 5194 | |
| 5195 | lettersize 8.5 inch 11 inch |
| 5196 | legalsize 8.5 inch 14 inch |
| 5197 | ledgersize 11 inch 17 inch |
| 5198 | executivesize 7.25 inch 10.5 inch |
| 5199 | Apaper 8.5 inch 11 inch |
| 5200 | Bpaper 11 inch 17 inch |
| 5201 | Cpaper 17 inch 22 inch |
| 5202 | Dpaper 22 inch 34 inch |
| 5203 | Epaper 34 inch 44 inch |
| 5204 | |
| 5205 | # Correspondence envelope sizes. #10 is the standard business |
| 5206 | # envelope in the USA. |
| 5207 | |
| 5208 | envelope6_25size 3.5 inch 6 inch |
| 5209 | envelope6_75size 3.625 inch 6.5 inch |
| 5210 | envelope7size 3.75 inch 6.75 inch |
| 5211 | envelope7_75size 3.875 inch 7.5 inch |
| 5212 | envelope8_625size 3.625 inch 8.625 inch |
| 5213 | envelope9size 3.875 inch 8.875 inch |
| 5214 | envelope10size 4.125 inch 9.5 inch |
| 5215 | envelope11size 4.5 inch 10.375 inch |
| 5216 | envelope12size 4.75 inch 11 inch |
| 5217 | envelope14size 5 inch 11.5 inch |
| 5218 | envelope16size 6 inch 12 inch |
| 5219 | |
| 5220 | # Announcement envelope sizes (no relation to metric paper sizes like A4) |
| 5221 | |
| 5222 | envelopeA1size 3.625 inch 5.125 inch # same as 4bar |
| 5223 | envelopeA2size 4.375 inch 5.75 inch |
| 5224 | envelopeA6size 4.75 inch 6.5 inch |
| 5225 | envelopeA7size 5.25 inch 7.25 inch |
| 5226 | envelopeA8size 5.5 inch 8.125 inch |
| 5227 | envelopeA9size 5.75 inch 8.75 inch |
| 5228 | envelopeA10size 6 inch 9.5 inch |
| 5229 | |
| 5230 | # Baronial envelopes |
| 5231 | |
| 5232 | envelope4bar 3.625 inch 5.125 inch # same as A1 |
| 5233 | envelope5_5bar 4.375 inch 5.75 inch |
| 5234 | envelope6bar 4.75 inch 6.5 inch |
| 5235 | |
| 5236 | # Coin envelopes |
| 5237 | |
| 5238 | envelope1baby 2.25 inch 3.5 inch # same as #1 coin |
| 5239 | envelope00coin 1.6875 inch 2.75 inch |
| 5240 | envelope1coin 2.25 inch 3.5 inch |
| 5241 | envelope3coin 2.5 inch 4.25 inch |
| 5242 | envelope4coin 3 inch 4.5 inch |
| 5243 | envelope4_5coin 3 inch 4.875 inch |
| 5244 | envelope5coin 2.875 inch 5.25 inch |
| 5245 | envelope5_5coin 3.125 inch 5.5 inch |
| 5246 | envelope6coin 3.375 inch 6 inch |
| 5247 | envelope7coin 3.5 inch 6.5 inch |
| 5248 | |
| 5249 | # The metric paper sizes are defined so that if a sheet is cut in half |
| 5250 | # along the short direction, the result is two sheets which are |
| 5251 | # similar to the original sheet. This means that for any metric size, |
| 5252 | # the long side is close to sqrt(2) times the length of the short |
| 5253 | # side. Each series of sizes is generated by repeated cuts in half, |
| 5254 | # with the values rounded down to the nearest millimeter. |
| 5255 | |
| 5256 | A0paper 841 mm 1189 mm # The basic size in the A series |
| 5257 | A1paper 594 mm 841 mm # is defined to have an area of |
| 5258 | A2paper 420 mm 594 mm # one square meter. |
| 5259 | A3paper 297 mm 420 mm |
| 5260 | A4paper 210 mm 297 mm |
| 5261 | A5paper 148 mm 210 mm |
| 5262 | A6paper 105 mm 148 mm |
| 5263 | A7paper 74 mm 105 mm |
| 5264 | A8paper 52 mm 74 mm |
| 5265 | A9paper 37 mm 52 mm |
| 5266 | A10paper 26 mm 37 mm |
| 5267 | |
| 5268 | B0paper 1000 mm 1414 mm # The basic B size has an area |
| 5269 | B1paper 707 mm 1000 mm # of sqrt(2) square meters. |
| 5270 | B2paper 500 mm 707 mm |
| 5271 | B3paper 353 mm 500 mm |
| 5272 | B4paper 250 mm 353 mm |
| 5273 | B5paper 176 mm 250 mm |
| 5274 | B6paper 125 mm 176 mm |
| 5275 | B7paper 88 mm 125 mm |
| 5276 | B8paper 62 mm 88 mm |
| 5277 | B9paper 44 mm 62 mm |
| 5278 | B10paper 31 mm 44 mm |
| 5279 | |
| 5280 | C0paper 917 mm 1297 mm # The basic C size has an area |
| 5281 | C1paper 648 mm 917 mm # of sqrt(sqrt(2)) square meters. |
| 5282 | C2paper 458 mm 648 mm |
| 5283 | C3paper 324 mm 458 mm # Intended for envelope sizes |
| 5284 | C4paper 229 mm 324 mm |
| 5285 | C5paper 162 mm 229 mm |
| 5286 | C6paper 114 mm 162 mm |
| 5287 | C7paper 81 mm 114 mm |
| 5288 | C8paper 57 mm 81 mm |
| 5289 | C9paper 40 mm 57 mm |
| 5290 | C10paper 28 mm 40 mm |
| 5291 | |
| 5292 | # gsm (Grams per Square Meter), a sane, metric paper weight measure |
| 5293 | |
| 5294 | gsm grams / meter^2 |
| 5295 | |
| 5296 | # In the USA, a collection of crazy historical paper measures are used. Paper |
| 5297 | # is measured as a weight of a ream of that particular type of paper. This is |
| 5298 | # sometimes called the "substance" or "basis" (as in "substance 20" paper). |
| 5299 | # The standard sheet size or "basis size" varies depending on the type of |
| 5300 | # paper. As a result, 20 pound bond paper and 50 pound text paper are actually |
| 5301 | # about the same weight. The different sheet sizes were historically the most |
| 5302 | # convenient for printing or folding in the different applications. These |
| 5303 | # different basis weights are standards maintained by American Society for |
| 5304 | # Testing Materials (ASTM) and the American Forest and Paper Association |
| 5305 | # (AF&PA). |
| 5306 | |
| 5307 | poundbookpaper lb / 25 inch 38 inch ream |
| 5308 | lbbook poundbookpaper |
| 5309 | poundtextpaper poundbookpaper |
| 5310 | lbtext poundtextpaper |
| 5311 | poundoffsetpaper poundbookpaper # For offset printing |
| 5312 | lboffset poundoffsetpaper |
| 5313 | poundbiblepaper poundbookpaper # Designed to be lightweight, thin, |
| 5314 | lbbible poundbiblepaper # strong and opaque. |
| 5315 | poundtagpaper lb / 24 inch 36 inch ream |
| 5316 | lbtag poundtagpaper |
| 5317 | poundbagpaper poundtagpaper |
| 5318 | lbbag poundbagpaper |
| 5319 | poundnewsprintpaper poundtagpaper |
| 5320 | lbnewsprint poundnewsprintpaper |
| 5321 | poundposterpaper poundtagpaper |
| 5322 | lbposter poundposterpaper |
| 5323 | poundtissuepaper poundtagpaper |
| 5324 | lbtissue poundtissuepaper |
| 5325 | poundwrappingpaper poundtagpaper |
| 5326 | lbwrapping poundwrappingpaper |
| 5327 | poundwaxingpaper poundtagpaper |
| 5328 | lbwaxing poundwaxingpaper |
| 5329 | poundglassinepaper poundtagpaper |
| 5330 | lbglassine poundglassinepaper |
| 5331 | poundcoverpaper lb / 20 inch 26 inch ream |
| 5332 | lbcover poundcoverpaper |
| 5333 | poundindexpaper lb / 25.5 inch 30.5 inch ream |
| 5334 | lbindex poundindexpaper |
| 5335 | poundindexbristolpaper poundindexpaper |
| 5336 | lbindexbristol poundindexpaper |
| 5337 | poundbondpaper lb / 17 inch 22 inch ream # Bond paper is stiff and |
| 5338 | lbbond poundbondpaper # durable for repeated |
| 5339 | poundwritingpaper poundbondpaper # filing, and it resists |
| 5340 | lbwriting poundwritingpaper # ink penetration. |
| 5341 | poundledgerpaper poundbondpaper |
| 5342 | lbledger poundledgerpaper |
| 5343 | poundcopypaper poundbondpaper |
| 5344 | lbcopy poundcopypaper |
| 5345 | poundblottingpaper lb / 19 inch 24 inch ream |
| 5346 | lbblotting poundblottingpaper |
| 5347 | poundblankspaper lb / 22 inch 28 inch ream |
| 5348 | lbblanks poundblankspaper |
| 5349 | poundpostcardpaper lb / 22.5 inch 28.5 inch ream |
| 5350 | lbpostcard poundpostcardpaper |
| 5351 | poundweddingbristol poundpostcardpaper |
| 5352 | lbweddingbristol poundweddingbristol |
| 5353 | poundbristolpaper poundweddingbristol |
| 5354 | lbbristol poundbristolpaper |
| 5355 | poundboxboard lb / 1000 ft^2 |
| 5356 | lbboxboard poundboxboard |
| 5357 | poundpaperboard poundboxboard |
| 5358 | lbpaperboard poundpaperboard |
| 5359 | |
| 5360 | # When paper is marked in units of M, it means the weight of 1000 sheets of the |
| 5361 | # given size of paper. To convert this to paper weight, divide by the size of |
| 5362 | # the paper in question. |
| 5363 | |
| 5364 | paperM lb / 1000 |
| 5365 | |
| 5366 | # In addition paper weight is reported in "caliper" which is simply the |
| 5367 | # thickness of one sheet, typically in inches. Thickness is also reported in |
| 5368 | # "points" where a point is 1|1000 inch. These conversions are supplied to |
| 5369 | # convert these units roughly (using an approximate density) into the standard |
| 5370 | # paper weight values. |
| 5371 | |
| 5372 | pointthickness 0.001 in |
| 5373 | paperdensity 0.8 g/cm^3 # approximate--paper densities vary! |
| 5374 | papercaliper in paperdensity |
| 5375 | paperpoint pointthickness paperdensity |
| 5376 | |
| 5377 | # |
| 5378 | # Printing |
| 5379 | # |
| 5380 | |
| 5381 | fournierpoint 0.1648 inch / 12 # First definition of the printers |
| 5382 | # point made by Pierre Fournier who |
| 5383 | # defined it in 1737 as 1|12 of a |
| 5384 | # cicero which was 0.1648 inches. |
| 5385 | olddidotpoint 1|72 frenchinch # Francois Ambroise Didot, one of |
| 5386 | # a family of printers, changed |
| 5387 | # Fournier's definition around 1770 |
| 5388 | # to fit to the French units then in |
| 5389 | # use. |
| 5390 | bertholdpoint 1|2660 m # H. Berthold tried to create a |
| 5391 | # metric version of the didot point |
| 5392 | # in 1878. |
| 5393 | INpoint 0.4 mm # This point was created by a |
| 5394 | # group directed by Fermin Didot in |
| 5395 | # 1881 and is associated with the |
| 5396 | # imprimerie nationale. It doesn't |
| 5397 | # seem to have been used much. |
| 5398 | germandidotpoint 0.376065 mm # Exact definition appears in DIN |
| 5399 | # 16507, a German standards document |
| 5400 | # of 1954. Adopted more broadly in |
| 5401 | # 1966 by ??? |
| 5402 | metricpoint 3|8 mm # Proposed in 1977 by Eurograf |
| 5403 | oldpoint 1|72.27 inch # The American point was invented |
| 5404 | printerspoint oldpoint # by Nelson Hawks in 1879 and |
| 5405 | texpoint oldpoint # dominates USA publishing. |
| 5406 | # It was standardized by the American |
| 5407 | # Typefounders Association at the |
| 5408 | # value of 0.013837 inches exactly. |
| 5409 | # Knuth uses the approximation given |
| 5410 | # here (which is very close). The |
| 5411 | # comp.fonts FAQ claims that this |
| 5412 | # value is supposed to be 1|12 of a |
| 5413 | # pica where 83 picas is equal to 35 |
| 5414 | # cm. But this value differs from |
| 5415 | # the standard. |
| 5416 | texscaledpoint 1|65536 texpoint # The TeX typesetting system uses |
| 5417 | texsp texscaledpoint # this for all computations. |
| 5418 | computerpoint 1|72 inch # The American point was rounded |
| 5419 | point computerpoint |
| 5420 | computerpica 12 computerpoint # to an even 1|72 inch by computer |
| 5421 | postscriptpoint computerpoint # people at some point. |
| 5422 | pspoint postscriptpoint |
| 5423 | twip 1|20 point # TWentieth of an Imperial Point |
| 5424 | Q 1|4 mm # Used in Japanese phototypesetting |
| 5425 | # Q is for quarter |
| 5426 | frenchprinterspoint olddidotpoint |
| 5427 | didotpoint germandidotpoint # This seems to be the dominant value |
| 5428 | europeanpoint didotpoint # for the point used in Europe |
| 5429 | cicero 12 didotpoint |
| 5430 | |
| 5431 | stick 2 inches |
| 5432 | |
| 5433 | # Type sizes |
| 5434 | |
| 5435 | excelsior 3 oldpoint |
| 5436 | brilliant 3.5 oldpoint |
| 5437 | diamondtype 4 oldpoint |
| 5438 | pearl 5 oldpoint |
| 5439 | agate 5.5 oldpoint # Originally agate type was 14 lines per |
| 5440 | # inch, giving a value of 1|14 in. |
| 5441 | ruby agate # British |
| 5442 | nonpareil 6 oldpoint |
| 5443 | mignonette 6.5 oldpoint |
| 5444 | emerald mignonette # British |
| 5445 | minion 7 oldpoint |
| 5446 | brevier 8 oldpoint |
| 5447 | bourgeois 9 oldpoint |
| 5448 | longprimer 10 oldpoint |
| 5449 | smallpica 11 oldpoint |
| 5450 | pica 12 oldpoint |
| 5451 | english 14 oldpoint |
| 5452 | columbian 16 oldpoint |
| 5453 | greatprimer 18 oldpoint |
| 5454 | paragon 20 oldpoint |
| 5455 | meridian 44 oldpoint |
| 5456 | canon 48 oldpoint |
| 5457 | |
| 5458 | # German type sizes |
| 5459 | |
| 5460 | nonplusultra 2 didotpoint |
| 5461 | brillant 3 didotpoint |
| 5462 | diamant 4 didotpoint |
| 5463 | perl 5 didotpoint |
| 5464 | nonpareille 6 didotpoint |
| 5465 | kolonel 7 didotpoint |
| 5466 | petit 8 didotpoint |
| 5467 | borgis 9 didotpoint |
| 5468 | korpus 10 didotpoint |
| 5469 | corpus korpus |
| 5470 | garamond korpus |
| 5471 | mittel 14 didotpoint |
| 5472 | tertia 16 didotpoint |
| 5473 | text 18 didotpoint |
| 5474 | kleine_kanon 32 didotpoint |
| 5475 | kanon 36 didotpoint |
| 5476 | grobe_kanon 42 didotpoint |
| 5477 | missal 48 didotpoint |
| 5478 | kleine_sabon 72 didotpoint |
| 5479 | grobe_sabon 84 didotpoint |
| 5480 | |
| 5481 | # |
| 5482 | # Information theory units. Note that the name "entropy" is used both |
| 5483 | # to measure information and as a physical quantity. |
| 5484 | # |
| 5485 | |
| 5486 | INFORMATION bit |
| 5487 | |
| 5488 | nat (1/ln(2)) bits # Entropy measured base e |
| 5489 | hartley log2(10) bits # Entropy of a uniformly |
| 5490 | ban hartley # distributed random variable |
| 5491 | # over 10 symbols. |
| 5492 | dit hartley # from Decimal digIT |
| 5493 | |
| 5494 | # |
| 5495 | # Computer |
| 5496 | # |
| 5497 | |
| 5498 | bps bit/sec # Sometimes the term "baud" is |
| 5499 | # incorrectly used to refer to |
| 5500 | # bits per second. Baud refers |
| 5501 | # to symbols per second. Modern |
| 5502 | # modems transmit several bits |
| 5503 | # per symbol. |
| 5504 | byte 8 bit # Not all machines had 8 bit |
| 5505 | B byte # bytes, but these days most of |
| 5506 | # them do. But beware: for |
| 5507 | # transmission over modems, a |
| 5508 | # few extra bits are used so |
| 5509 | # there are actually 10 bits per |
| 5510 | # byte. |
| 5511 | octet 8 bits # The octet is always 8 bits |
| 5512 | nybble 4 bits # Half of a byte. Sometimes |
| 5513 | # equal to different lengths |
| 5514 | # such as 3 bits. |
| 5515 | nibble nybble |
| 5516 | nyp 2 bits # Donald Knuth asks in an exercise |
| 5517 | # for a name for a 2 bit |
| 5518 | # quantity and gives the "nyp" |
| 5519 | # as a solution due to Gregor |
| 5520 | # Purdy. Not in common use. |
| 5521 | meg megabyte # Some people consider these |
| 5522 | # units along with the kilobyte |
| 5523 | gig gigabyte # to be defined according to |
| 5524 | # powers of 2 with the kilobyte |
| 5525 | # equal to 2^10 bytes, the |
| 5526 | # megabyte equal to 2^20 bytes and |
| 5527 | # the gigabyte equal to 2^30 bytes |
| 5528 | # but these usages are forbidden |
| 5529 | # by SI. Binary prefixes have |
| 5530 | # been defined by IEC to replace |
| 5531 | # the SI prefixes. Use them to |
| 5532 | # get the binary units KiB, MiB, |
| 5533 | # GiB, etc. |
| 5534 | jiffy 0.01 sec # This is defined in the Jargon File |
| 5535 | jiffies jiffy # (http://www.jargon.org) as being the |
| 5536 | # duration of a clock tick for measuring |
| 5537 | # wall-clock time. Supposedly the value |
| 5538 | # used to be 1|60 sec or 1|50 sec |
| 5539 | # depending on the frequency of AC power, |
| 5540 | # but then 1|100 sec became more common. |
| 5541 | # On linux systems, this term is used and |
| 5542 | # for the Intel based chips, it does have |
| 5543 | # the value of .01 sec. The Jargon File |
| 5544 | # also lists two other definitions: |
| 5545 | # millisecond, and the time taken for |
| 5546 | # light to travel one foot. |
| 5547 | cdaudiospeed 44.1 kHz 2*16 bits # CD audio data rate at 44.1 kHz with 2 |
| 5548 | # samples of sixteen bits each. |
| 5549 | cdromspeed 75 2048 bytes / sec # For data CDs (mode1) 75 sectors are read |
| 5550 | # each second with 2048 bytes per sector. |
| 5551 | # Audio CDs do not have sectors, but |
| 5552 | # people sometimes divide the bit rate by |
| 5553 | # 75 and claim a sector length of 2352. |
| 5554 | # Data CDs have a lower rate due to |
| 5555 | # increased error correction overhead. |
| 5556 | # There is a rarely used mode (mode2) with |
| 5557 | # 2336 bytes per sector that has fewer |
| 5558 | # error correction bits than mode1. |
| 5559 | dvdspeed 1385 kB/s # This is the "1x" speed of a DVD using |
| 5560 | # constant linear velocity (CLV) mode. |
| 5561 | # Modern DVDs may vary the linear velocity |
| 5562 | # as they go from the inside to the |
| 5563 | # outside of the disc. |
| 5564 | # See http://www.osta.org/technology/dvdqa/dvdqa4.htm |
| 5565 | |
| 5566 | FIT / 1e9 hour # Failures In Time, number of failures per billion hours |
| 5567 | |
| 5568 | # |
| 5569 | # The IP address space is divided into subnets. The number of hosts |
| 5570 | # in a subnet depends on the length of the subnet prefix. This is |
| 5571 | # often written as /N where N is the number of bits in the prefix. |
| 5572 | # |
| 5573 | # https://en.wikipedia.org/wiki/Subnetwork |
| 5574 | # |
| 5575 | # These definitions gives the number of hosts for a subnet whose |
| 5576 | # prefix has the specified length in bits. |
| 5577 | # |
| 5578 | |
| 5579 | ipv4subnetsize(prefix_len) units=[1;1] domain=[0,32] range=[1,4294967296] \ |
| 5580 | 2^(32-prefix_len) ; 32-log2(ipv4subnetsize) |
| 5581 | ipv4classA ipv4subnetsize(8) |
| 5582 | ipv4classB ipv4subnetsize(16) |
| 5583 | ipv4classC ipv4subnetsize(24) |
| 5584 | |
| 5585 | ipv6subnetsize(prefix_len) units=[1;1] domain=[0,128] \ |
| 5586 | range=[1,340282366920938463463374607431768211456] \ |
| 5587 | 2^(128-prefix_len) ; 128-log2(ipv6subnetsize) |
| 5588 | |
| 5589 | # |
| 5590 | # Musical measures. Musical intervals expressed as ratios. Multiply |
| 5591 | # two intervals together to get the sum of the interval. The function |
| 5592 | # musicalcent can be used to convert ratios to cents. |
| 5593 | # |
| 5594 | |
| 5595 | # Perfect intervals |
| 5596 | |
| 5597 | octave 2 |
| 5598 | majorsecond musicalfifth^2 / octave |
| 5599 | majorthird 5|4 |
| 5600 | minorthird 6|5 |
| 5601 | musicalfourth 4|3 |
| 5602 | musicalfifth 3|2 |
| 5603 | majorsixth musicalfourth majorthird |
| 5604 | minorsixth musicalfourth minorthird |
| 5605 | majorseventh musicalfifth majorthird |
| 5606 | minorseventh musicalfifth minorthird |
| 5607 | |
| 5608 | pythagoreanthird majorsecond musicalfifth^2 / octave |
| 5609 | syntoniccomma pythagoreanthird / majorthird |
| 5610 | pythagoreancomma musicalfifth^12 / octave^7 |
| 5611 | |
| 5612 | # Equal tempered definitions |
| 5613 | |
| 5614 | semitone octave^(1|12) |
| 5615 | musicalcent(x) units=[1;1] range=(0,) semitone^(x/100) ; \ |
| 5616 | 100 log(musicalcent)/log(semitone) |
| 5617 | |
| 5618 | # |
| 5619 | # Musical note lengths. |
| 5620 | # |
| 5621 | |
| 5622 | wholenote ! |
| 5623 | MUSICAL_NOTE_LENGTH wholenote |
| 5624 | halfnote 1|2 wholenote |
| 5625 | quarternote 1|4 wholenote |
| 5626 | eighthnote 1|8 wholenote |
| 5627 | sixteenthnote 1|16 wholenote |
| 5628 | thirtysecondnote 1|32 wholenote |
| 5629 | sixtyfourthnote 1|64 wholenote |
| 5630 | dotted 3|2 |
| 5631 | doubledotted 7|4 |
| 5632 | breve doublewholenote |
| 5633 | semibreve wholenote |
| 5634 | minimnote halfnote |
| 5635 | crotchet quarternote |
| 5636 | quaver eighthnote |
| 5637 | semiquaver sixteenthnote |
| 5638 | demisemiquaver thirtysecondnote |
| 5639 | hemidemisemiquaver sixtyfourthnote |
| 5640 | semidemisemiquaver hemidemisemiquaver |
| 5641 | |
| 5642 | # |
| 5643 | # yarn and cloth measures |
| 5644 | # |
| 5645 | |
| 5646 | # yarn linear density |
| 5647 | |
| 5648 | woolyarnrun 1600 yard/pound # 1600 yds of "number 1 yarn" weighs |
| 5649 | # a pound. |
| 5650 | yarncut 300 yard/pound # Less common system used in |
| 5651 | # Pennsylvania for wool yarn |
| 5652 | cottonyarncount 840 yard/pound |
| 5653 | linenyarncount 300 yard/pound # Also used for hemp and ramie |
| 5654 | worstedyarncount 1680 ft/pound |
| 5655 | metricyarncount meter/gram |
| 5656 | denier 1|9 tex # used for silk and rayon |
| 5657 | manchesteryarnnumber drams/1000 yards # old system used for silk |
| 5658 | pli lb/in |
| 5659 | typp 1000 yd/lb # abbreviation for Thousand Yard Per Pound |
| 5660 | asbestoscut 100 yd/lb # used for glass and asbestos yarn |
| 5661 | |
| 5662 | tex gram / km # rational metric yarn measure, meant |
| 5663 | drex 0.1 tex # to be used for any kind of yarn |
| 5664 | poumar lb / 1e6 yard |
| 5665 | |
| 5666 | # yarn and cloth length |
| 5667 | |
| 5668 | skeincotton 80*54 inch # 80 turns of thread on a reel with a |
| 5669 | # 54 in circumference (varies for other |
| 5670 | # kinds of thread) |
| 5671 | cottonbolt 120 ft # cloth measurement |
| 5672 | woolbolt 210 ft |
| 5673 | bolt cottonbolt |
| 5674 | heer 600 yards |
| 5675 | cut 300 yards # used for wet-spun linen yarn |
| 5676 | lea 300 yards |
| 5677 | |
| 5678 | sailmakersyard 28.5 in |
| 5679 | sailmakersounce oz / sailmakersyard 36 inch |
| 5680 | |
| 5681 | silkmomme momme / 25 yards 1.49 inch # Traditional silk weight |
| 5682 | silkmm silkmomme # But it is also defined as |
| 5683 | # lb/100 yd 45 inch. The two |
| 5684 | # definitions are slightly different |
| 5685 | # and neither one seems likely to be |
| 5686 | # the true source definition. |
| 5687 | |
| 5688 | # |
| 5689 | # drug dosage |
| 5690 | # |
| 5691 | |
| 5692 | mcg microgram # Frequently used for vitamins |
| 5693 | iudiptheria 62.8 microgram # IU is for international unit |
| 5694 | iupenicillin 0.6 microgram |
| 5695 | iuinsulin 41.67 microgram |
| 5696 | drop 1|20 ml # The drop was an old "unit" that was |
| 5697 | # replaced by the minim. But I was |
| 5698 | # told by a pharmacist that in his |
| 5699 | # profession, the conversion of 20 |
| 5700 | # drops per ml is actually used. |
| 5701 | bloodunit 450 ml # For whole blood. For blood |
| 5702 | # components, a blood unit is the |
| 5703 | # quantity of the component found in a |
| 5704 | # blood unit of whole blood. The |
| 5705 | # human body contains about 12 blood |
| 5706 | # units of whole blood. |
| 5707 | |
| 5708 | # |
| 5709 | # misc medical measure |
| 5710 | # |
| 5711 | |
| 5712 | frenchcathetersize 1|3 mm # measure used for the outer diameter |
| 5713 | # of a catheter |
| 5714 | charriere frenchcathetersize |
| 5715 | |
| 5716 | |
| 5717 | # |
| 5718 | # fixup units for times when prefix handling doesn't do the job |
| 5719 | # |
| 5720 | |
| 5721 | hectare hectoare |
| 5722 | megohm megaohm |
| 5723 | kilohm kiloohm |
| 5724 | microhm microohm |
| 5725 | megalerg megaerg # 'L' added to make it pronounceable [18]. |
| 5726 | |
| 5727 | # |
| 5728 | # Money |
| 5729 | # |
| 5730 | # Note that US$ is the primitive unit so other currencies are |
| 5731 | # generally given in US$. |
| 5732 | # |
| 5733 | |
| 5734 | unitedstatesdollar US$ |
| 5735 | usdollar US$ |
| 5736 | $ dollar |
| 5737 | mark germanymark |
| 5738 | #bolivar venezuelabolivar # Not all databases are |
| 5739 | #venezuelabolivarfuerte 1e-5 bolivar # supplying these |
| 5740 | #bolivarfuerte 1e-5 bolivar # The currency was revalued |
| 5741 | #oldbolivar 1|1000 bolivarfuerte # twice |
| 5742 | peseta spainpeseta |
| 5743 | rand southafricarand |
| 5744 | escudo portugalescudo |
| 5745 | guilder netherlandsguilder |
| 5746 | hollandguilder netherlandsguilder |
| 5747 | peso mexicopeso |
| 5748 | yen japanyen |
| 5749 | lira turkeylira |
| 5750 | rupee indiarupee |
| 5751 | drachma greecedrachma |
| 5752 | franc francefranc |
| 5753 | markka finlandmarkka |
| 5754 | britainpound unitedkingdompound |
| 5755 | greatbritainpound unitedkingdompound |
| 5756 | unitedkingdompound ukpound |
| 5757 | poundsterling britainpound |
| 5758 | yuan chinayuan |
| 5759 | |
| 5760 | # Unicode Currency Names |
| 5761 | |
| 5762 | !utf8 |
| 5763 | icelandkróna icelandkrona |
| 5764 | polandzłoty polandzloty |
| 5765 | tongapa’anga tongapa'anga |
| 5766 | #venezuelabolívar venezuelabolivar |
| 5767 | vietnamđồng vietnamdong |
| 5768 | mongoliatögrög mongoliatugrik |
| 5769 | sãotomé&príncipedobra saotome&principedobra |
| 5770 | !endutf8 |
| 5771 | |
| 5772 | UKP GBP # Not an ISO code, but looks like one, and |
| 5773 | # sometimes used on usenet. |
| 5774 | |
| 5775 | !include currency.units |
| 5776 | |
| 5777 | # Money on the gold standard, used in the late 19th century and early |
| 5778 | # 20th century. |
| 5779 | |
| 5780 | olddollargold 23.22 grains goldprice # Used until 1934 |
| 5781 | newdollargold 96|7 grains goldprice # After Jan 31, 1934 |
| 5782 | dollargold newdollargold |
| 5783 | poundgold 113 grains goldprice # British pound |
| 5784 | |
| 5785 | # Precious metals |
| 5786 | |
| 5787 | goldounce goldprice troyounce |
| 5788 | silverounce silverprice troyounce |
| 5789 | platinumounce platinumprice troyounce |
| 5790 | XAU goldounce |
| 5791 | XPT platinumounce |
| 5792 | XAG silverounce |
| 5793 | |
| 5794 | # Nominal masses of US coins. Note that dimes, quarters and half dollars |
| 5795 | # have weight proportional to value. Before 1965 it was $40 / kg. |
| 5796 | |
| 5797 | USpennyweight 2.5 grams # Since 1982, 48 grains before |
| 5798 | USnickelweight 5 grams |
| 5799 | USdimeweight US$ 0.10 / (20 US$ / lb) # Since 1965 |
| 5800 | USquarterweight US$ 0.25 / (20 US$ / lb) # Since 1965 |
| 5801 | UShalfdollarweight US$ 0.50 / (20 US$ / lb) # Since 1971 |
| 5802 | USdollarweight 8.1 grams # Weight of Susan B. Anthony and |
| 5803 | # Sacagawea dollar coins |
| 5804 | |
| 5805 | # British currency |
| 5806 | |
| 5807 | quid britainpound # Slang names |
| 5808 | fiver 5 quid |
| 5809 | tenner 10 quid |
| 5810 | monkey 500 quid |
| 5811 | brgrand 1000 quid |
| 5812 | bob shilling |
| 5813 | |
| 5814 | shilling 1|20 britainpound # Before decimalisation, there |
| 5815 | oldpence 1|12 shilling # were 20 shillings to a pound, |
| 5816 | farthing 1|4 oldpence # each of twelve old pence |
| 5817 | guinea 21 shilling # Still used in horse racing |
| 5818 | crown 5 shilling |
| 5819 | florin 2 shilling |
| 5820 | groat 4 oldpence |
| 5821 | tanner 6 oldpence |
| 5822 | brpenny 0.01 britainpound |
| 5823 | pence brpenny |
| 5824 | tuppence 2 pence |
| 5825 | tuppenny tuppence |
| 5826 | ha'penny halfbrpenny |
| 5827 | hapenny ha'penny |
| 5828 | oldpenny oldpence |
| 5829 | oldtuppence 2 oldpence |
| 5830 | oldtuppenny oldtuppence |
| 5831 | threepence 3 oldpence # threepence never refers to new money |
| 5832 | threepenny threepence |
| 5833 | oldthreepence threepence |
| 5834 | oldthreepenny threepence |
| 5835 | oldhalfpenny halfoldpenny |
| 5836 | oldha'penny oldhalfpenny |
| 5837 | oldhapenny oldha'penny |
| 5838 | brpony 25 britainpound |
| 5839 | |
| 5840 | # Canadian currency |
| 5841 | |
| 5842 | loony 1 canadadollar # This coin depicts a loon |
| 5843 | toony 2 canadadollar |
| 5844 | |
| 5845 | # Cryptocurrency |
| 5846 | |
| 5847 | satoshi 1e-8 bitcoin |
| 5848 | XBT bitcoin # nonstandard code |
| 5849 | |
| 5850 | # Inflation. |
| 5851 | # |
| 5852 | # Currently US inflation as reported by the BLS CPI index is available. |
| 5853 | # The UScpi() table reports the USA consumer price index. Note that |
| 5854 | # if you specify a year like 2015, that refers to the CPI reported |
| 5855 | # for December of 2014 (which is released in mid January 2015), |
| 5856 | # so it refers to the point right at the start of the given year. |
| 5857 | # Months are increments of 1|12 on the year, so the January 2015 |
| 5858 | # release will be 2015+1|12 = 2015.08333. |
| 5859 | |
| 5860 | !include cpi.units |
| 5861 | |
| 5862 | USCPI() UScpi |
| 5863 | USCPI_now UScpi_now |
| 5864 | USCPI_lastdate UScpi_lastdate |
| 5865 | cpi() UScpi |
| 5866 | CPI() UScpi |
| 5867 | cpi_now UScpi_now |
| 5868 | CPI_now UScpi_now |
| 5869 | cpi_lastdate UScpi_lastdate |
| 5870 | CPI_lastdate UScpi_lastdate |
| 5871 | |
| 5872 | # These definitions hide the CPI index and directly convert US dollars |
| 5873 | # from a specified date to current dollars. You can use this to convert |
| 5874 | # historical dollars to present value or to convert money in the past |
| 5875 | # between two dates. |
| 5876 | |
| 5877 | dollars_in() USdollars_in |
| 5878 | US$in() USdollars_in |
| 5879 | $in() USdollars_in |
| 5880 | |
| 5881 | # This definition gives the dimensionless US inflation factor since the |
| 5882 | # specified date. |
| 5883 | |
| 5884 | inflation_since() USinflation_since |
| 5885 | |
| 5886 | |
| 5887 | # |
| 5888 | # Units used for measuring volume of wood |
| 5889 | # |
| 5890 | |
| 5891 | cord 4*4*8 ft^3 # 4 ft by 4 ft by 8 ft bundle of wood |
| 5892 | facecord 1|2 cord |
| 5893 | cordfoot 1|8 cord # One foot long section of a cord |
| 5894 | cordfeet cordfoot |
| 5895 | housecord 1|3 cord # Used to sell firewood for residences, |
| 5896 | # often confusingly called a "cord" |
| 5897 | boardfoot ft^2 inch # Usually 1 inch thick wood |
| 5898 | boardfeet boardfoot |
| 5899 | fbm boardfoot # feet board measure |
| 5900 | stack 4 yard^3 # British, used for firewood and coal [18] |
| 5901 | rick 4 ft 8 ft 16 inches # Stack of firewood, supposedly |
| 5902 | # sometimes called a face cord, but this |
| 5903 | # value is equal to 1|3 cord. Name |
| 5904 | # comes from an old Norse word for a |
| 5905 | # stack of wood. |
| 5906 | stere m^3 |
| 5907 | timberfoot ft^3 # Used for measuring solid blocks of wood |
| 5908 | standard 120 12 ft 11 in 1.5 in # This is the St Petersburg or |
| 5909 | # Pittsburg standard. Apparently the |
| 5910 | # term is short for "standard hundred" |
| 5911 | # which was meant to refer to 100 pieces |
| 5912 | # of wood (deals). However, this |
| 5913 | # particular standard is equal to 120 |
| 5914 | # deals which are 12 ft by 11 in by 1.5 |
| 5915 | # inches (not the standard deal). |
| 5916 | hoppusfoot (4/pi) ft^3 # Volume calculation suggested in 1736 |
| 5917 | hoppusboardfoot 1|12 hoppusfoot # forestry manual by Edward Hoppus, for |
| 5918 | hoppuston 50 hoppusfoot # estimating the usable volume of a log. |
| 5919 | # It results from computing the volume |
| 5920 | # of a cylindrical log of length, L, and |
| 5921 | # girth (circumference), G, by V=L(G/4)^2. |
| 5922 | # The hoppus ton is apparently still in |
| 5923 | # use for shipments from Southeast Asia. |
| 5924 | |
| 5925 | # In Britain, the deal is apparently any piece of wood over 6 feet long, over |
| 5926 | # 7 wide and 2.5 inches thick. The OED doesn't give a standard size. A piece |
| 5927 | # of wood less than 7 inches wide is called a "batten". This unit is now used |
| 5928 | # exclusively for fir and pine. |
| 5929 | |
| 5930 | deal 12 ft 11 in 2.5 in # The standard North American deal [OED] |
| 5931 | wholedeal 12 ft 11 in 1.25 in # If it's half as thick as the standard |
| 5932 | # deal it's called a "whole deal"! |
| 5933 | splitdeal 12 ft 11 in 5|8 in # And half again as thick is a split deal. |
| 5934 | |
| 5935 | |
| 5936 | # Used for shellac mixing rate |
| 5937 | |
| 5938 | poundcut pound / gallon |
| 5939 | lbcut poundcut |
| 5940 | |
| 5941 | # |
| 5942 | # Gas and Liquid flow units |
| 5943 | # |
| 5944 | |
| 5945 | FLUID_FLOW VOLUME / TIME |
| 5946 | |
| 5947 | # Some obvious volumetric gas flow units (cu is short for cubic) |
| 5948 | |
| 5949 | cumec m^3/s |
| 5950 | cusec ft^3/s |
| 5951 | |
| 5952 | # Conventional abbreviations for fluid flow units |
| 5953 | |
| 5954 | gph gal/hr |
| 5955 | gpm gal/min |
| 5956 | mgd megagal/day |
| 5957 | brgph brgallon/hr |
| 5958 | brgpm brgallon/min |
| 5959 | brmgd mega brgallon/day |
| 5960 | usgph usgallon/hr |
| 5961 | usgpm usgallon/min |
| 5962 | usmgd mega usgallon/day |
| 5963 | cfs ft^3/s |
| 5964 | cfh ft^3/hour |
| 5965 | cfm ft^3/min |
| 5966 | lpm liter/min |
| 5967 | lfm ft/min # Used to report air flow produced by fans. |
| 5968 | # Multiply by cross sectional area to get a |
| 5969 | # flow in cfm. |
| 5970 | |
| 5971 | pru mmHg / (ml/min) # peripheral resistance unit, used in |
| 5972 | # medicine to assess blood flow in |
| 5973 | # the capillaries. |
| 5974 | |
| 5975 | # Miner's inch: This is an old historic unit used in the Western United |
| 5976 | # States. It is generally defined as the rate of flow through a one square |
| 5977 | # inch hole at a specified depth such as 4 inches. In the late 19th century, |
| 5978 | # volume of water was sometimes measured in the "24 hour inch". Values for the |
| 5979 | # miner's inch were fixed by state statues. (This information is from a web |
| 5980 | # site operated by the Nevada Division of Water Planning: The Water Words |
| 5981 | # Dictionary at http://water.nv.gov/WaterPlanDictionary.aspx, specifically |
| 5982 | # http://water.nv.gov/programs/planning/dictionary/wwords-M.pdf. All |
| 5983 | # but minersinchNV are s.v. Miner's Inch [Western United States]) |
| 5984 | |
| 5985 | minersinchAZ 1.5 ft^3/min |
| 5986 | minersinchCA 1.5 ft^3/min |
| 5987 | minersinchMT 1.5 ft^3/min |
| 5988 | minersinchNV 1.5 ft^3/min |
| 5989 | minersinchOR 1.5 ft^3/min |
| 5990 | minersinchID 1.2 ft^3/min |
| 5991 | minersinchKS 1.2 ft^3/min |
| 5992 | minersinchNE 1.2 ft^3/min |
| 5993 | minersinchNM 1.2 ft^3/min |
| 5994 | minersinchND 1.2 ft^3/min |
| 5995 | minersinchSD 1.2 ft^3/min |
| 5996 | minersinchUT 1.2 ft^3/min |
| 5997 | minersinchCO 1 ft^3/sec / 38.4 # 38.4 miner's inches = 1 ft^3/sec |
| 5998 | minersinchBC 1.68 ft^3/min # British Columbia |
| 5999 | |
| 6000 | # Oceanographic flow |
| 6001 | |
| 6002 | sverdrup 1e6 m^3 / sec # Used to express flow of ocean |
| 6003 | # currents. Named after Norwegian |
| 6004 | # oceanographer H. Sverdrup. |
| 6005 | |
| 6006 | # In vacuum science and some other applications, gas flow is measured |
| 6007 | # as the product of volumetric flow and pressure. This is useful |
| 6008 | # because it makes it easy to compare with the flow at standard |
| 6009 | # pressure (one atmosphere). It also directly relates to the number |
| 6010 | # of gas molecules per unit time, and hence to the mass flow if the |
| 6011 | # molecular mass is known. |
| 6012 | |
| 6013 | GAS_FLOW PRESSURE FLUID_FLOW |
| 6014 | |
| 6015 | sccm atm cc/min # 's' is for "standard" to indicate |
| 6016 | sccs atm cc/sec # flow at standard pressure |
| 6017 | scfh atm ft^3/hour # |
| 6018 | scfm atm ft^3/min |
| 6019 | slpm atm liter/min |
| 6020 | slph atm liter/hour |
| 6021 | lusec liter micron Hg / s # Used in vacuum science |
| 6022 | |
| 6023 | # US Standard Atmosphere (1976) |
| 6024 | # Atmospheric temperature and pressure vs. geometric height above sea level |
| 6025 | # This definition covers only the troposphere (the lowest atmospheric |
| 6026 | # layer, up to 11 km), and assumes the layer is polytropic. |
| 6027 | # A polytropic process is one for which PV^k = const, where P is the |
| 6028 | # pressure, V is the volume, and k is the polytropic exponent. The |
| 6029 | # polytropic index is n = 1 / (k - 1). As noted in the Wikipedia article |
| 6030 | # https://en.wikipedia.org/wiki/Polytropic_process, some authors reverse |
| 6031 | # the definitions of "exponent" and "index." The functions below assume |
| 6032 | # the following parameters: |
| 6033 | |
| 6034 | # temperature lapse rate, -dT/dz, in troposphere |
| 6035 | |
| 6036 | lapserate 6.5 K/km # US Std Atm (1976) |
| 6037 | |
| 6038 | # air molecular weight, including constituent mol wt, given |
| 6039 | # in Table 3, p. 3; CH4 (16.04303) and N2O (44.0128) from |
| 6040 | # Table 15, p. 33. Values for molecular weights are slightly |
| 6041 | # different from current values, so the original numerical |
| 6042 | # values are retained. |
| 6043 | |
| 6044 | air_1976 78.084 % 28.0134 \ |
| 6045 | + 20.9476 % 31.9988 \ |
| 6046 | + 9340 ppm 39.948 \ |
| 6047 | + 314 ppm 44.00995 \ |
| 6048 | + 18.18 ppm 20.183 \ |
| 6049 | + 5.24 ppm 4.0026 \ |
| 6050 | + 1.5 ppm 16.04303 \ |
| 6051 | + 1.14 ppm 83.80 \ |
| 6052 | + 0.5 ppm 2.01594 \ |
| 6053 | + 0.27 ppm 44.0128 \ |
| 6054 | + 0.087 ppm 131.30 |
| 6055 | |
| 6056 | # from US Standard Atmosphere, 1962, Table I.2.7, p. 9 |
| 6057 | |
| 6058 | air_1962 78.084 % 28.0134 \ |
| 6059 | + 20.9476 % 31.9988 \ |
| 6060 | + 9340 ppm 39.948 \ |
| 6061 | + 314 ppm 44.00995 \ |
| 6062 | + 18.18 ppm 20.183 \ |
| 6063 | + 5.24 ppm 4.0026 \ |
| 6064 | + 2 ppm 16.04303 \ |
| 6065 | + 1.14 ppm 83.80 \ |
| 6066 | + 0.5 ppm 2.01594 \ |
| 6067 | + 0.5 ppm 44.0128 \ |
| 6068 | + 0.087 ppm 131.30 |
| 6069 | |
| 6070 | # Average molecular weight of air |
| 6071 | # |
| 6072 | # Concentration of greenhouse gases CO2, CH4, and N20 are from |
| 6073 | # https://gml.noaa.gov/ccgg/trends/global.html (accessed 2023-04-10); |
| 6074 | # others are from NASA Earth Fact Sheet |
| 6075 | # https://nssdc.gsfc.nasa.gov/planetary/factsheet/earthfact.html (accessed 2023-04-10) |
| 6076 | # Numbers do not add up to exactly 100% due to roundoff and uncertainty. Water |
| 6077 | # is highly variable, typically makes up about 1% |
| 6078 | |
| 6079 | air_2023 78.08% nitrogen 2 \ |
| 6080 | + 20.95% oxygen 2 \ |
| 6081 | + 9340 ppm argon \ |
| 6082 | + 419 ppm (carbon + oxygen 2) \ |
| 6083 | + 18.18 ppm neon \ |
| 6084 | + 5.24 ppm helium \ |
| 6085 | + 1.92 ppm (carbon + 4 hydrogen) \ |
| 6086 | + 1.14 ppm krypton \ |
| 6087 | + 0.55 ppm hydrogen 2 \ |
| 6088 | + 0.34 ppm (nitrogen 2 + oxygen) |
| 6089 | |
| 6090 | # from NASA Earth Fact Sheet (accessed 28 August 2015) |
| 6091 | # http://nssdc.gsfc.nasa.gov/planetary/factsheet/earthfact.html |
| 6092 | |
| 6093 | air_2015 78.08% nitrogen 2 \ |
| 6094 | + 20.95% oxygen 2 \ |
| 6095 | + 9340 ppm argon \ |
| 6096 | + 400 ppm (carbon + oxygen 2) \ |
| 6097 | + 18.18 ppm neon \ |
| 6098 | + 5.24 ppm helium \ |
| 6099 | + 1.7 ppm (carbon + 4 hydrogen) \ |
| 6100 | + 1.14 ppm krypton \ |
| 6101 | + 0.55 ppm hydrogen 2 |
| 6102 | |
| 6103 | air air_2023 |
| 6104 | |
| 6105 | # universal gas constant |
| 6106 | R_1976 8.31432e3 N m/(kmol K) |
| 6107 | |
| 6108 | # polytropic index n |
| 6109 | polyndx_1976 air_1976 (kg/kmol) gravity/(R_1976 lapserate) - 1 |
| 6110 | |
| 6111 | # If desired, redefine using current values for air mol wt and R |
| 6112 | |
| 6113 | polyndx polyndx_1976 |
| 6114 | # polyndx air (kg/kmol) gravity/(R lapserate) - 1 |
| 6115 | |
| 6116 | # for comparison with various references |
| 6117 | |
| 6118 | polyexpnt (polyndx + 1) / polyndx |
| 6119 | |
| 6120 | # The model assumes the following reference values: |
| 6121 | # sea-level temperature and pressure |
| 6122 | |
| 6123 | stdatmT0 288.15 K |
| 6124 | stdatmP0 atm |
| 6125 | |
| 6126 | # "effective radius" for relation of geometric to geopotential height, |
| 6127 | # at a latitude at which g = 9.80665 m/s (approximately 45.543 deg); no |
| 6128 | # relation to actual radius |
| 6129 | |
| 6130 | earthradUSAtm 6356766 m |
| 6131 | |
| 6132 | # Temperature vs. geopotential height h |
| 6133 | # Assumes 15 degC at sea level |
| 6134 | # Based on approx 45 deg latitude |
| 6135 | # Lower limits of domain and upper limits of range are those of the |
| 6136 | # tables in US Standard Atmosphere (NASA 1976) |
| 6137 | |
| 6138 | stdatmTH(h) units=[m;K] domain=[-5000,11e3] range=[217,321] \ |
| 6139 | stdatmT0+(-lapserate h) ; (stdatmT0+(-stdatmTH))/lapserate |
| 6140 | |
| 6141 | # Temperature vs. geometric height z; based on approx 45 deg latitude |
| 6142 | stdatmT(z) units=[m;K] domain=[-5000,11e3] range=[217,321] \ |
| 6143 | stdatmTH(geop_ht(z)) ; ~geop_ht(~stdatmTH(stdatmT)) |
| 6144 | |
| 6145 | # Pressure vs. geopotential height h |
| 6146 | # Assumes 15 degC and 101325 Pa at sea level |
| 6147 | # Based on approx 45 deg latitude |
| 6148 | # Lower limits of domain and upper limits of range are those of the |
| 6149 | # tables in US Standard Atmosphere (NASA 1976) |
| 6150 | |
| 6151 | stdatmPH(h) units=[m;Pa] domain=[-5000,11e3] range=[22877,177764] \ |
| 6152 | atm (1 - (lapserate/stdatmT0) h)^(polyndx + 1) ; \ |
| 6153 | (stdatmT0/lapserate) (1+(-(stdatmPH/stdatmP0)^(1/(polyndx + 1)))) |
| 6154 | |
| 6155 | # Pressure vs. geometric height z; based on approx 45 deg latitude |
| 6156 | stdatmP(z) units=[m;Pa] domain=[-5000,11e3] range=[22877,177764] \ |
| 6157 | stdatmPH(geop_ht(z)); ~geop_ht(~stdatmPH(stdatmP)) |
| 6158 | |
| 6159 | # Geopotential height from geometric height |
| 6160 | # Based on approx 45 deg latitude |
| 6161 | # Lower limits of domain and range are somewhat arbitrary; they |
| 6162 | # correspond to the limits in the US Std Atm tables |
| 6163 | |
| 6164 | geop_ht(z) units=[m;m] domain=[-5000,) range=[-5004,) \ |
| 6165 | (earthradUSAtm z) / (earthradUSAtm + z) ; \ |
| 6166 | (earthradUSAtm geop_ht) / (earthradUSAtm + (-geop_ht)) |
| 6167 | |
| 6168 | # The standard value for the sea-level acceleration due to gravity is |
| 6169 | # 9.80665 m/s^2, but the actual value varies with latitude (Harrison 1949) |
| 6170 | # R_eff = 2 g_phi / denom |
| 6171 | # g_phi = 978.0356e-2 (1+0.0052885 sin(lat)^2+(-0.0000059) sin(2 lat)^2) |
| 6172 | # or |
| 6173 | # g_phi = 980.6160e-2 (1+(-0.0026373) cos(2 lat)+0.0000059 cos(2 lat)^2) |
| 6174 | # denom = 3.085462e-6+2.27e-9 cos(2 lat)+(-2e-12) cos(4 lat) (minutes?) |
| 6175 | # There is no inverse function; the standard value applies at a latitude |
| 6176 | # of about 45.543 deg |
| 6177 | |
| 6178 | g_phi(lat) units=[deg;m/s2] domain=[0,90] noerror \ |
| 6179 | 980.6160e-2 (1+(-0.0026373) cos(2 lat)+0.0000059 cos(2 lat)^2) m/s2 |
| 6180 | |
| 6181 | # effective Earth radius for relation of geometric height to |
| 6182 | # geopotential height, as function of latitude (Harrison 1949) |
| 6183 | |
| 6184 | earthradius_eff(lat) units=[deg;m] domain=[0,90] noerror \ |
| 6185 | m 2 9.780356 (1+0.0052885 sin(lat)^2+(-0.0000059) sin(2 lat)^2) / \ |
| 6186 | (3.085462e-6 + 2.27e-9 cos(2 lat) + (-2e-12) cos(4 lat)) |
| 6187 | |
| 6188 | # References |
| 6189 | # Harrison, L.P. 1949. Relation Between Geopotential and Geometric |
| 6190 | # Height. In Smithsonian Meteorological Tables. List, Robert J., ed. |
| 6191 | # 6th ed., 4th reprint, 1968. Washington, DC: Smithsonian Institution. |
| 6192 | # NASA. US National Aeronautics and Space Administration. 1976. |
| 6193 | # US Standard Atmosphere 1976. Washington, DC: US Government Printing Office. |
| 6194 | |
| 6195 | # Gauge pressure functions |
| 6196 | # |
| 6197 | # Gauge pressure is measured relative to atmospheric pressure. In the English |
| 6198 | # system, where pressure is often given in pounds per square inch, gauge |
| 6199 | # pressure is often indicated by 'psig' to distinguish it from absolute |
| 6200 | # pressure, often indicated by 'psia'. At the standard atmospheric pressure |
| 6201 | # of 14.696 psia, a gauge pressure of 0 psig is an absolute pressure of 14.696 |
| 6202 | # psia; an automobile tire inflated to 31 psig has an absolute pressure of |
| 6203 | # 45.696 psia. |
| 6204 | # |
| 6205 | # With gaugepressure(), the units must be specified (e.g., gaugepressure(1.5 |
| 6206 | # bar)); with psig(), the units are taken as psi, so the example above of tire |
| 6207 | # pressure could be given as psig(31). |
| 6208 | # |
| 6209 | # If the normal elevation is significantly different from sea level, change |
| 6210 | # Patm appropriately, and adjust the lower domain limit on the gaugepressure |
| 6211 | # definition. |
| 6212 | |
| 6213 | Patm atm |
| 6214 | |
| 6215 | gaugepressure(x) units=[Pa;Pa] domain=[-101325,) range=[0,) \ |
| 6216 | x + Patm ; gaugepressure+(-Patm) |
| 6217 | |
| 6218 | psig(x) units=[1;Pa] domain=[-14.6959487755135,) range=[0,) \ |
| 6219 | gaugepressure(x psi) ; ~gaugepressure(psig) / psi |
| 6220 | |
| 6221 | |
| 6222 | # Pressure for underwater diving |
| 6223 | |
| 6224 | seawater 0.1 bar / meter |
| 6225 | msw meter seawater |
| 6226 | fsw foot seawater |
| 6227 | |
| 6228 | # |
| 6229 | # Wire Gauge |
| 6230 | # |
| 6231 | # This area is a nightmare with huge charts of wire gauge diameters |
| 6232 | # that usually have no clear origin. There are at least 5 competing wire gauge |
| 6233 | # systems to add to the confusion. The use of wire gauge is related to the |
| 6234 | # manufacturing method: a metal rod is heated and drawn through a hole. The |
| 6235 | # size change can't be too big. To get smaller wires, the process is repeated |
| 6236 | # with a series of smaller holes. Generally larger gauges mean smaller wires. |
| 6237 | # The gauges often have values such as "00" and "000" which are larger sizes |
| 6238 | # than simply "0" gauge. In the tables that appear below, these gauges must be |
| 6239 | # specified as negative numbers (e.g. "00" is -1, "000" is -2, etc). |
| 6240 | # Alternatively, you can use the following units: |
| 6241 | # |
| 6242 | |
| 6243 | g00 (-1) |
| 6244 | g000 (-2) |
| 6245 | g0000 (-3) |
| 6246 | g00000 (-4) |
| 6247 | g000000 (-5) |
| 6248 | g0000000 (-6) |
| 6249 | |
| 6250 | # American Wire Gauge (AWG) or Brown & Sharpe Gauge appears to be the most |
| 6251 | # important gauge. ASTM B-258 specifies that this gauge is based on geometric |
| 6252 | # interpolation between gauge 0000, which is 0.46 inches exactly, and gauge 36 |
| 6253 | # which is 0.005 inches exactly. Therefore, the diameter in inches of a wire |
| 6254 | # is given by the formula 1|200 92^((36-g)/39). Note that 92^(1/39) is close |
| 6255 | # to 2^(1/6), so diameter is approximately halved for every 6 gauges. For the |
| 6256 | # repeated zero values, use negative numbers in the formula. The same document |
| 6257 | # also specifies rounding rules which seem to be ignored by makers of tables. |
| 6258 | # Gauges up to 44 are to be specified with up to 4 significant figures, but no |
| 6259 | # closer than 0.0001 inch. Gauges from 44 to 56 are to be rounded to the |
| 6260 | # nearest 0.00001 inch. |
| 6261 | # |
| 6262 | # In addition to being used to measure wire thickness, this gauge is used to |
| 6263 | # measure the thickness of sheets of aluminum, copper, and most metals other |
| 6264 | # than steel, iron and zinc. |
| 6265 | |
| 6266 | wiregauge(g) units=[1;m] range=(0,) \ |
| 6267 | 1|200 92^((36+(-g))/39) in; 36+(-39)ln(200 wiregauge/in)/ln(92) |
| 6268 | awg() wiregauge |
| 6269 | |
| 6270 | # Next we have the SWG, the Imperial or British Standard Wire Gauge. This one |
| 6271 | # is piecewise linear. It was used for aluminum sheets but also shows up for |
| 6272 | # wire used in jewelry. |
| 6273 | |
| 6274 | brwiregauge[in] \ |
| 6275 | -6 0.5 \ |
| 6276 | -5 0.464 \ |
| 6277 | -3 0.4 \ |
| 6278 | -2 0.372 \ |
| 6279 | 3 0.252 \ |
| 6280 | 6 0.192 \ |
| 6281 | 10 0.128 \ |
| 6282 | 14 0.08 \ |
| 6283 | 19 0.04 \ |
| 6284 | 23 0.024 \ |
| 6285 | 26 0.018 \ |
| 6286 | 28 0.0148 \ |
| 6287 | 30 0.0124 \ |
| 6288 | 39 0.0052 \ |
| 6289 | 49 0.0012 \ |
| 6290 | 50 0.001 |
| 6291 | |
| 6292 | swg() brwiregauge |
| 6293 | |
| 6294 | # The following is from the Appendix to ASTM B 258 |
| 6295 | # |
| 6296 | # For example, in U.S. gage, the standard for sheet metal is based on the |
| 6297 | # weight of the metal, not on the thickness. 16-gage is listed as |
| 6298 | # approximately .0625 inch thick and 40 ounces per square foot (the original |
| 6299 | # standard was based on wrought iron at .2778 pounds per cubic inch; steel |
| 6300 | # has almost entirely superseded wrought iron for sheet use, at .2833 pounds |
| 6301 | # per cubic inch). Smaller numbers refer to greater thickness. There is no |
| 6302 | # formula for converting gage to thickness or weight. |
| 6303 | # |
| 6304 | # It's rather unclear from the passage above whether the plate gauge values are |
| 6305 | # therefore wrong if steel is being used. Reference [15] states that steel is |
| 6306 | # in fact measured using this gauge (under the name Manufacturers' Standard |
| 6307 | # Gauge) with a density of 501.84 lb/ft3 = 0.2904 lb/in3 used for steel. |
| 6308 | # But this doesn't seem to be the correct density of steel (.2833 lb/in3 is |
| 6309 | # closer). |
| 6310 | # |
| 6311 | # This gauge was established in 1893 for purposes of taxation. |
| 6312 | |
| 6313 | # Old plate gauge for iron |
| 6314 | |
| 6315 | plategauge[(oz/ft^2)/(480*lb/ft^3)] \ |
| 6316 | -5 300 \ |
| 6317 | 1 180 \ |
| 6318 | 14 50 \ |
| 6319 | 16 40 \ |
| 6320 | 17 36 \ |
| 6321 | 20 24 \ |
| 6322 | 26 12 \ |
| 6323 | 31 7 \ |
| 6324 | 36 4.5 \ |
| 6325 | 38 4 |
| 6326 | |
| 6327 | # Manufacturers Standard Gage |
| 6328 | |
| 6329 | stdgauge[(oz/ft^2)/(501.84*lb/ft^3)] \ |
| 6330 | -5 300 \ |
| 6331 | 1 180 \ |
| 6332 | 14 50 \ |
| 6333 | 16 40 \ |
| 6334 | 17 36 \ |
| 6335 | 20 24 \ |
| 6336 | 26 12 \ |
| 6337 | 31 7 \ |
| 6338 | 36 4.5 \ |
| 6339 | 38 4 |
| 6340 | |
| 6341 | # A special gauge is used for zinc sheet metal. Notice that larger gauges |
| 6342 | # indicate thicker sheets. |
| 6343 | |
| 6344 | zincgauge[in] \ |
| 6345 | 1 0.002 \ |
| 6346 | 10 0.02 \ |
| 6347 | 15 0.04 \ |
| 6348 | 19 0.06 \ |
| 6349 | 23 0.1 \ |
| 6350 | 24 0.125 \ |
| 6351 | 27 0.5 \ |
| 6352 | 28 1 |
| 6353 | |
| 6354 | # |
| 6355 | # Imperial drill bit sizes are reported in inches or in a numerical or |
| 6356 | # letter gauge. |
| 6357 | # |
| 6358 | |
| 6359 | drillgauge[in] \ |
| 6360 | 1 0.2280 \ |
| 6361 | 2 0.2210 \ |
| 6362 | 3 0.2130 \ |
| 6363 | 4 0.2090 \ |
| 6364 | 5 0.2055 \ |
| 6365 | 6 0.2040 \ |
| 6366 | 7 0.2010 \ |
| 6367 | 8 0.1990 \ |
| 6368 | 9 0.1960 \ |
| 6369 | 10 0.1935 \ |
| 6370 | 11 0.1910 \ |
| 6371 | 12 0.1890 \ |
| 6372 | 13 0.1850 \ |
| 6373 | 14 0.1820 \ |
| 6374 | 15 0.1800 \ |
| 6375 | 16 0.1770 \ |
| 6376 | 17 0.1730 \ |
| 6377 | 18 0.1695 \ |
| 6378 | 19 0.1660 \ |
| 6379 | 20 0.1610 \ |
| 6380 | 22 0.1570 \ |
| 6381 | 23 0.1540 \ |
| 6382 | 24 0.1520 \ |
| 6383 | 25 0.1495 \ |
| 6384 | 26 0.1470 \ |
| 6385 | 27 0.1440 \ |
| 6386 | 28 0.1405 \ |
| 6387 | 29 0.1360 \ |
| 6388 | 30 0.1285 \ |
| 6389 | 31 0.1200 \ |
| 6390 | 32 0.1160 \ |
| 6391 | 33 0.1130 \ |
| 6392 | 34 0.1110 \ |
| 6393 | 35 0.1100 \ |
| 6394 | 36 0.1065 \ |
| 6395 | 38 0.1015 \ |
| 6396 | 39 0.0995 \ |
| 6397 | 40 0.0980 \ |
| 6398 | 41 0.0960 \ |
| 6399 | 42 0.0935 \ |
| 6400 | 43 0.0890 \ |
| 6401 | 44 0.0860 \ |
| 6402 | 45 0.0820 \ |
| 6403 | 46 0.0810 \ |
| 6404 | 48 0.0760 \ |
| 6405 | 51 0.0670 \ |
| 6406 | 52 0.0635 \ |
| 6407 | 53 0.0595 \ |
| 6408 | 54 0.0550 \ |
| 6409 | 55 0.0520 \ |
| 6410 | 56 0.0465 \ |
| 6411 | 57 0.0430 \ |
| 6412 | 65 0.0350 \ |
| 6413 | 66 0.0330 \ |
| 6414 | 68 0.0310 \ |
| 6415 | 69 0.0292 \ |
| 6416 | 70 0.0280 \ |
| 6417 | 71 0.0260 \ |
| 6418 | 73 0.0240 \ |
| 6419 | 74 0.0225 \ |
| 6420 | 75 0.0210 \ |
| 6421 | 76 0.0200 \ |
| 6422 | 78 0.0160 \ |
| 6423 | 79 0.0145 \ |
| 6424 | 80 0.0135 \ |
| 6425 | 88 0.0095 \ |
| 6426 | 104 0.0031 |
| 6427 | |
| 6428 | drillA 0.234 in |
| 6429 | drillB 0.238 in |
| 6430 | drillC 0.242 in |
| 6431 | drillD 0.246 in |
| 6432 | drillE 0.250 in |
| 6433 | drillF 0.257 in |
| 6434 | drillG 0.261 in |
| 6435 | drillH 0.266 in |
| 6436 | drillI 0.272 in |
| 6437 | drillJ 0.277 in |
| 6438 | drillK 0.281 in |
| 6439 | drillL 0.290 in |
| 6440 | drillM 0.295 in |
| 6441 | drillN 0.302 in |
| 6442 | drillO 0.316 in |
| 6443 | drillP 0.323 in |
| 6444 | drillQ 0.332 in |
| 6445 | drillR 0.339 in |
| 6446 | drillS 0.348 in |
| 6447 | drillT 0.358 in |
| 6448 | drillU 0.368 in |
| 6449 | drillV 0.377 in |
| 6450 | drillW 0.386 in |
| 6451 | drillX 0.397 in |
| 6452 | drillY 0.404 in |
| 6453 | drillZ 0.413 in |
| 6454 | |
| 6455 | # |
| 6456 | # Screw sizes |
| 6457 | # |
| 6458 | # In the USA, screw diameters for both wood screws and machine screws |
| 6459 | # are reported using a gauge number. Metric machine screws are |
| 6460 | # reported as Mxx where xx is the diameter in mm. |
| 6461 | # |
| 6462 | |
| 6463 | screwgauge(g) units=[1;m] range=[0,) \ |
| 6464 | (.06 + .013 g) in ; (screwgauge/in + (-.06)) / .013 |
| 6465 | |
| 6466 | # |
| 6467 | # Abrasive grit size |
| 6468 | # |
| 6469 | # Standards governing abrasive grit sizes are complicated, specifying |
| 6470 | # fractions of particles that are passed or retained by different mesh |
| 6471 | # sizes. As a result, it is not possible to make precise comparisons |
| 6472 | # of different grit standards. The tables below allow the |
| 6473 | # determination of rough equivlants by using median particle size. |
| 6474 | # |
| 6475 | # Standards in the USA are determined by the Unified Abrasives |
| 6476 | # Manufacturers' Association (UAMA), which resulted from the merger of |
| 6477 | # several previous organizations. One of the old organizations was |
| 6478 | # CAMI (Coated Abrasives Manufacturers' Institute). |
| 6479 | # |
| 6480 | # UAMA has a web page with plots showing abrasive particle ranges for |
| 6481 | # various different grits and comparisons between standards. |
| 6482 | # |
| 6483 | # https://uama.org/abrasives-101/ |
| 6484 | # |
| 6485 | # Abrasives are grouped into "bonded" abrasives for use with grinding |
| 6486 | # wheels and "coated" abrasives for sandpapers and abrasive films. |
| 6487 | # The industry uses different grit standards for these two |
| 6488 | # categories. |
| 6489 | # |
| 6490 | # Another division is between "macrogrits", grits below 240 and |
| 6491 | # "microgrits", which are above 240. Standards differ, as do methods |
| 6492 | # for determining particle size. In the USA, ANSI B74.12 is the |
| 6493 | # standard governing macrogrits. ANSI B74.10 covers bonded microgrit |
| 6494 | # abrasives, and ANSI B74.18 covers coated microgrit abrasives. It |
| 6495 | # appears that the coated standard is identical to the bonded standard |
| 6496 | # for grits up through 600 but then diverges significantly. |
| 6497 | # |
| 6498 | # European grit sizes are determined by the Federation of European |
| 6499 | # Producers of Abrasives. http://www.fepa-abrasives.org |
| 6500 | # |
| 6501 | # They give two standards, the "F" grit for bonded abrasives and the |
| 6502 | # "P" grit for coated abrasives. This data is taken directly from |
| 6503 | # their web page. |
| 6504 | |
| 6505 | # FEPA P grit for coated abrasives is commonly seen on sandpaper in |
| 6506 | # the USA where the paper will be marked P600, for example. FEPA P |
| 6507 | # grits are said to be more tightly constrained than comparable ANSI |
| 6508 | # grits so that the particles are more uniform in size and hence give |
| 6509 | # a better finish. |
| 6510 | |
| 6511 | grit_P[micron] \ |
| 6512 | 12 1815 \ |
| 6513 | 16 1324 \ |
| 6514 | 20 1000 \ |
| 6515 | 24 764 \ |
| 6516 | 30 642 \ |
| 6517 | 36 538 \ |
| 6518 | 40 425 \ |
| 6519 | 50 336 \ |
| 6520 | 60 269 \ |
| 6521 | 80 201 \ |
| 6522 | 100 162 \ |
| 6523 | 120 125 \ |
| 6524 | 150 100 \ |
| 6525 | 180 82 \ |
| 6526 | 220 68 \ |
| 6527 | 240 58.5 \ |
| 6528 | 280 52.2 \ |
| 6529 | 320 46.2 \ |
| 6530 | 360 40.5 \ |
| 6531 | 400 35 \ |
| 6532 | 500 30.2 \ |
| 6533 | 600 25.8 \ |
| 6534 | 800 21.8 \ |
| 6535 | 1000 18.3 \ |
| 6536 | 1200 15.3 \ |
| 6537 | 1500 12.6 \ |
| 6538 | 2000 10.3 \ |
| 6539 | 2500 8.4 |
| 6540 | |
| 6541 | # The F grit is the European standard for bonded abrasives such as |
| 6542 | # grinding wheels |
| 6543 | |
| 6544 | grit_F[micron] \ |
| 6545 | 4 4890 \ |
| 6546 | 5 4125 \ |
| 6547 | 6 3460 \ |
| 6548 | 7 2900 \ |
| 6549 | 8 2460 \ |
| 6550 | 10 2085 \ |
| 6551 | 12 1765 \ |
| 6552 | 14 1470 \ |
| 6553 | 16 1230 \ |
| 6554 | 20 1040 \ |
| 6555 | 22 885 \ |
| 6556 | 24 745 \ |
| 6557 | 30 625 \ |
| 6558 | 36 525 \ |
| 6559 | 40 438 \ |
| 6560 | 46 370 \ |
| 6561 | 54 310 \ |
| 6562 | 60 260 \ |
| 6563 | 70 218 \ |
| 6564 | 80 185 \ |
| 6565 | 90 154 \ |
| 6566 | 100 129 \ |
| 6567 | 120 109 \ |
| 6568 | 150 82 \ |
| 6569 | 180 69 \ |
| 6570 | 220 58 \ |
| 6571 | 230 53 \ |
| 6572 | 240 44.5 \ |
| 6573 | 280 36.5 \ |
| 6574 | 320 29.2 \ |
| 6575 | 360 22.8 \ |
| 6576 | 400 17.3 \ |
| 6577 | 500 12.8 \ |
| 6578 | 600 9.3 \ |
| 6579 | 800 6.5 \ |
| 6580 | 1000 4.5 \ |
| 6581 | 1200 3 \ |
| 6582 | 1500 2.0 \ |
| 6583 | 2000 1.2 |
| 6584 | |
| 6585 | # According to the UAMA web page, the ANSI bonded and ANSI coated standards |
| 6586 | # are identical to FEPA F in the macrogrit range (under 240 grit), so these |
| 6587 | # values are taken from the FEPA F table. The values for 240 and above are |
| 6588 | # from the UAMA web site and represent the average of the "d50" range |
| 6589 | # endpoints listed there. |
| 6590 | |
| 6591 | ansibonded[micron] \ |
| 6592 | 4 4890 \ |
| 6593 | 5 4125 \ |
| 6594 | 6 3460 \ |
| 6595 | 7 2900 \ |
| 6596 | 8 2460 \ |
| 6597 | 10 2085 \ |
| 6598 | 12 1765 \ |
| 6599 | 14 1470 \ |
| 6600 | 16 1230 \ |
| 6601 | 20 1040 \ |
| 6602 | 22 885 \ |
| 6603 | 24 745 \ |
| 6604 | 30 625 \ |
| 6605 | 36 525 \ |
| 6606 | 40 438 \ |
| 6607 | 46 370 \ |
| 6608 | 54 310 \ |
| 6609 | 60 260 \ |
| 6610 | 70 218 \ |
| 6611 | 80 185 \ |
| 6612 | 90 154 \ |
| 6613 | 100 129 \ |
| 6614 | 120 109 \ |
| 6615 | 150 82 \ |
| 6616 | 180 69 \ |
| 6617 | 220 58 \ |
| 6618 | 240 50 \ |
| 6619 | 280 39.5 \ |
| 6620 | 320 29.5 \ |
| 6621 | 360 23 \ |
| 6622 | 400 18.25 \ |
| 6623 | 500 13.9 \ |
| 6624 | 600 10.55 \ |
| 6625 | 800 7.65 \ |
| 6626 | 1000 5.8 \ |
| 6627 | 1200 3.8 |
| 6628 | |
| 6629 | grit_ansibonded() ansibonded |
| 6630 | |
| 6631 | # Like the bonded grit, the coated macrogrits below 240 are taken from the |
| 6632 | # FEPA F table. Data above this is from the UAMA site. Note that the coated |
| 6633 | # and bonded standards are evidently the same from 240 up to 600 grit, but |
| 6634 | # starting at 800 grit, the coated standard diverges. The data from UAMA show |
| 6635 | # that 800 grit coated has an average size slightly larger than the average |
| 6636 | # size of 600 grit coated/bonded. However, the 800 grit has a significantly |
| 6637 | # smaller particle size variation. |
| 6638 | # |
| 6639 | # Because of this non-monotonicity from 600 grit to 800 grit this definition |
| 6640 | # produces a warning about the lack of a unique inverse. |
| 6641 | |
| 6642 | ansicoated[micron] noerror \ |
| 6643 | 4 4890 \ |
| 6644 | 5 4125 \ |
| 6645 | 6 3460 \ |
| 6646 | 7 2900 \ |
| 6647 | 8 2460 \ |
| 6648 | 10 2085 \ |
| 6649 | 12 1765 \ |
| 6650 | 14 1470 \ |
| 6651 | 16 1230 \ |
| 6652 | 20 1040 \ |
| 6653 | 22 885 \ |
| 6654 | 24 745 \ |
| 6655 | 30 625 \ |
| 6656 | 36 525 \ |
| 6657 | 40 438 \ |
| 6658 | 46 370 \ |
| 6659 | 54 310 \ |
| 6660 | 60 260 \ |
| 6661 | 70 218 \ |
| 6662 | 80 185 \ |
| 6663 | 90 154 \ |
| 6664 | 100 129 \ |
| 6665 | 120 109 \ |
| 6666 | 150 82 \ |
| 6667 | 180 69 \ |
| 6668 | 220 58 \ |
| 6669 | 240 50 \ |
| 6670 | 280 39.5 \ |
| 6671 | 320 29.5 \ |
| 6672 | 360 23 \ |
| 6673 | 400 18.25 \ |
| 6674 | 500 13.9 \ |
| 6675 | 600 10.55 \ |
| 6676 | 800 11.5 \ |
| 6677 | 1000 9.5 \ |
| 6678 | 2000 7.2 \ |
| 6679 | 2500 5.5 \ |
| 6680 | 3000 4 \ |
| 6681 | 4000 3 \ |
| 6682 | 6000 2 \ |
| 6683 | 8000 1.2 |
| 6684 | |
| 6685 | grit_ansicoated() ansicoated |
| 6686 | |
| 6687 | |
| 6688 | # |
| 6689 | # Is this correct? This is the JIS Japanese standard used on waterstones |
| 6690 | # |
| 6691 | jisgrit[micron] \ |
| 6692 | 150 75 \ |
| 6693 | 180 63 \ |
| 6694 | 220 53 \ |
| 6695 | 280 48 \ |
| 6696 | 320 40 \ |
| 6697 | 360 35 \ |
| 6698 | 400 30 \ |
| 6699 | 600 20 \ |
| 6700 | 700 17 \ |
| 6701 | 800 14 \ |
| 6702 | 1000 11.5 \ |
| 6703 | 1200 9.5 \ |
| 6704 | 1500 8 \ |
| 6705 | 2000 6.7 \ |
| 6706 | 2500 5.5 \ |
| 6707 | 3000 4 \ |
| 6708 | 4000 3 \ |
| 6709 | 6000 2 \ |
| 6710 | 8000 1.2 |
| 6711 | |
| 6712 | # The "Finishing Scale" marked with an A (e.g. A75). This information |
| 6713 | # is from the web page of the sand paper manufacturer Klingspor |
| 6714 | # https://www.klingspor.com/ctemplate1.aspx?page=default/html/gritGradingSystems_en-US.html |
| 6715 | # |
| 6716 | # I have no information about what this scale is used for. |
| 6717 | |
| 6718 | grit_A[micron]\ |
| 6719 | 16 15.3 \ |
| 6720 | 25 21.8 \ |
| 6721 | 30 23.6 \ |
| 6722 | 35 25.75 \ |
| 6723 | 45 35 \ |
| 6724 | 60 46.2 \ |
| 6725 | 65 53.5 \ |
| 6726 | 75 58.5 \ |
| 6727 | 90 65 \ |
| 6728 | 110 78 \ |
| 6729 | 130 93 \ |
| 6730 | 160 127 \ |
| 6731 | 200 156 |
| 6732 | # |
| 6733 | # Grits for DMT brand diamond sharpening stones from |
| 6734 | # https://www.dmtsharp.com/resources/dmt-catalog-product-information.html |
| 6735 | # "DMT Diamond Grits" PDF download |
| 6736 | |
| 6737 | dmtxxcoarse 120 micron # 120 mesh |
| 6738 | dmtsilver dmtxxcoarse |
| 6739 | dmtxx dmtxxcoarse |
| 6740 | dmtxcoarse 60 micron # 220 mesh |
| 6741 | dmtx dmtxcoarse |
| 6742 | dmtblack dmtxcoarse |
| 6743 | dmtcoarse 45 micron # 325 mesh |
| 6744 | dmtc dmtcoarse |
| 6745 | dmtblue dmtcoarse |
| 6746 | dmtfine 25 micron # 600 mesh |
| 6747 | dmtred dmtfine |
| 6748 | dmtf dmtfine |
| 6749 | dmtefine 9 micron # 1200 mesh |
| 6750 | dmte dmtefine |
| 6751 | dmtgreen dmtefine |
| 6752 | dmtceramic 7 micron # 2200 mesh |
| 6753 | dmtcer dmtceramic |
| 6754 | dmtwhite dmtceramic |
| 6755 | dmteefine 3 micron # 8000 mesh |
| 6756 | dmttan dmteefine |
| 6757 | dmtee dmteefine |
| 6758 | |
| 6759 | # |
| 6760 | # The following values come from a page in the Norton Stones catalog, |
| 6761 | # available at their web page, http://www.nortonstones.com. |
| 6762 | # |
| 6763 | |
| 6764 | hardtranslucentarkansas 6 micron # Natural novaculite (silicon quartz) |
| 6765 | softarkansas 22 micron # stones |
| 6766 | |
| 6767 | extrafineindia 22 micron # India stones are Norton's manufactured |
| 6768 | fineindia 35 micron # aluminum oxide product |
| 6769 | mediumindia 53.5 micron |
| 6770 | coarseindia 97 micron |
| 6771 | |
| 6772 | finecrystolon 45 micron # Crystolon stones are Norton's |
| 6773 | mediumcrystalon 78 micron # manufactured silicon carbide product |
| 6774 | coarsecrystalon 127 micron |
| 6775 | |
| 6776 | # The following are not from the Norton catalog |
| 6777 | hardblackarkansas 6 micron |
| 6778 | hardwhitearkansas 11 micron |
| 6779 | washita 35 micron |
| 6780 | |
| 6781 | # |
| 6782 | # Mesh systems for measuring particle sizes by sifting through a wire |
| 6783 | # mesh or sieve |
| 6784 | # |
| 6785 | |
| 6786 | # The Tyler system and US Sieve system are based on four steps for |
| 6787 | # each factor of 2 change in the size, so each size is 2^1|4 different |
| 6788 | # from the adjacent sizes. Unfortunately, the mesh numbers are |
| 6789 | # arbitrary, so the sizes cannot be expressed with a functional form. |
| 6790 | # Various references round the values differently. The mesh numbers |
| 6791 | # are supposed to correspond to the number of holes per inch, but this |
| 6792 | # correspondence is only approximate because it doesn't include the |
| 6793 | # wire size of the mesh. |
| 6794 | |
| 6795 | # The Tyler Mesh system was apparently introduced by the WS Tyler |
| 6796 | # company, but it appears that they no longer use it. They follow the |
| 6797 | # ASTM E11 standard. |
| 6798 | |
| 6799 | meshtyler[micron] \ |
| 6800 | 2.5 8000 \ |
| 6801 | 3 6727 \ |
| 6802 | 3.5 5657 \ |
| 6803 | 4 4757 \ |
| 6804 | 5 4000 \ |
| 6805 | 6 3364 \ |
| 6806 | 7 2828 \ |
| 6807 | 8 2378 \ |
| 6808 | 9 2000 \ |
| 6809 | 10 1682 \ |
| 6810 | 12 1414 \ |
| 6811 | 14 1189 \ |
| 6812 | 16 1000 \ |
| 6813 | 20 841 \ |
| 6814 | 24 707 \ |
| 6815 | 28 595 \ |
| 6816 | 32 500 \ |
| 6817 | 35 420 \ |
| 6818 | 42 354 \ |
| 6819 | 48 297 \ |
| 6820 | 60 250 \ |
| 6821 | 65 210 \ |
| 6822 | 80 177 \ |
| 6823 | 100 149 \ |
| 6824 | 115 125 \ |
| 6825 | 150 105 \ |
| 6826 | 170 88 \ |
| 6827 | 200 74 \ |
| 6828 | 250 63 \ |
| 6829 | 270 53 \ |
| 6830 | 325 44 \ |
| 6831 | 400 37 |
| 6832 | |
| 6833 | # US Sieve size, ASTM E11 |
| 6834 | # |
| 6835 | # The WS Tyler company prints the list from ASTM E11 in |
| 6836 | # A Calculator for ASTM E11 Standard Sieve Designations |
| 6837 | # https://blog.wstyler.com/particle-analysis/astm-e11-standard-designations |
| 6838 | |
| 6839 | sieve[micron] \ |
| 6840 | 3.5 5600 \ |
| 6841 | 4 4750 \ |
| 6842 | 5 4000 \ |
| 6843 | 6 3350 \ |
| 6844 | 7 2800 \ |
| 6845 | 8 2360 \ |
| 6846 | 10 2000 \ |
| 6847 | 12 1700 \ |
| 6848 | 14 1400 \ |
| 6849 | 16 1180 \ |
| 6850 | 18 1000 \ |
| 6851 | 20 850 \ |
| 6852 | 25 710 \ |
| 6853 | 30 600 \ |
| 6854 | 35 500 \ |
| 6855 | 40 425 \ |
| 6856 | 45 355 \ |
| 6857 | 50 300 \ |
| 6858 | 60 250 \ |
| 6859 | 70 212 \ |
| 6860 | 80 180 \ |
| 6861 | 100 150 \ |
| 6862 | 120 125 \ |
| 6863 | 140 106 \ |
| 6864 | 170 90 \ |
| 6865 | 200 75 \ |
| 6866 | 230 63 \ |
| 6867 | 270 53 \ |
| 6868 | 325 45 \ |
| 6869 | 400 38 \ |
| 6870 | 450 32 \ |
| 6871 | 500 25 \ |
| 6872 | 625 20 # These last two values are not in the standard series |
| 6873 | # but were included in the ASTM standard because they |
| 6874 | meshUS() sieve # were in common usage. |
| 6875 | |
| 6876 | # British Mesh size, BS 410: 1986 |
| 6877 | # This system appears to correspond to the Tyler and US system, but |
| 6878 | # with different mesh numbers. |
| 6879 | # |
| 6880 | # http://www.panadyne.com/technical/panadyne_international_sieve_chart.pdf |
| 6881 | # |
| 6882 | |
| 6883 | meshbritish[micron] \ |
| 6884 | 3 5657 \ |
| 6885 | 3.5 4757 \ |
| 6886 | 4 4000 \ |
| 6887 | 5 3364 \ |
| 6888 | 6 2828 \ |
| 6889 | 7 2378 \ |
| 6890 | 8 2000 \ |
| 6891 | 10 1682 \ |
| 6892 | 12 1414 \ |
| 6893 | 14 1189 \ |
| 6894 | 16 1000 \ |
| 6895 | 18 841 \ |
| 6896 | 22 707 \ |
| 6897 | 25 595 \ |
| 6898 | 30 500 \ |
| 6899 | 36 420 \ |
| 6900 | 44 354 \ |
| 6901 | 52 297 \ |
| 6902 | 60 250 \ |
| 6903 | 72 210 \ |
| 6904 | 85 177 \ |
| 6905 | 100 149 \ |
| 6906 | 120 125 \ |
| 6907 | 150 105 \ |
| 6908 | 170 88 \ |
| 6909 | 200 74 \ |
| 6910 | 240 63 \ |
| 6911 | 300 53 \ |
| 6912 | 350 44 \ |
| 6913 | 400 37 |
| 6914 | |
| 6915 | # French system, AFNOR NFX11-501: 1970 |
| 6916 | # The system appears to be based on size doubling every 3 mesh |
| 6917 | # numbers, though the values have been aggressively rounded. |
| 6918 | # It's not clear if the unrounded values would be considered |
| 6919 | # incorrect, so this is given as a table rather than a function. |
| 6920 | # Functional form: |
| 6921 | # meshtamis(mesh) units=[1;m] 5000 2^(1|3 (mesh-38)) micron |
| 6922 | # |
| 6923 | # http://www.panadyne.com/technical/panadyne_international_sieve_chart.pdf |
| 6924 | |
| 6925 | meshtamis[micron] \ |
| 6926 | 17 40 \ |
| 6927 | 18 50 \ |
| 6928 | 19 63 \ |
| 6929 | 20 80 \ |
| 6930 | 21 100 \ |
| 6931 | 22 125 \ |
| 6932 | 23 160 \ |
| 6933 | 24 200 \ |
| 6934 | 25 250 \ |
| 6935 | 26 315 \ |
| 6936 | 27 400 \ |
| 6937 | 28 500 \ |
| 6938 | 29 630 \ |
| 6939 | 30 800 \ |
| 6940 | 31 1000 \ |
| 6941 | 32 1250 \ |
| 6942 | 33 1600 \ |
| 6943 | 34 2000 \ |
| 6944 | 35 2500 \ |
| 6945 | 36 3150 \ |
| 6946 | 37 4000 \ |
| 6947 | 38 5000 |
| 6948 | |
| 6949 | # |
| 6950 | # Ring size. All ring sizes are given as the circumference of the ring. |
| 6951 | # |
| 6952 | |
| 6953 | # USA ring sizes. Several slightly different definitions seem to be in |
| 6954 | # circulation. According to [15], the interior diameter of size n ring in |
| 6955 | # inches is 0.32 n + 0.458 for n ranging from 3 to 13.5 by steps of 0.5. The |
| 6956 | # size 2 ring is inconsistently 0.538in and no 2.5 size is listed. |
| 6957 | # |
| 6958 | # However, other sources list 0.455 + 0.0326 n and 0.4525 + 0.0324 n as the |
| 6959 | # diameter and list no special case for size 2. (Or alternatively they are |
| 6960 | # 1.43 + .102 n and 1.4216+.1018 n for measuring circumference in inches.) One |
| 6961 | # reference claimed that the original system was that each size was 1|10 inch |
| 6962 | # circumference, but that source doesn't have an explanation for the modern |
| 6963 | # system which is somewhat different. |
| 6964 | |
| 6965 | ringsize(n) units=[1;in] domain=[2,) range=[1.6252,) \ |
| 6966 | (1.4216+.1018 n) in ; (ringsize/in + (-1.4216))/.1018 |
| 6967 | |
| 6968 | # Old practice in the UK measured rings using the "Wheatsheaf gauge" with sizes |
| 6969 | # specified alphabetically and based on the ring inside diameter in steps of |
| 6970 | # 1|64 inch. This system was replaced in 1987 by British Standard 6820 which |
| 6971 | # specifies sizes based on circumference. Each size is 1.25 mm different from |
| 6972 | # the preceding size. The baseline is size C which is 40 mm circumference. |
| 6973 | # The new sizes are close to the old ones. Sometimes it's necessary to go |
| 6974 | # beyond size Z to Z+1, Z+2, etc. |
| 6975 | |
| 6976 | sizeAring 37.50 mm |
| 6977 | sizeBring 38.75 mm |
| 6978 | sizeCring 40.00 mm |
| 6979 | sizeDring 41.25 mm |
| 6980 | sizeEring 42.50 mm |
| 6981 | sizeFring 43.75 mm |
| 6982 | sizeGring 45.00 mm |
| 6983 | sizeHring 46.25 mm |
| 6984 | sizeIring 47.50 mm |
| 6985 | sizeJring 48.75 mm |
| 6986 | sizeKring 50.00 mm |
| 6987 | sizeLring 51.25 mm |
| 6988 | sizeMring 52.50 mm |
| 6989 | sizeNring 53.75 mm |
| 6990 | sizeOring 55.00 mm |
| 6991 | sizePring 56.25 mm |
| 6992 | sizeQring 57.50 mm |
| 6993 | sizeRring 58.75 mm |
| 6994 | sizeSring 60.00 mm |
| 6995 | sizeTring 61.25 mm |
| 6996 | sizeUring 62.50 mm |
| 6997 | sizeVring 63.75 mm |
| 6998 | sizeWring 65.00 mm |
| 6999 | sizeXring 66.25 mm |
| 7000 | sizeYring 67.50 mm |
| 7001 | sizeZring 68.75 mm |
| 7002 | |
| 7003 | # Japanese sizes start with size 1 at a 13mm inside diameter and each size is |
| 7004 | # 1|3 mm larger in diameter than the previous one. They are multiplied by pi |
| 7005 | # to give circumference. |
| 7006 | |
| 7007 | jpringsize(n) units=[1;mm] domain=[1,) range=[0.040840704,) \ |
| 7008 | (38|3 + n/3) pi mm ; 3 jpringsize/ pi mm + (-38) |
| 7009 | |
| 7010 | # The European ring sizes are the length of the circumference in mm minus 40. |
| 7011 | |
| 7012 | euringsize(n) units=[1;mm] (n+40) mm ; euringsize/mm + (-40) |
| 7013 | |
| 7014 | # |
| 7015 | # Abbreviations |
| 7016 | # |
| 7017 | |
| 7018 | mph mile/hr |
| 7019 | brmpg mile/brgallon |
| 7020 | usmpg mile/usgallon |
| 7021 | mpg mile/gal |
| 7022 | kph km/hr |
| 7023 | fL footlambert |
| 7024 | fpm ft/min |
| 7025 | fps ft/s |
| 7026 | rpm rev/min |
| 7027 | rps rev/sec |
| 7028 | mi mile |
| 7029 | smi mile |
| 7030 | nmi nauticalmile |
| 7031 | mbh 1e3 btu/hour |
| 7032 | mcm 1e3 circularmil |
| 7033 | ipy inch/year # used for corrosion rates |
| 7034 | ccf 100 ft^3 # used for selling water [18] |
| 7035 | Mcf 1000 ft^3 # not million cubic feet [18] |
| 7036 | kp kilopond |
| 7037 | kpm kp meter |
| 7038 | Wh W hour |
| 7039 | hph hp hour |
| 7040 | plf lb / foot # pounds per linear foot |
| 7041 | |
| 7042 | # |
| 7043 | # Compatibility units with Unix version |
| 7044 | # |
| 7045 | |
| 7046 | pa Pa |
| 7047 | ev eV |
| 7048 | hg Hg |
| 7049 | oe Oe |
| 7050 | mh mH |
| 7051 | rd rod |
| 7052 | pf pF |
| 7053 | gr grain |
| 7054 | nt N |
| 7055 | hz Hz |
| 7056 | hd hogshead |
| 7057 | dry drygallon/gallon |
| 7058 | nmile nauticalmile |
| 7059 | beV GeV |
| 7060 | bev beV |
| 7061 | coul C |
| 7062 | |
| 7063 | # |
| 7064 | # Radioactivity units |
| 7065 | # |
| 7066 | event !dimensionless |
| 7067 | becquerel event /s # Activity of radioactive source |
| 7068 | Bq becquerel # |
| 7069 | curie 3.7e10 Bq # Defined in 1910 as the radioactivity |
| 7070 | Ci curie # emitted by the amount of radon that is |
| 7071 | # in equilibrium with 1 gram of radium. |
| 7072 | rutherford 1e6 Bq # |
| 7073 | |
| 7074 | RADIATION_DOSE gray |
| 7075 | gray J/kg # Absorbed dose of radiation |
| 7076 | Gy gray # |
| 7077 | rad 1e-2 Gy # From Radiation Absorbed Dose |
| 7078 | rep 8.38 mGy # Roentgen Equivalent Physical, the amount |
| 7079 | # of radiation which , absorbed in the |
| 7080 | # body, would liberate the same amount |
| 7081 | # of energy as 1 roentgen of X rays |
| 7082 | # would, or 97 ergs. |
| 7083 | |
| 7084 | sievert J/kg # Dose equivalent: dosage that has the |
| 7085 | Sv sievert # same effect on human tissues as 200 |
| 7086 | rem 1e-2 Sv # keV X-rays. Different types of |
| 7087 | # radiation are weighted by the |
| 7088 | # Relative Biological Effectiveness |
| 7089 | # (RBE). |
| 7090 | # |
| 7091 | # Radiation type RBE |
| 7092 | # X-ray, gamma ray 1 |
| 7093 | # beta rays, > 1 MeV 1 |
| 7094 | # beta rays, < 1 MeV 1.08 |
| 7095 | # neutrons, < 1 MeV 4-5 |
| 7096 | # neutrons, 1-10 MeV 10 |
| 7097 | # protons, 1 MeV 8.5 |
| 7098 | # protons, .1 MeV 10 |
| 7099 | # alpha, 5 MeV 15 |
| 7100 | # alpha, 1 MeV 20 |
| 7101 | # |
| 7102 | # The energies are the kinetic energy |
| 7103 | # of the particles. Slower particles |
| 7104 | # interact more, so they are more |
| 7105 | # effective ionizers, and hence have |
| 7106 | # higher RBE values. |
| 7107 | # |
| 7108 | # rem stands for Roentgen Equivalent |
| 7109 | # Mammal |
| 7110 | banana_dose 0.1e-6 sievert # Informal measure of the dose due to |
| 7111 | # eating one average sized banana |
| 7112 | roentgen 2.58e-4 C / kg # Ionizing radiation that produces |
| 7113 | # 1 statcoulomb of charge in 1 cc of |
| 7114 | # dry air at stp. |
| 7115 | rontgen roentgen # Sometimes it appears spelled this way |
| 7116 | sievertunit 8.38 rontgen # Unit of gamma ray dose delivered in one |
| 7117 | # hour at a distance of 1 cm from a |
| 7118 | # point source of 1 mg of radium |
| 7119 | # enclosed in platinum .5 mm thick. |
| 7120 | |
| 7121 | eman 1e-7 Ci/m^3 # radioactive concentration |
| 7122 | mache 3.7e-7 Ci/m^3 |
| 7123 | |
| 7124 | # |
| 7125 | # Atomic weights. The atomic weight of an element is the ratio of the mass of |
| 7126 | # a mole of the element to 1|12 of a mole of Carbon 12. For each element, we |
| 7127 | # list the atomic weights of all of the isotopes. The Standard Atomic Weights |
| 7128 | # apply to the elements in the isotopic composition that occurs naturally on |
| 7129 | # Earth. These are computed values based on the isotopic distribution, and |
| 7130 | # may vary for specific samples. Elements which do not occur naturally do |
| 7131 | # not have Standard Atomic Weights. For these elements, if data on the most |
| 7132 | # stable isotope is available, is given. Otherwise, the user must specify the |
| 7133 | # desired isotope. |
| 7134 | |
| 7135 | !include elements.units |
| 7136 | |
| 7137 | # Density of the elements |
| 7138 | # |
| 7139 | # Note some elements occur in multiple forms (allotropes) with different |
| 7140 | # densities, and they are accordingly listed multiple times. |
| 7141 | |
| 7142 | # Density of gas phase elements at STP |
| 7143 | |
| 7144 | hydrogendensity 0.08988 g/l |
| 7145 | heliumdensity 0.1786 g/l |
| 7146 | neondensity 0.9002 g/l |
| 7147 | nitrogendensity 1.2506 g/l |
| 7148 | oxygendensity 1.429 g/l |
| 7149 | fluorinedensity 1.696 g/l |
| 7150 | argondensity 1.784 g/l |
| 7151 | chlorinedensity 3.2 g/l |
| 7152 | kryptondensity 3.749 g/l |
| 7153 | xenondensity 5.894 g/l |
| 7154 | radondensity 9.73 g/l |
| 7155 | |
| 7156 | # Density of liquid phase elements near room temperature |
| 7157 | |
| 7158 | brominedensity 3.1028 g/cm^3 |
| 7159 | mercurydensity 13.534 g/cm^3 |
| 7160 | |
| 7161 | # Density of solid elements near room temperature |
| 7162 | |
| 7163 | lithiumdensity 0.534 g/cm^3 |
| 7164 | potassiumdensity 0.862 g/cm^3 |
| 7165 | sodiumdensity 0.968 g/cm^3 |
| 7166 | rubidiumdensity 1.532 g/cm^3 |
| 7167 | calciumdensity 1.55 g/cm^3 |
| 7168 | magnesiumdensity 1.738 g/cm^3 |
| 7169 | phosphorus_white_density 1.823 g/cm^3 |
| 7170 | berylliumdensity 1.85 g/cm^3 |
| 7171 | sulfur_gamma_density 1.92 g/cm^3 |
| 7172 | cesiumdensity 1.93 g/cm^3 |
| 7173 | carbon_amorphous_density 1.95 g/cm^3 # average value |
| 7174 | sulfur_betadensity 1.96 g/cm^3 |
| 7175 | sulfur_alpha_density 2.07 g/cm^3 |
| 7176 | carbon_graphite_density 2.267 g/cm^3 |
| 7177 | phosphorus_red_density 2.27 g/cm^3 # average value |
| 7178 | silicondensity 2.3290 g/cm^3 |
| 7179 | phosphorus_violet_density 2.36 g/cm^3 |
| 7180 | borondensity 2.37 g/cm^3 |
| 7181 | strontiumdensity 2.64 g/cm^3 |
| 7182 | phosphorus_black_density 2.69 g/cm^3 |
| 7183 | aluminumdensity 2.7 g/cm^3 |
| 7184 | bariumdensity 3.51 g/cm^3 |
| 7185 | carbon_diamond_density 3.515 g/cm^3 |
| 7186 | scandiumdensity 3.985 g/cm^3 |
| 7187 | selenium_vitreous_density 4.28 g/cm^3 |
| 7188 | selenium_alpha_density 4.39 g/cm^3 |
| 7189 | titaniumdensity 4.406 g/cm^3 |
| 7190 | yttriumdensity 4.472 g/cm^3 |
| 7191 | selenium_gray_density 4.81 g/cm^3 |
| 7192 | iodinedensity 4.933 g/cm^3 |
| 7193 | europiumdensity 5.264 g/cm^3 |
| 7194 | germaniumdensity 5.323 g/cm^3 |
| 7195 | radiumdensity 5.5 g/cm^3 |
| 7196 | arsenicdensity 5.727 g/cm^3 |
| 7197 | tin_alpha_density 5.769 g/cm^3 |
| 7198 | galliumdensity 5.91 g/cm^3 |
| 7199 | vanadiumdensity 6.11 g/cm^3 |
| 7200 | lanthanumdensity 6.162 g/cm^3 |
| 7201 | telluriumdensity 6.24 g/cm^3 |
| 7202 | zirconiumdensity 6.52 g/cm^3 |
| 7203 | antimonydensity 6.697 g/cm^3 |
| 7204 | ceriumdensity 6.77 g/cm^3 |
| 7205 | praseodymiumdensity 6.77 g/cm^3 |
| 7206 | ytterbiumdensity 6.9 g/cm^3 |
| 7207 | neodymiumdensity 7.01 g/cm^3 |
| 7208 | zincdensity 7.14 g/cm^3 |
| 7209 | chromiumdensity 7.19 g/cm^3 |
| 7210 | manganesedensity 7.21 g/cm^3 |
| 7211 | promethiumdensity 7.26 g/cm^3 |
| 7212 | tin_beta_density 7.265 g/cm^3 |
| 7213 | indiumdensity 7.31 g/cm^3 |
| 7214 | samariumdensity 7.52 g/cm^3 |
| 7215 | irondensity 7.874 g/cm^3 |
| 7216 | gadoliniumdensity 7.9 g/cm^3 |
| 7217 | terbiumdensity 8.23 g/cm^3 |
| 7218 | dysprosiumdensity 8.54 g/cm^3 |
| 7219 | niobiumdensity 8.57 g/cm^3 |
| 7220 | cadmiumdensity 8.65 g/cm^3 |
| 7221 | holmiumdensity 8.79 g/cm^3 |
| 7222 | cobaltdensity 8.9 g/cm^3 |
| 7223 | nickeldensity 8.908 g/cm^3 |
| 7224 | erbiumdensity 9.066 g/cm^3 |
| 7225 | polonium_alpha_density 9.196 g/cm^3 |
| 7226 | thuliumdensity 9.32 g/cm^3 |
| 7227 | polonium_beta_density 9.398 g/cm^3 |
| 7228 | bismuthdensity 9.78 g/cm^3 |
| 7229 | lutetiumdensity 9.841 g/cm^3 |
| 7230 | actiniumdensity 10 g/cm^3 |
| 7231 | molybdenumdensity 10.28 g/cm^3 |
| 7232 | silverdensity 10.49 g/cm^3 |
| 7233 | technetiumdensity 11 g/cm^3 |
| 7234 | leaddensity 11.34 g/cm^3 |
| 7235 | thoriumdensity 11.7 g/cm^3 |
| 7236 | thalliumdensity 11.85 g/cm^3 |
| 7237 | americiumdensity 12 g/cm^3 |
| 7238 | palladiumdensity 12.023 g/cm^3 |
| 7239 | rhodiumdensity 12.41 g/cm^3 |
| 7240 | rutheniumdensity 12.45 g/cm^3 |
| 7241 | berkelium_beta_density 13.25 g/cm^3 |
| 7242 | hafniumdensity 13.31 g/cm^3 |
| 7243 | curiumdensity 13.51 g/cm^3 |
| 7244 | berkelium_alphadensity 14.78 g/cm^3 |
| 7245 | californiumdensity 15.1 g/cm^3 |
| 7246 | protactiniumdensity 15.37 g/cm^3 |
| 7247 | tantalumdensity 16.69 g/cm^3 |
| 7248 | uraniumdensity 19.1 g/cm^3 |
| 7249 | tungstendensity 19.3 g/cm^3 |
| 7250 | golddensity 19.30 g/cm^3 |
| 7251 | plutoniumdensity 19.816 g/cm^3 |
| 7252 | neptuniumdensity 20.45 g/cm^3 # alpha form, only one at room temp |
| 7253 | rheniumdensity 21.02 g/cm^3 |
| 7254 | platinumdensity 21.45 g/cm^3 |
| 7255 | iridiumdensity 22.56 g/cm^3 |
| 7256 | osmiumdensity 22.59 g/cm^3 |
| 7257 | |
| 7258 | # A few alternate names |
| 7259 | |
| 7260 | tin_gray tin_alpha_density |
| 7261 | tin_white tin_beta_density |
| 7262 | graphitedensity carbon_graphite_density |
| 7263 | diamonddensity carbon_diamond_density |
| 7264 | |
| 7265 | # Predicted density of elements that have not been made in sufficient |
| 7266 | # quantities for measurement. |
| 7267 | |
| 7268 | franciumdensity 2.48 g/cm^3 # liquid, predicted melting point 8 degC |
| 7269 | astatinedensity 6.35 g/cm^3 |
| 7270 | einsteiniumdensity 8.84 g/cm^3 |
| 7271 | fermiumdensity 9.7 g/cm^3 |
| 7272 | nobeliumdensity 9.9 g/cm^3 |
| 7273 | mendeleviumdensity 10.3 g/cm^3 |
| 7274 | lawrenciumdensity 16 g/cm^3 |
| 7275 | rutherfordiumdensity 23.2 g/cm^3 |
| 7276 | roentgeniumdensity 28.7 g/cm^3 |
| 7277 | dubniumdensity 29.3 g/cm^3 |
| 7278 | darmstadtiumdensity 34.8 g/cm^3 |
| 7279 | seaborgiumdensity 35 g/cm^3 |
| 7280 | bohriumdensity 37.1 g/cm^3 |
| 7281 | meitneriumdensity 37.4 g/cm^3 |
| 7282 | hassiumdensity 41 g/cm^3 |
| 7283 | |
| 7284 | # |
| 7285 | # population units |
| 7286 | # |
| 7287 | |
| 7288 | people 1 |
| 7289 | person people |
| 7290 | death people |
| 7291 | capita people |
| 7292 | percapita per capita |
| 7293 | |
| 7294 | # TGM dozen based unit system listed on the "dozenal" forum |
| 7295 | # http://www.dozenalsociety.org.uk/apps/tgm.htm. These units are |
| 7296 | # proposed as an allegedly more rational alternative to the SI system. |
| 7297 | |
| 7298 | Tim 12^-4 hour # Time |
| 7299 | Grafut gravity Tim^2 # Length based on gravity |
| 7300 | Surf Grafut^2 # area |
| 7301 | Volm Grafut^3 # volume |
| 7302 | Vlos Grafut/Tim # speed |
| 7303 | Denz Maz/Volm # density |
| 7304 | Mag Maz gravity # force |
| 7305 | Maz Volm kg / oldliter # mass based on water |
| 7306 | |
| 7307 | # Abbreviations |
| 7308 | |
| 7309 | # Tm Tim # Conflicts with Tm = Terameter |
| 7310 | Gf Grafut |
| 7311 | Sf Surf |
| 7312 | Vm Volm |
| 7313 | Vl Vlos |
| 7314 | Mz Maz |
| 7315 | Dz Denz |
| 7316 | |
| 7317 | # Dozen based unit prefixes |
| 7318 | |
| 7319 | Zena- 12 |
| 7320 | Duna- 12^2 |
| 7321 | Trina- 12^3 |
| 7322 | Quedra- 12^4 |
| 7323 | Quena- 12^5 |
| 7324 | Hesa- 12^6 |
| 7325 | Seva- 12^7 |
| 7326 | Aka- 12^8 |
| 7327 | Neena- 12^9 |
| 7328 | Dexa- 12^10 |
| 7329 | Lefa- 12^11 |
| 7330 | Zennila- 12^12 |
| 7331 | |
| 7332 | Zeni- 12^-1 |
| 7333 | Duni- 12^-2 |
| 7334 | Trini- 12^-3 |
| 7335 | Quedri- 12^-4 |
| 7336 | Queni- 12^-5 |
| 7337 | Hesi- 12^-6 |
| 7338 | Sevi- 12^-7 |
| 7339 | Aki- 12^-8 |
| 7340 | Neeni- 12^-9 |
| 7341 | Dexi- 12^-10 |
| 7342 | Lefi- 12^-11 |
| 7343 | Zennili- 12^-12 |
| 7344 | |
| 7345 | # |
| 7346 | # Traditional Japanese units (shakkanhou) |
| 7347 | # |
| 7348 | # The traditional system of weights and measures is called shakkanhou from the |
| 7349 | # shaku and the ken. Japan accepted SI units in 1891 and legalized conversions |
| 7350 | # to the traditional system. In 1909 the inch-pound system was also legalized, |
| 7351 | # so Japan had three legally approved systems. A change to the metric system |
| 7352 | # started in 1921 but there was a lot of resistance. The Measurement Law of |
| 7353 | # October 1999 prohibits sales in anything but SI units. However, the old |
| 7354 | # units still live on in construction and as the basis for paper sizes of books |
| 7355 | # and tools used for handicrafts. |
| 7356 | # |
| 7357 | # Note that units below use the Hepburn romanization system. Some other |
| 7358 | # systems would render "mou", "jou", and "chou" as "mo", "jo" and "cho". |
| 7359 | # |
| 7360 | # |
| 7361 | # http://hiramatu-hifuka.com/onyak/onyindx.html |
| 7362 | |
| 7363 | # Japanese Proportions. These are still in everyday use. They also |
| 7364 | # get used as units to represent the proportion of the standard unit. |
| 7365 | |
| 7366 | wari_proportion 1|10 |
| 7367 | wari wari_proportion |
| 7368 | bu_proportion 1|100 # The character bu can also be read fun or bun |
| 7369 | # but usually "bu" is used for units. |
| 7370 | rin_proportion 1|1000 |
| 7371 | mou_proportion 1|10000 |
| 7372 | |
| 7373 | |
| 7374 | # Japanese Length Measures |
| 7375 | # |
| 7376 | # The length system is called kanejaku or |
| 7377 | # square and originated in China. It was |
| 7378 | # adopted as Japan's official measure in 701 |
| 7379 | # by the Taiho Code. This system is still in |
| 7380 | # common use in architecture and clothing. |
| 7381 | |
| 7382 | shaku 1|3.3 m |
| 7383 | mou 1|10000 shaku |
| 7384 | rin 1|1000 shaku |
| 7385 | bu_distance 1|100 shaku |
| 7386 | sun 1|10 shaku |
| 7387 | jou_distance 10 shaku |
| 7388 | jou jou_distance |
| 7389 | |
| 7390 | kanejakusun sun # Alias to emphasize architectural name |
| 7391 | kanejaku shaku |
| 7392 | kanejakujou jou |
| 7393 | |
| 7394 | # http://en.wikipedia.org/wiki/Taiwanese_units_of_measurement |
| 7395 | taichi shaku # http://zh.wikipedia.org/wiki/台尺 |
| 7396 | taicun sun # http://zh.wikipedia.org/wiki/台制 |
| 7397 | !utf8 |
| 7398 | 台尺 taichi # via Hanyu Pinyin romanizations |
| 7399 | 台寸 taicun |
| 7400 | !endutf8 |
| 7401 | |
| 7402 | # In context of clothing, shaku is different from architecture |
| 7403 | |
| 7404 | kujirajaku 10|8 shaku |
| 7405 | kujirajakusun 1|10 kujirajaku |
| 7406 | kujirajakubu 1|100 kujirajaku |
| 7407 | kujirajakujou 10 kujirajaku |
| 7408 | tan_distance 3 kujirajakujou |
| 7409 | |
| 7410 | ken 6 shaku # Also sometimes 6.3, 6.5, or 6.6 |
| 7411 | # http://www.homarewood.co.jp/syakusun.htm |
| 7412 | |
| 7413 | # mostly unused |
| 7414 | chou_distance 60 ken |
| 7415 | chou chou_distance |
| 7416 | ri 36 chou |
| 7417 | |
| 7418 | # Japanese Area Measures |
| 7419 | |
| 7420 | # Tsubo is still used for land size, though the others are more |
| 7421 | # recognized by their homonyms in the other measurements. |
| 7422 | |
| 7423 | gou_area 1|10 tsubo |
| 7424 | tsubo 36 shaku^2 # Size of two tatami = ken^2 ?? |
| 7425 | se 30 tsubo |
| 7426 | tan_area 10 se |
| 7427 | chou_area 10 tan_area |
| 7428 | |
| 7429 | # http://en.wikipedia.org/wiki/Taiwanese_units_of_measurement |
| 7430 | ping tsubo # http://zh.wikipedia.org/wiki/坪 |
| 7431 | jia 2934 ping # http://zh.wikipedia.org/wiki/甲_(单位) |
| 7432 | fen 1|10 jia # http://zh.wikipedia.org/wiki/分 |
| 7433 | fen_area 1|10 jia # Protection against future collisions |
| 7434 | !utf8 |
| 7435 | 坪 ping # via Hanyu Pinyin romanizations |
| 7436 | 甲 jia |
| 7437 | 分 fen |
| 7438 | 分地 fen_area # Protection against future collisions |
| 7439 | !endutf8 |
| 7440 | |
| 7441 | # Japanese architecture is based on a "standard" size of tatami mat. |
| 7442 | # Room sizes today are given in number of tatami, and this number |
| 7443 | # determines the spacing between colums and hence sizes of sliding |
| 7444 | # doors and paper screens. However, every region has its own slightly |
| 7445 | # different tatami size. Edoma, used in and around Tokyo and |
| 7446 | # Hokkaido, is becoming a nationwide standard. Kyouma is used around |
| 7447 | # Kyoto, Osaka and Kyuushu, and Chuukyouma is used around Nagoya. |
| 7448 | # Note that the tatami all have the aspect ratio 2:1 so that the mats |
| 7449 | # can tile the room with some of them turned 90 degrees. |
| 7450 | # |
| 7451 | # http://www.moon2.net/tatami/infotatami/structure.html |
| 7452 | |
| 7453 | edoma (5.8*2.9) shaku^2 |
| 7454 | kyouma (6.3*3.15) shaku^2 |
| 7455 | chuukyouma (6*3) shaku^2 |
| 7456 | jou_area edoma |
| 7457 | tatami jou_area |
| 7458 | |
| 7459 | # Japanese Volume Measures |
| 7460 | |
| 7461 | # The "shou" is still used for such things as alcohol and seasonings. |
| 7462 | # Large quantities of paint are still purchased in terms of "to". |
| 7463 | |
| 7464 | shaku_volume 1|10 gou_volume |
| 7465 | gou_volume 1|10 shou |
| 7466 | gou gou_volume |
| 7467 | shou (4.9*4.9*2.7) sun^3 # The character shou which is |
| 7468 | # the same as masu refers to a |
| 7469 | # rectangular wooden cup used to |
| 7470 | # measure liquids and cereal. |
| 7471 | # Sake is sometimes served in a masu |
| 7472 | # Note that it happens to be |
| 7473 | # EXACTLY 7^4/11^3 liters. |
| 7474 | to 10 shou |
| 7475 | koku 10 to # No longer used; historically a measure of rice |
| 7476 | |
| 7477 | # Japanese Weight Measures |
| 7478 | # |
| 7479 | # https://web.archive.org/web/20040927115452/http://wyoming.hp.infoseek.co.jp/zatugaku/zamoney.html |
| 7480 | # https://en.wikipedia.org/wiki/Japanese_units_of_measurement |
| 7481 | |
| 7482 | # Not really used anymore. |
| 7483 | |
| 7484 | rin_weight 1|10 bu_weight |
| 7485 | bu_weight 1|10 monme |
| 7486 | fun 1|10 monme |
| 7487 | monme momme |
| 7488 | kin 160 monme |
| 7489 | kan 1000 monme |
| 7490 | kwan kan # This was the old pronunciation of the unit. |
| 7491 | # The old spelling persisted a few centuries |
| 7492 | # longer and was not changed until around |
| 7493 | # 1950. |
| 7494 | |
| 7495 | # http://en.wikipedia.org/wiki/Taiwanese_units_of_measurement |
| 7496 | # says: "Volume measure in Taiwan is largely metric". |
| 7497 | taijin kin # http://zh.wikipedia.org/wiki/台斤 |
| 7498 | tailiang 10 monme # http://zh.wikipedia.org/wiki/台斤 |
| 7499 | taiqian monme # http://zh.wikipedia.org/wiki/台制 |
| 7500 | !utf8 |
| 7501 | 台斤 taijin # via Hanyu Pinyin romanizations |
| 7502 | 台兩 tailiang |
| 7503 | 台錢 taiqian |
| 7504 | !endutf8 |
| 7505 | |
| 7506 | # |
| 7507 | # Australian unit |
| 7508 | # |
| 7509 | |
| 7510 | australiasquare (10 ft)^2 # Used for house area |
| 7511 | |
| 7512 | |
| 7513 | # |
| 7514 | # A few German units as currently in use. |
| 7515 | # |
| 7516 | |
| 7517 | zentner 50 kg |
| 7518 | doppelzentner 2 zentner |
| 7519 | pfund 500 g |
| 7520 | |
| 7521 | # The klafter, which was used in central Europe, was derived from the span of |
| 7522 | # outstretched arms. |
| 7523 | # |
| 7524 | # https://en.wikipedia.org/wiki/Obsolete_Austrian_units_of_measurement |
| 7525 | # https://www.llv.li/files/abi/klafter-m2-en.pdf |
| 7526 | |
| 7527 | austriaklafter 1.89648384 m # Exact definition, 23 July 1871 |
| 7528 | austriafoot 1|6 austriaklafter |
| 7529 | prussiaklafter 1.88 m |
| 7530 | prussiafoot 1|6 prussiaklafter |
| 7531 | bavariaklafter 1.751155 m |
| 7532 | bavariafoot 1|6 bavariaklafter |
| 7533 | hesseklafter 2.5 m |
| 7534 | hessefoot 1|6 hesseklafter |
| 7535 | switzerlandklafter metricklafter |
| 7536 | switzerlandfoot 1|6 switzerlandklafter |
| 7537 | swissklafter switzerlandklafter |
| 7538 | swissfoot 1|6 swissklafter |
| 7539 | metricklafter 1.8 m |
| 7540 | |
| 7541 | austriayoke 8 austriaklafter * 200 austriaklafter |
| 7542 | |
| 7543 | liechtensteinsquareklafter 3.596652 m^2 # Used until 2017 to measure land area |
| 7544 | liechtensteinklafter sqrt(liechtensteinsquareklafter) |
| 7545 | |
| 7546 | # The klafter was also used to measure volume of wood, generally being a stack |
| 7547 | # of wood one klafter wide, one klafter long, with logs 3 feet (half a klafter) |
| 7548 | # in length |
| 7549 | |
| 7550 | prussiawoodklafter 0.5 prussiaklafter^3 |
| 7551 | austriawoodklafter 0.5 austriaklafter^3 |
| 7552 | festmeter m^3 # modern measure of wood, solid cube |
| 7553 | raummeter 0.7 festmeter # Air space between the logs, stacked |
| 7554 | schuettraummeter 0.65 raummeter # A cubic meter volume of split and cut |
| 7555 | # firewood in a loose, unordered |
| 7556 | # pile, not stacked. This is called |
| 7557 | # "tipped". |
| 7558 | !utf8 |
| 7559 | schüttraummeter schuettraummeter |
| 7560 | !endutf8 |
| 7561 | |
| 7562 | |
| 7563 | # |
| 7564 | # Swedish (Sweden) pre-metric units of 1739. |
| 7565 | # The metric system was adopted in 1878. |
| 7566 | # https://sv.wikipedia.org/wiki/Verkm%C3%A5tt |
| 7567 | # |
| 7568 | |
| 7569 | verklinje 2.0618125 mm |
| 7570 | verktum 12 verklinje |
| 7571 | kvarter 6 verktum |
| 7572 | fot 2 kvarter |
| 7573 | aln 2 fot |
| 7574 | famn 3 aln |
| 7575 | |
| 7576 | # |
| 7577 | # Some traditional Russian measures |
| 7578 | # |
| 7579 | # If you would like to help expand this section and understand |
| 7580 | # cyrillic transliteration, let me know. These measures are meant to |
| 7581 | # reflect common usage, e.g. in translated literature. |
| 7582 | # |
| 7583 | |
| 7584 | dessiatine 2400 sazhen^2 # Land measure |
| 7585 | dessjatine dessiatine |
| 7586 | |
| 7587 | funt 409.51718 grams # similar to pound |
| 7588 | zolotnik 1|96 funt # used for precious metal measure |
| 7589 | pood 40 funt # common in agricultural measure |
| 7590 | |
| 7591 | arshin (2 + 1|3) feet |
| 7592 | sazhen 3 arshin # analogous to fathom |
| 7593 | verst 500 sazhen # of similar use to mile |
| 7594 | versta verst |
| 7595 | borderverst 1000 sazhen |
| 7596 | russianmile 7 verst |
| 7597 | |
| 7598 | |
| 7599 | |
| 7600 | |
| 7601 | # |
| 7602 | # Old French distance measures, from French Weights and Measures |
| 7603 | # Before the Revolution by Zupko |
| 7604 | # |
| 7605 | |
| 7606 | frenchfoot 144|443.296 m # pied de roi, the standard of Paris. |
| 7607 | pied frenchfoot # Half of the hashimicubit, |
| 7608 | frenchfeet frenchfoot # instituted by Charlemagne. |
| 7609 | frenchinch 1|12 frenchfoot # This exact definition comes from |
| 7610 | frenchthumb frenchinch # a law passed on 10 Dec 1799 which |
| 7611 | pouce frenchthumb # fixed the meter at |
| 7612 | # 3 frenchfeet + 11.296 lignes. |
| 7613 | frenchline 1|12 frenchinch # This is supposed to be the size |
| 7614 | ligne frenchline # of the average barleycorn |
| 7615 | frenchpoint 1|12 frenchline |
| 7616 | toise 6 frenchfeet |
| 7617 | arpent 180^2 pied^2 # The arpent is 100 square perches, |
| 7618 | # but the perche seems to vary a lot |
| 7619 | # and can be 18 feet, 20 feet, or 22 |
| 7620 | # feet. This measure was described |
| 7621 | # as being in common use in Canada in |
| 7622 | # 1934 (Websters 2nd). The value |
| 7623 | # given here is the Paris standard |
| 7624 | # arpent. |
| 7625 | frenchgrain 1|18827.15 kg # Weight of a wheat grain, hence |
| 7626 | # smaller than the British grain. |
| 7627 | frenchpound 9216 frenchgrain |
| 7628 | |
| 7629 | # |
| 7630 | # Before the Imperial Weights and Measures Act of 1824, various different |
| 7631 | # weights and measures were in use in different places. |
| 7632 | # |
| 7633 | |
| 7634 | # Scots linear measure |
| 7635 | |
| 7636 | scotsinch 1.00540054 UKinch |
| 7637 | scotslink 1|100 scotschain |
| 7638 | scotsfoot 12 scotsinch |
| 7639 | scotsfeet scotsfoot |
| 7640 | scotsell 37 scotsinch |
| 7641 | scotsfall 6 scotsell |
| 7642 | scotschain 4 scotsfall |
| 7643 | scotsfurlong 10 scotschain |
| 7644 | scotsmile 8 scotsfurlong |
| 7645 | |
| 7646 | # Scots area measure |
| 7647 | |
| 7648 | scotsrood 40 scotsfall^2 |
| 7649 | scotsacre 4 scotsrood |
| 7650 | |
| 7651 | # Irish linear measure |
| 7652 | |
| 7653 | irishinch UKinch |
| 7654 | irishpalm 3 irishinch |
| 7655 | irishspan 3 irishpalm |
| 7656 | irishfoot 12 irishinch |
| 7657 | irishfeet irishfoot |
| 7658 | irishcubit 18 irishinch |
| 7659 | irishyard 3 irishfeet |
| 7660 | irishpace 5 irishfeet |
| 7661 | irishfathom 6 irishfeet |
| 7662 | irishpole 7 irishyard # Only these values |
| 7663 | irishperch irishpole # are different from |
| 7664 | irishchain 4 irishperch # the British Imperial |
| 7665 | irishlink 1|100 irishchain # or English values for |
| 7666 | irishfurlong 10 irishchain # these lengths. |
| 7667 | irishmile 8 irishfurlong # |
| 7668 | |
| 7669 | # Irish area measure |
| 7670 | |
| 7671 | irishrood 40 irishpole^2 |
| 7672 | irishacre 4 irishrood |
| 7673 | |
| 7674 | # English wine capacity measures (Winchester measures) |
| 7675 | |
| 7676 | winepint 1|2 winequart |
| 7677 | winequart 1|4 winegallon |
| 7678 | winegallon 231 UKinch^3 # Sometimes called the Winchester Wine Gallon, |
| 7679 | # it was legalized in 1707 by Queen Anne, and |
| 7680 | # given the definition of 231 cubic inches. It |
| 7681 | # had been in use for a while as 8 pounds of wine |
| 7682 | # using a merchant's pound, but the definition of |
| 7683 | # the merchant's pound had become uncertain. A |
| 7684 | # pound of 15 tower ounces (6750 grains) had been |
| 7685 | # common, but then a pound of 15 troy ounces |
| 7686 | # (7200 grains) gained popularity. Because of |
| 7687 | # the switch in the value of the merchants pound, |
| 7688 | # the size of the wine gallon was uncertain in |
| 7689 | # the market, hence the official act in 1707. |
| 7690 | # The act allowed that a six inch tall cylinder |
| 7691 | # with a 7 inch diameter was a lawful wine |
| 7692 | # gallon. (This comes out to 230.9 in^3.) |
| 7693 | # Note also that in Britain a legal conversion |
| 7694 | # was established to the 1824 Imperial gallon |
| 7695 | # then taken as 277.274 in^3 so that the wine |
| 7696 | # gallon was 0.8331 imperial gallons. This is |
| 7697 | # 231.1 cubic inches (using the international |
| 7698 | # inch). |
| 7699 | winerundlet 18 winegallon |
| 7700 | winebarrel 31.5 winegallon |
| 7701 | winetierce 42 winegallon |
| 7702 | winehogshead 2 winebarrel |
| 7703 | winepuncheon 2 winetierce |
| 7704 | winebutt 2 winehogshead |
| 7705 | winepipe winebutt |
| 7706 | winetun 2 winebutt |
| 7707 | |
| 7708 | # English beer and ale measures used 1803-1824 and used for beer before 1688 |
| 7709 | |
| 7710 | beerpint 1|2 beerquart |
| 7711 | beerquart 1|4 beergallon |
| 7712 | beergallon 282 UKinch^3 |
| 7713 | beerbarrel 36 beergallon |
| 7714 | beerhogshead 1.5 beerbarrel |
| 7715 | |
| 7716 | # English ale measures used from 1688-1803 for both ale and beer |
| 7717 | |
| 7718 | alepint 1|2 alequart |
| 7719 | alequart 1|4 alegallon |
| 7720 | alegallon beergallon |
| 7721 | alebarrel 34 alegallon |
| 7722 | alehogshead 1.5 alebarrel |
| 7723 | |
| 7724 | # Scots capacity measure |
| 7725 | |
| 7726 | scotsgill 1|4 mutchkin |
| 7727 | mutchkin 1|2 choppin |
| 7728 | choppin 1|2 scotspint |
| 7729 | scotspint 1|2 scotsquart |
| 7730 | scotsquart 1|4 scotsgallon |
| 7731 | scotsgallon 827.232 UKinch^3 |
| 7732 | scotsbarrel 8 scotsgallon |
| 7733 | jug scotspint |
| 7734 | |
| 7735 | # Scots dry capacity measure |
| 7736 | |
| 7737 | scotswheatlippy 137.333 UKinch^3 # Also used for peas, beans, rye, salt |
| 7738 | scotswheatlippies scotswheatlippy |
| 7739 | scotswheatpeck 4 scotswheatlippy |
| 7740 | scotswheatfirlot 4 scotswheatpeck |
| 7741 | scotswheatboll 4 scotswheatfirlot |
| 7742 | scotswheatchalder 16 scotswheatboll |
| 7743 | |
| 7744 | scotsoatlippy 200.345 UKinch^3 # Also used for barley and malt |
| 7745 | scotsoatlippies scotsoatlippy |
| 7746 | scotsoatpeck 4 scotsoatlippy |
| 7747 | scotsoatfirlot 4 scotsoatpeck |
| 7748 | scotsoatboll 4 scotsoatfirlot |
| 7749 | scotsoatchalder 16 scotsoatboll |
| 7750 | |
| 7751 | # Scots Tron weight |
| 7752 | |
| 7753 | trondrop 1|16 tronounce |
| 7754 | tronounce 1|20 tronpound |
| 7755 | tronpound 9520 grain |
| 7756 | tronstone 16 tronpound |
| 7757 | |
| 7758 | # Irish liquid capacity measure |
| 7759 | |
| 7760 | irishnoggin 1|4 irishpint |
| 7761 | irishpint 1|2 irishquart |
| 7762 | irishquart 1|2 irishpottle |
| 7763 | irishpottle 1|2 irishgallon |
| 7764 | irishgallon 217.6 UKinch^3 |
| 7765 | irishrundlet 18 irishgallon |
| 7766 | irishbarrel 31.5 irishgallon |
| 7767 | irishtierce 42 irishgallon |
| 7768 | irishhogshead 2 irishbarrel |
| 7769 | irishpuncheon 2 irishtierce |
| 7770 | irishpipe 2 irishhogshead |
| 7771 | irishtun 2 irishpipe |
| 7772 | |
| 7773 | # Irish dry capacity measure |
| 7774 | |
| 7775 | irishpeck 2 irishgallon |
| 7776 | irishbushel 4 irishpeck |
| 7777 | irishstrike 2 irishbushel |
| 7778 | irishdrybarrel 2 irishstrike |
| 7779 | irishquarter 2 irishbarrel |
| 7780 | |
| 7781 | # English Tower weights, abolished in 1528 |
| 7782 | |
| 7783 | towerpound 5400 grain |
| 7784 | towerounce 1|12 towerpound |
| 7785 | towerpennyweight 1|20 towerounce |
| 7786 | towergrain 1|32 towerpennyweight |
| 7787 | |
| 7788 | # English Mercantile weights, used since the late 12th century |
| 7789 | |
| 7790 | mercpound 6750 grain |
| 7791 | mercounce 1|15 mercpound |
| 7792 | mercpennyweight 1|20 mercounce |
| 7793 | |
| 7794 | # English weights for lead |
| 7795 | |
| 7796 | leadstone 12.5 lb |
| 7797 | fotmal 70 lb |
| 7798 | leadwey 14 leadstone |
| 7799 | fothers 12 leadwey |
| 7800 | |
| 7801 | # English Hay measure |
| 7802 | |
| 7803 | newhaytruss 60 lb # New and old here seem to refer to "new" |
| 7804 | newhayload 36 newhaytruss # hay and "old" hay rather than a new unit |
| 7805 | oldhaytruss 56 lb # and an old unit. |
| 7806 | oldhayload 36 oldhaytruss |
| 7807 | |
| 7808 | # English wool measure |
| 7809 | |
| 7810 | woolclove 7 lb |
| 7811 | woolstone 2 woolclove |
| 7812 | wooltod 2 woolstone |
| 7813 | woolwey 13 woolstone |
| 7814 | woolsack 2 woolwey |
| 7815 | woolsarpler 2 woolsack |
| 7816 | woollast 6 woolsarpler |
| 7817 | |
| 7818 | # |
| 7819 | # Ancient history units: There tends to be uncertainty in the definitions |
| 7820 | # of the units in this section |
| 7821 | # These units are from [11] |
| 7822 | |
| 7823 | # Roman measure. The Romans had a well defined distance measure, but their |
| 7824 | # measures of weight were poor. They adopted local weights in different |
| 7825 | # regions without distinguishing among them so that there are half a dozen |
| 7826 | # different Roman "standard" weight systems. |
| 7827 | |
| 7828 | romanfoot 296 mm # There is some uncertainty in this definition |
| 7829 | romanfeet romanfoot # from which all the other units are derived. |
| 7830 | pes romanfoot # This value appears in numerous sources. In "The |
| 7831 | pedes romanfoot # Roman Land Surveyors", Dilke gives 295.7 mm. |
| 7832 | romaninch 1|12 romanfoot # The subdivisions of the Roman foot have the |
| 7833 | romandigit 1|16 romanfoot # same names as the subdivisions of the pound, |
| 7834 | romanpalm 1|4 romanfoot # but we can't have the names for different |
| 7835 | romancubit 18 romaninch # units. |
| 7836 | romanpace 5 romanfeet # Roman double pace (basic military unit) |
| 7837 | passus romanpace |
| 7838 | romanperch 10 romanfeet |
| 7839 | stade 125 romanpaces |
| 7840 | stadia stade |
| 7841 | stadium stade |
| 7842 | romanmile 8 stadia # 1000 paces |
| 7843 | romanleague 1.5 romanmile |
| 7844 | schoenus 4 romanmile |
| 7845 | |
| 7846 | # Other values for the Roman foot (from Dilke) |
| 7847 | |
| 7848 | earlyromanfoot 29.73 cm |
| 7849 | pesdrusianus 33.3 cm # or 33.35 cm, used in Gaul & Germany in 1st c BC |
| 7850 | lateromanfoot 29.42 cm |
| 7851 | |
| 7852 | # Roman areas |
| 7853 | |
| 7854 | actuslength 120 romanfeet # length of a Roman furrow |
| 7855 | actus 120*4 romanfeet^2 # area of the furrow |
| 7856 | squareactus 120^2 romanfeet^2 # actus quadratus |
| 7857 | acnua squareactus |
| 7858 | iugerum 2 squareactus |
| 7859 | iugera iugerum |
| 7860 | jugerum iugerum |
| 7861 | jugera iugerum |
| 7862 | heredium 2 iugera # heritable plot |
| 7863 | heredia heredium |
| 7864 | centuria 100 heredia |
| 7865 | centurium centuria |
| 7866 | |
| 7867 | # Roman volumes |
| 7868 | |
| 7869 | sextarius 35.4 in^3 # Basic unit of Roman volume. As always, |
| 7870 | sextarii sextarius # there is uncertainty. Six large Roman |
| 7871 | # measures survive with volumes ranging from |
| 7872 | # 34.4 in^3 to 39.55 in^3. Three of them |
| 7873 | # cluster around the size given here. |
| 7874 | # |
| 7875 | # But the values for this unit vary wildly |
| 7876 | # in other sources. One reference gives 0.547 |
| 7877 | # liters, but then says the amphora is a |
| 7878 | # cubic Roman foot. This gives a value for the |
| 7879 | # sextarius of 0.540 liters. And the |
| 7880 | # encyclopedia Britannica lists 0.53 liters for |
| 7881 | # this unit. Both [7] and [11], which were |
| 7882 | # written by scholars of weights and measures, |
| 7883 | # give the value of 35.4 cubic inches. |
| 7884 | cochlearia 1|48 sextarius |
| 7885 | cyathi 1|12 sextarius |
| 7886 | acetabula 1|8 sextarius |
| 7887 | quartaria 1|4 sextarius |
| 7888 | quartarius quartaria |
| 7889 | heminae 1|2 sextarius |
| 7890 | hemina heminae |
| 7891 | cheonix 1.5 sextarii |
| 7892 | |
| 7893 | # Dry volume measures (usually) |
| 7894 | |
| 7895 | semodius 8 sextarius |
| 7896 | semodii semodius |
| 7897 | modius 16 sextarius |
| 7898 | modii modius |
| 7899 | |
| 7900 | # Liquid volume measures (usually) |
| 7901 | |
| 7902 | congius 12 heminae |
| 7903 | congii congius |
| 7904 | amphora 8 congii |
| 7905 | amphorae amphora # Also a dry volume measure |
| 7906 | culleus 20 amphorae |
| 7907 | quadrantal amphora |
| 7908 | |
| 7909 | # Roman weights |
| 7910 | |
| 7911 | libra 5052 grain # The Roman pound varied significantly |
| 7912 | librae libra # from 4210 grains to 5232 grains. Most of |
| 7913 | romanpound libra # the standards were obtained from the weight |
| 7914 | uncia 1|12 libra # of particular coins. The one given here is |
| 7915 | unciae uncia # based on the Gold Aureus of Augustus which |
| 7916 | romanounce uncia # was in use from BC 27 to AD 296. |
| 7917 | deunx 11 uncia |
| 7918 | dextans 10 uncia |
| 7919 | dodrans 9 uncia |
| 7920 | bes 8 uncia |
| 7921 | seprunx 7 uncia |
| 7922 | semis 6 uncia |
| 7923 | quincunx 5 uncia |
| 7924 | triens 4 uncia |
| 7925 | quadrans 3 uncia |
| 7926 | sextans 2 uncia |
| 7927 | sescuncia 1.5 uncia |
| 7928 | semuncia 1|2 uncia |
| 7929 | siscilius 1|4 uncia |
| 7930 | sextula 1|6 uncia |
| 7931 | semisextula 1|12 uncia |
| 7932 | scriptulum 1|24 uncia |
| 7933 | scrupula scriptulum |
| 7934 | romanobol 1|2 scrupula |
| 7935 | |
| 7936 | romanaspound 4210 grain # Old pound based on bronze coinage, the |
| 7937 | # earliest money of Rome BC 338 to BC 268. |
| 7938 | |
| 7939 | # Egyptian length measure |
| 7940 | |
| 7941 | egyptianroyalcubit 20.63 in # plus or minus .2 in |
| 7942 | egyptianpalm 1|7 egyptianroyalcubit |
| 7943 | egyptiandigit 1|4 egyptianpalm |
| 7944 | egyptianshortcubit 6 egyptianpalm |
| 7945 | |
| 7946 | doubleremen 29.16 in # Length of the diagonal of a square with |
| 7947 | remendigit 1|40 doubleremen # side length of 1 royal egyptian cubit. |
| 7948 | # This is divided into 40 digits which are |
| 7949 | # not the same size as the digits based on |
| 7950 | # the royal cubit. |
| 7951 | |
| 7952 | # Greek length measures |
| 7953 | |
| 7954 | greekfoot 12.45 in # Listed as being derived from the |
| 7955 | greekfeet greekfoot # Egyptian Royal cubit in [11]. It is |
| 7956 | greekcubit 1.5 greekfoot # said to be 3|5 of a 20.75 in cubit. |
| 7957 | pous greekfoot |
| 7958 | podes greekfoot |
| 7959 | orguia 6 greekfoot |
| 7960 | greekfathom orguia |
| 7961 | stadion 100 orguia |
| 7962 | akaina 10 greekfeet |
| 7963 | plethron 10 akaina |
| 7964 | greekfinger 1|16 greekfoot |
| 7965 | homericcubit 20 greekfingers # Elbow to end of knuckles. |
| 7966 | shortgreekcubit 18 greekfingers # Elbow to start of fingers. |
| 7967 | |
| 7968 | ionicfoot 296 mm |
| 7969 | doricfoot 326 mm |
| 7970 | |
| 7971 | olympiccubit 25 remendigit # These olympic measures were not as |
| 7972 | olympicfoot 2|3 olympiccubit # common as the other greek measures. |
| 7973 | olympicfinger 1|16 olympicfoot # They were used in agriculture. |
| 7974 | olympicfeet olympicfoot |
| 7975 | olympicdakylos olympicfinger |
| 7976 | olympicpalm 1|4 olympicfoot |
| 7977 | olympicpalestra olympicpalm |
| 7978 | olympicspithame 3|4 foot |
| 7979 | olympicspan olympicspithame |
| 7980 | olympicbema 2.5 olympicfeet |
| 7981 | olympicpace olympicbema |
| 7982 | olympicorguia 6 olympicfeet |
| 7983 | olympicfathom olympicorguia |
| 7984 | olympiccord 60 olympicfeet |
| 7985 | olympicamma olympiccord |
| 7986 | olympicplethron 100 olympicfeet |
| 7987 | olympicstadion 600 olympicfeet |
| 7988 | |
| 7989 | # Greek capacity measure |
| 7990 | |
| 7991 | greekkotyle 270 ml # This approximate value is obtained |
| 7992 | xestes 2 greekkotyle # from two earthenware vessels that |
| 7993 | khous 12 greekkotyle # were reconstructed from fragments. |
| 7994 | metretes 12 khous # The kotyle is a day's corn ration |
| 7995 | choinix 4 greekkotyle # for one man. |
| 7996 | hekteos 8 choinix |
| 7997 | medimnos 6 hekteos |
| 7998 | |
| 7999 | # Greek weight. Two weight standards were used, an Aegina standard based |
| 8000 | # on the Beqa shekel and an Athens (attic) standard. |
| 8001 | |
| 8002 | aeginastater 192 grain # Varies up to 199 grain |
| 8003 | aeginadrachmae 1|2 aeginastater |
| 8004 | aeginaobol 1|6 aeginadrachmae |
| 8005 | aeginamina 50 aeginastaters |
| 8006 | aeginatalent 60 aeginamina # Supposedly the mass of a cubic foot |
| 8007 | # of water (whichever foot was in use) |
| 8008 | |
| 8009 | atticstater 135 grain # Varies 134-138 grain |
| 8010 | atticdrachmae 1|2 atticstater |
| 8011 | atticobol 1|6 atticdrachmae |
| 8012 | atticmina 50 atticstaters |
| 8013 | attictalent 60 atticmina # Supposedly the mass of a cubic foot |
| 8014 | # of water (whichever foot was in use) |
| 8015 | |
| 8016 | # "Northern" cubit and foot. This was used by the pre-Aryan civilization in |
| 8017 | # the Indus valley. It was used in Mesopotamia, Egypt, North Africa, China, |
| 8018 | # central and Western Europe until modern times when it was displaced by |
| 8019 | # the metric system. |
| 8020 | |
| 8021 | northerncubit 26.6 in # plus/minus .2 in |
| 8022 | northernfoot 1|2 northerncubit |
| 8023 | |
| 8024 | sumeriancubit 495 mm |
| 8025 | kus sumeriancubit |
| 8026 | sumerianfoot 2|3 sumeriancubit |
| 8027 | |
| 8028 | assyriancubit 21.6 in |
| 8029 | assyrianfoot 1|2 assyriancubit |
| 8030 | assyrianpalm 1|3 assyrianfoot |
| 8031 | assyriansusi 1|20 assyrianpalm |
| 8032 | susi assyriansusi |
| 8033 | persianroyalcubit 7 assyrianpalm |
| 8034 | |
| 8035 | |
| 8036 | # Arabic measures. The arabic standards were meticulously kept. Glass weights |
| 8037 | # accurate to .2 grains were made during AD 714-900. |
| 8038 | |
| 8039 | hashimicubit 25.56 in # Standard of linear measure used |
| 8040 | # in Persian dominions of the Arabic |
| 8041 | # empire 7-8th cent. Is equal to two |
| 8042 | # French feet. |
| 8043 | |
| 8044 | blackcubit 21.28 in |
| 8045 | arabicfeet 1|2 blackcubit |
| 8046 | arabicfoot arabicfeet |
| 8047 | arabicinch 1|12 arabicfoot |
| 8048 | arabicmile 4000 blackcubit |
| 8049 | |
| 8050 | silverdirhem 45 grain # The weights were derived from these two |
| 8051 | tradedirhem 48 grain # units with two identically named systems |
| 8052 | # used for silver and used for trade purposes |
| 8053 | |
| 8054 | silverkirat 1|16 silverdirhem |
| 8055 | silverwukiyeh 10 silverdirhem |
| 8056 | silverrotl 12 silverwukiyeh |
| 8057 | arabicsilverpound silverrotl |
| 8058 | |
| 8059 | tradekirat 1|16 tradedirhem |
| 8060 | tradewukiyeh 10 tradedirhem |
| 8061 | traderotl 12 tradewukiyeh |
| 8062 | arabictradepound traderotl |
| 8063 | |
| 8064 | # Miscellaneous ancient units |
| 8065 | |
| 8066 | parasang 3.5 mile # Persian unit of length usually thought |
| 8067 | # to be between 3 and 3.5 miles |
| 8068 | biblicalcubit 21.8 in |
| 8069 | hebrewcubit 17.58 in |
| 8070 | li 10|27.8 mile # Chinese unit of length |
| 8071 | # 100 li is considered a day's march |
| 8072 | liang 11|3 oz # Chinese weight unit |
| 8073 | |
| 8074 | |
| 8075 | # Medieval time units. According to the OED, these appear in Du Cange |
| 8076 | # by Papias. |
| 8077 | |
| 8078 | timepoint 1|5 hour # also given as 1|4 |
| 8079 | timeminute 1|10 hour |
| 8080 | timeostent 1|60 hour |
| 8081 | timeounce 1|8 timeostent |
| 8082 | timeatom 1|47 timeounce |
| 8083 | |
| 8084 | # Given in [15], these subdivisions of the grain were supposedly used |
| 8085 | # by jewelers. The mite may have been used but the blanc could not |
| 8086 | # have been accurately measured. |
| 8087 | |
| 8088 | mite 1|20 grain |
| 8089 | droit 1|24 mite |
| 8090 | periot 1|20 droit |
| 8091 | blanc 1|24 periot |
| 8092 | |
| 8093 | # |
| 8094 | # Localization |
| 8095 | # |
| 8096 | |
| 8097 | !var UNITS_ENGLISH US |
| 8098 | hundredweight ushundredweight |
| 8099 | ton uston |
| 8100 | scruple apscruple |
| 8101 | fluidounce usfluidounce |
| 8102 | gallon usgallon |
| 8103 | bushel usbushel |
| 8104 | quarter quarterweight |
| 8105 | cup uscup |
| 8106 | tablespoon ustablespoon |
| 8107 | teaspoon usteaspoon |
| 8108 | dollar US$ |
| 8109 | cent $ 0.01 |
| 8110 | penny cent |
| 8111 | minim minimvolume |
| 8112 | pony ponyvolume |
| 8113 | grand usgrand |
| 8114 | firkin usfirkin |
| 8115 | hogshead ushogshead |
| 8116 | cable uscable |
| 8117 | !endvar |
| 8118 | |
| 8119 | !var UNITS_ENGLISH GB |
| 8120 | hundredweight brhundredweight |
| 8121 | ton brton |
| 8122 | scruple brscruple |
| 8123 | fluidounce brfluidounce |
| 8124 | gallon brgallon |
| 8125 | bushel brbushel |
| 8126 | quarter brquarter |
| 8127 | chaldron brchaldron |
| 8128 | cup brcup |
| 8129 | teacup brteacup |
| 8130 | tablespoon brtablespoon |
| 8131 | teaspoon brteaspoon |
| 8132 | dollar US$ |
| 8133 | cent $ 0.01 |
| 8134 | penny brpenny |
| 8135 | minim minimnote |
| 8136 | pony brpony |
| 8137 | grand brgrand |
| 8138 | firkin brfirkin |
| 8139 | hogshead brhogshead |
| 8140 | cable brcable |
| 8141 | !endvar |
| 8142 | |
| 8143 | !varnot UNITS_ENGLISH GB US |
| 8144 | !message Unknown value for environment variable UNITS_ENGLISH. Should be GB or US. |
| 8145 | !endvar |
| 8146 | |
| 8147 | |
| 8148 | !utf8 |
| 8149 | ⅛- 1|8 |
| 8150 | ¼- 1|4 |
| 8151 | ⅜- 3|8 |
| 8152 | ½- 1|2 |
| 8153 | ⅝- 5|8 |
| 8154 | ¾- 3|4 |
| 8155 | ⅞- 7|8 |
| 8156 | ⅙- 1|6 |
| 8157 | ⅓- 1|3 |
| 8158 | ⅔- 2|3 |
| 8159 | ⅚- 5|6 |
| 8160 | ⅕- 1|5 |
| 8161 | ⅖- 2|5 |
| 8162 | ⅗- 3|5 |
| 8163 | ⅘- 4|5 |
| 8164 | # U+2150- 1|7 For some reason these characters are getting |
| 8165 | # U+2151- 1|9 flagged as invalid UTF8. |
| 8166 | # U+2152- 1|10 |
| 8167 | #⅐- 1|7 # fails under MacOS |
| 8168 | #⅑- 1|9 # fails under MacOS |
| 8169 | #⅒- 1|10 # fails under MacOS |
| 8170 | ℯ exp(1) # U+212F, base of natural log |
| 8171 | µ- micro # micro sign U+00B5 |
| 8172 | μ- micro # small mu U+03BC |
| 8173 | ångström angstrom |
| 8174 | Å angstrom # angstrom symbol U+212B |
| 8175 | Å angstrom # A with ring U+00C5 |
| 8176 | röntgen roentgen |
| 8177 | °C degC |
| 8178 | °F degF |
| 8179 | °K K # °K is incorrect notation |
| 8180 | °R degR |
| 8181 | ° degree |
| 8182 | ℃ degC |
| 8183 | ℉ degF |
| 8184 | K K # Kelvin symbol, U+212A |
| 8185 | ℓ liter # unofficial abbreviation used in some places |
| 8186 | Ω ohm # Ohm symbol U+2126 |
| 8187 | Ω ohm # Greek capital omega U+03A9 |
| 8188 | ℧ mho |
| 8189 | G₀ G0 |
| 8190 | H₀ H0 |
| 8191 | Z₀ Z0 |
| 8192 | a₀ a0 |
| 8193 | n₀ n0 |
| 8194 | ε₀ epsilon0 |
| 8195 | μ₀ mu0 |
| 8196 | Φ₀ Phi0 |
| 8197 | R∞ Rinfinity |
| 8198 | R_∞ Rinfinity |
| 8199 | λ_C lambda_C |
| 8200 | μ_B mu_B |
| 8201 | ν_133Cs nu_133Cs |
| 8202 | ʒ dram # U+0292 |
| 8203 | ℈ scruple |
| 8204 | ℥ ounce |
| 8205 | ℔ lb |
| 8206 | ℎ h |
| 8207 | ℏ hbar |
| 8208 | τ tau |
| 8209 | π pi # Greek letter pi |
| 8210 | 𝜋 pi # mathematical italic small pi |
| 8211 | α alpha |
| 8212 | σ sigma |
| 8213 | ‰ 1|1000 |
| 8214 | ‱ 1|10000 |
| 8215 | ′ ' # U+2032 |
| 8216 | ″ " # U+2033 |
| 8217 | |
| 8218 | # |
| 8219 | # Unicode currency symbols |
| 8220 | # |
| 8221 | |
| 8222 | ¢ cent |
| 8223 | £ britainpound |
| 8224 | ¥ japanyen |
| 8225 | € euro |
| 8226 | ₩ southkoreawon |
| 8227 | ₪ israelnewshekel |
| 8228 | ₤ lira |
| 8229 | # ₺ turkeylira # fails under MacOS |
| 8230 | ₨ rupee # unofficial legacy rupee sign |
| 8231 | # ₹ indiarupee # official rupee sign # MacOS fail |
| 8232 | #؋ afghanafghani # fails under MacOS |
| 8233 | ฿ thailandbaht |
| 8234 | ₡ costaricacolon |
| 8235 | ₣ francefranc |
| 8236 | ₦ nigerianaira |
| 8237 | ₧ spainpeseta |
| 8238 | ₫ vietnamdong |
| 8239 | ₭ laokip |
| 8240 | ₮ mongoliatugrik |
| 8241 | ₯ greecedrachma |
| 8242 | ₱ philippinepeso |
| 8243 | # ₲ paraguayguarani # fails under MacOS |
| 8244 | #₴ ukrainehryvnia # fails under MacOS |
| 8245 | #₵ ghanacedi # fails under MacOS |
| 8246 | #₸ kazakhstantenge # fails under MacOS |
| 8247 | #₼ azerbaijanmanat # fails under MacOS |
| 8248 | #₽ russiaruble # fails under MacOS |
| 8249 | #₾ georgialari # fails under MacOS |
| 8250 | ﷼ iranrial |
| 8251 | ﹩ $ |
| 8252 | ¢ ¢ |
| 8253 | £ £ |
| 8254 | ¥ ¥ |
| 8255 | ₩ ₩ |
| 8256 | |
| 8257 | # |
| 8258 | # Square Unicode symbols starting at U+3371 |
| 8259 | # |
| 8260 | |
| 8261 | ㍱ hPa |
| 8262 | ㍲ da |
| 8263 | ㍳ au |
| 8264 | ㍴ bar |
| 8265 | # ㍵ oV??? |
| 8266 | ㍶ pc |
| 8267 | #㍷ dm invalid on Mac |
| 8268 | #㍸ dm^2 invalid on Mac |
| 8269 | #㍹ dm^3 invalid on Mac |
| 8270 | ㎀ pA |
| 8271 | ㎁ nA |
| 8272 | ㎂ µA |
| 8273 | ㎃ mA |
| 8274 | ㎄ kA |
| 8275 | ㎅ kB |
| 8276 | ㎆ MB |
| 8277 | ㎇ GB |
| 8278 | ㎈ cal |
| 8279 | ㎉ kcal |
| 8280 | ㎊ pF |
| 8281 | ㎋ nF |
| 8282 | ㎌ µF |
| 8283 | ㎍ µg |
| 8284 | ㎎ mg |
| 8285 | ㎏ kg |
| 8286 | ㎐ Hz |
| 8287 | ㎑ kHz |
| 8288 | ㎒ MHz |
| 8289 | ㎓ GHz |
| 8290 | ㎔ THz |
| 8291 | ㎕ µL |
| 8292 | ㎖ mL |
| 8293 | ㎗ dL |
| 8294 | ㎘ kL |
| 8295 | ㎙ fm |
| 8296 | ㎚ nm |
| 8297 | ㎛ µm |
| 8298 | ㎜ mm |
| 8299 | ㎝ cm |
| 8300 | ㎞ km |
| 8301 | ㎟ mm^2 |
| 8302 | ㎠ cm^2 |
| 8303 | ㎡ m^2 |
| 8304 | ㎢ km^2 |
| 8305 | ㎣ mm^3 |
| 8306 | ㎤ cm^3 |
| 8307 | ㎥ m^3 |
| 8308 | ㎦ km^3 |
| 8309 | ㎧ m/s |
| 8310 | ㎨ m/s^2 |
| 8311 | ㎩ Pa |
| 8312 | ㎪ kPa |
| 8313 | ㎫ MPa |
| 8314 | ㎬ GPa |
| 8315 | ㎭ rad |
| 8316 | ㎮ rad/s |
| 8317 | ㎯ rad/s^2 |
| 8318 | ㎰ ps |
| 8319 | ㎱ ns |
| 8320 | ㎲ µs |
| 8321 | ㎳ ms |
| 8322 | ㎴ pV |
| 8323 | ㎵ nV |
| 8324 | ㎶ µV |
| 8325 | ㎷ mV |
| 8326 | ㎸ kV |
| 8327 | ㎹ MV |
| 8328 | ㎺ pW |
| 8329 | ㎻ nW |
| 8330 | ㎼ µW |
| 8331 | ㎽ mW |
| 8332 | ㎾ kW |
| 8333 | ㎿ MW |
| 8334 | ㏀ kΩ |
| 8335 | ㏁ MΩ |
| 8336 | ㏃ Bq |
| 8337 | ㏄ cc |
| 8338 | ㏅ cd |
| 8339 | ㏆ C/kg |
| 8340 | ㏈() dB |
| 8341 | ㏉ Gy |
| 8342 | ㏊ ha |
| 8343 | # ㏋ HP?? |
| 8344 | ㏌ in |
| 8345 | # ㏍ KK?? |
| 8346 | # ㏎ KM??? |
| 8347 | ㏏ kt |
| 8348 | ㏐ lm |
| 8349 | # ㏑ ln |
| 8350 | # ㏒ log |
| 8351 | ㏓ lx |
| 8352 | ㏔ mb |
| 8353 | ㏕ mil |
| 8354 | ㏖ mol |
| 8355 | ㏗() pH |
| 8356 | ㏙ ppm |
| 8357 | # ㏚ PR??? |
| 8358 | ㏛ sr |
| 8359 | ㏜ Sv |
| 8360 | ㏝ Wb |
| 8361 | #㏞ V/m Invalid on Mac |
| 8362 | #㏟ A/m Invalid on Mac |
| 8363 | #㏿ gal Invalid on Mac |
| 8364 | |
| 8365 | !endutf8 |
| 8366 | |
| 8367 | ############################################################################ |
| 8368 | # |
| 8369 | # Unit list aliases |
| 8370 | # |
| 8371 | # These provide a shorthand for conversions to unit lists. |
| 8372 | # |
| 8373 | ############################################################################ |
| 8374 | |
| 8375 | !unitlist uswt lb;oz |
| 8376 | !unitlist hms hr;min;sec |
| 8377 | !unitlist time year;day;hr;min;sec |
| 8378 | !unitlist dms deg;arcmin;arcsec |
| 8379 | !unitlist ftin ft;in;1|8 in |
| 8380 | !unitlist inchfine in;1|8 in;1|16 in;1|32 in;1|64 in |
| 8381 | !unitlist usvol cup;3|4 cup;2|3 cup;1|2 cup;1|3 cup;1|4 cup;\ |
| 8382 | tbsp;tsp;1|2 tsp;1|4 tsp;1|8 tsp |
| 8383 | |
| 8384 | ############################################################################ |
| 8385 | # |
| 8386 | # The following units were in the Unix units database but do not appear in |
| 8387 | # this file: |
| 8388 | # |
| 8389 | # wey used for cheese, salt and other goods. Measured mass or |
| 8390 | # waymass volume depending on what was measured and where the measuring |
| 8391 | # took place. A wey of cheese ranged from 200 to 324 pounds. |
| 8392 | # |
| 8393 | # sack No precise definition |
| 8394 | # |
| 8395 | # spindle The length depends on the type of yarn |
| 8396 | # |
| 8397 | # block Defined variously on different computer systems |
| 8398 | # |
| 8399 | # erlang A unit of telephone traffic defined variously. |
| 8400 | # Omitted because there are no other units for this |
| 8401 | # dimension. Is this true? What about CCS = 1/36 erlang? |
| 8402 | # Erlang is supposed to be dimensionless. One erlang means |
| 8403 | # a single channel occupied for one hour. |
| 8404 | # |
| 8405 | ############################################################################ |
| 8406 | # |
| 8407 | # The following have been suggested or considered and deemed out of scope. |
| 8408 | # They will not be added to GNU units. |
| 8409 | # |
| 8410 | # Conversions between different calendar systems used in different countries or |
| 8411 | # different historical periods are out of scope for units and will not be added. |
| 8412 | # |
| 8413 | # Wind chill and heat index cannot be handled because they are bivarite, |
| 8414 | # with dependence on both the temperature and wind speed or humidity. |
| 8415 | # |
| 8416 | # Plain english text output like "one hectare is equivalent to one hundred |
| 8417 | # million square centimeters" is out of scope. |
| 8418 | # |