The gas constant is theconstant of proportionality that relates the energy scale in physics to the temperature scale and the scale used foramount of substance. Thus, the value of the gas constant ultimately derives from historical decisions and accidents in the setting of units of energy, temperature and amount of substance. The Boltzmann constant and theAvogadro constant were similarly determined, which separately relate energy to temperature and particle count to amount of substance.
The gas constantR is defined as the Avogadro constantNA multiplied by the Boltzmann constantk (orkB):
Since the2019 revision of the SI, bothNA andk are defined with exact numerical values when expressed in SI units.[2] As a consequence, the SI value of the molar gas constant is exact.
Some have suggested that it might be appropriate to name the symbolR theRegnault constant in honour of the French chemistHenri Victor Regnault, whose accurate experimental data were used to calculate the early value of the constant. However, the origin of the letterR to represent the constant is elusive. The universal gas constant was apparently introduced independently byAugust Friedrich Horstmann (1873)[3][4] andDmitri Mendeleev who reported it first on 12 September 1874.[5] Using his extensive measurements of the properties of gases,[6][7] Mendeleev also calculated it with high precision, within 0.3% of its modern value.[8]
The gas constant occurs in the ideal gas law:whereP is the absolutepressure,V is the volume of gas,n is theamount of substance,m is themass, andT is thethermodynamic temperature.Rspecific is the mass-specific gas constant. The gas constant is expressed in the same unit asmolar heat.
From the ideal gas law we getwhereP is pressure,V is volume,n is the amount of a given substance, andT istemperature.
As pressure is defined as force per area, the gas equation can also be written as
Area and volume are (length)2 and (length)3 respectively. Therefore:
Since force × length = work,
The physical significance ofR is work per mole per kelvin. It may be expressed in any set of units representing work or energy (such asjoules), units representing temperature on an absolute scale (such askelvin orrankine), and any system of units designating a mole or a similar pure number that allows an equation ofmacroscopic mass and fundamental particle numbers in a system, such as an ideal gas (seeAvogadro constant).
Instead of a mole, the constant can be expressed by considering thenormal cubic metre.
Otherwise, we can also say that
Therefore, we can writeR as
And so, in terms ofSI base units,R =8.31446261815324 kg⋅m2⋅s−2⋅K−1⋅mol−1.
TheBoltzmann constantkB (alternativelyk) may be used in place of the molar gas constant by working in pure particle count,N, rather than amount of substance,n, sincewhereNA is theAvogadro constant. For example, theideal gas law in terms of the Boltzmann constant iswhereN is the number of particles (molecules in this case), or to generalize to an inhomogeneous system the local form holds:wheren =N/V is thenumber density. Finally, by defining thekinetic energy associated to the temperature,the equation becomes simplywhich is the form usually encountered instatistical mechanics and other branches oftheoretical physics.
As of 2006, the most precise measurement ofR had been obtained by measuring thespeed of soundca(P, T) inargon at the temperatureT of thetriple point of water at differentpressuresP, andextrapolating to the zero-pressure limitca(0, T). The value ofR is then obtained from the relationwhere
Thespecific gas constant of a gas or a mixture of gases (Rspecific) is given by the molar gas constant divided by themolar mass (M) of the gas or mixture:
Just as the molar gas constant can be related to theBoltzmann constant, so can the specific gas constant by dividing the Boltzmann constant by themolecular mass of the gas:
Another important relationship comes from thermodynamics.Mayer's relation relates the specific gas constant to the specific heat capacities for a calorically or thermallyperfect gas:wherecP is thespecific heat capacity for a constant pressure andcV is the specific heat capacity for a constant volume.[10]
It is common, especially in engineering applications, to represent the specific gas constant by the symbolR. In such cases, the universal gas constant is usually given a different symbol such asR to distinguish it. In any case, the context and/or unit of the gas constant should make it clear as to whether the universal or specific gas constant is being referred to.[11]
In case of air, using the perfect gas law and thestandard sea-level conditions (SSL) (air densityρ0 = 1.225 kg/m3, temperatureT0 = 288.15 K and pressurep0 =101325Pa), we have thatRair =P0/(ρ0T0) =287.052874247 J·kg−1·K−1. Then the molar mass of air is computed byM0 =R/Rair =28.964917 g/mol.[12]
TheU.S. Standard Atmosphere, 1976 (USSA1976) defines the gas constantR∗ as[13][14]R∗ =8.31432×103 N⋅m⋅kmol−1⋅K−1, equivalent to8.31432 J⋅K−1⋅mol−1.
The use of the kilomole in the unit results in an extra factor of1000 in the constant. The USSA1976 acknowledges that their defined value ofR* is not consistent with the cited values for the Avogadro constant and the Boltzmann constant.[14] This disparity is not a significant departure from accuracy –R∗ is slightly greater than 99.998% of the actual value of the constant,R = 8.31446261815324 J⋅mol−1⋅K−1[1] – and USSA1976 uses this value ofR∗ for all the calculations of the standard atmosphere. When using theISO value ofR, the calculated pressure increases by only 0.62 pascal at 11 kilometres (the equivalent of a difference of only 17.4 centimetres or 6.8 inches) and 0.292 Pa at 20 km (the equivalent of a difference of only 33.8 cm or 13.2 in).
This definition was published well before the 2019 SI revision, through which the constant was given an exact value.
^Mendeleev, Dmitri I. (September 12, 1874). "An exert from the Proceedings of the Chemical Society's Meeting on Sept. 12, 1874".Journal of Russian Chemical-Physical Society, Chemical Part.VI (7):208–209.
^Mendeleev, Dmitri I. (1875).On the elasticity of gases [Объ упругости газовъ]. A. M. Kotomin, St.-Petersburg.
^abNational Oceanic and Atmospheric Administration; National Aeronautics and Space Administration; United States Air Force (October 1976).U.S. Standard Atmosphere, 1976(PDF). Washington, D.C.: U.S. Government Printing Office. p. 3. NOAA-S/T 76-1562. Archived fromthe original(PDF) on 2007-07-05. Retrieved2007-01-16.