Values of R^{[1]} | Units |
---|---|
SI Units | |
J?K^{-1}?mol^{-1} | |
m^{3}?Pa?K^{-1}?mol^{-1} | |
kg?m^{2}?s^{-2}?K^{-1}?mol^{-1} | |
(K-12) | L?kPa?K^{-1}?mol^{-1} |
Other Common Units | |
atm?ft^{3}?lbmol^{-1}?°R^{-1} | |
psi?ft^{3}?lbmol^{-1}?°R^{-1} | |
BTU?lbmol^{-1}?°R^{-1} | |
inH_{2}O?ft^{3}?lbmol^{-1}?°R^{-1} | |
torr?ft^{3}?lbmol^{-1}?°R^{-1} | |
L?Pa?K^{-1}?mol^{-1} | |
L?bar?K^{-1}?mol^{-1} | |
L?atm?K^{-1}?mol^{-1} | |
L?Torr?K^{-1}?mol^{-1} | |
cal?K^{-1}?mol^{-1} | |
m^{3}?atm?K^{-1}?mol^{-1} | |
erg?K^{-1}?mol^{-1} |
The molar gas constant (also known as the gas constant, universal gas constant, or ideal gas constant) is denoted by the symbol R or R. It is the molar equivalent to the Boltzmann constant, expressed in units of energy per temperature increment per mole, i.e. the pressure-volume product, rather than energy per temperature increment per particle. The constant is also a combination of the constants from Boyle's law, Charles's law, Avogadro's law, and Gay-Lussac's law. It is a physical constant that is featured in many fundamental equations in the physical sciences, such as the ideal gas law, the Arrhenius equation, and the Nernst equation.
The gas constant is the constant of proportionality that relates the energy scale in physics to the temperature scale and the scale used for amount 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 the Avogadro constant were similarly determined, which separately relate energy to temperature and particle count to amount of substance.
The gas constant R is defined as the Avogadro constant N_{A} multiplied by the Boltzmann constant k (or k_{B}):
Since the 2019 redefinition of SI base units, both N_{A} and k are defined with exact numerical values when expressed in SI units.^{[2]} As a consequence, the SI value of the molar gas constant is exactly .
Some have suggested that it might be appropriate to name the symbol R the Regnault constant in honour of the French chemist Henri Victor Regnault, whose accurate experimental data were used to calculate the early value of the constant. However, the origin of the letter R to represent the constant is elusive. The universal gas constant was apparently introduced independently by Clausius' student, A.F. Horstmann (1873)^{[3]}^{[4]} and Dmitri Mendeleev who reported it first on Sep. 12, 1874.^{[5]} Using his extensive measurements of the properties of gases,^{[6]}^{[7]} he also calculated it with high precision, within 0.3% of its modern value.^{[8]}
The gas constant occurs in the ideal gas law:
From the ideal gas law PV = nRT we get:
where P is pressure, V is volume, n is number of moles of a given substance, and T is temperature.
As pressure is defined as force per area of measurement, 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 of R is work per degree per mole. It may be expressed in any set of units representing work or energy (such as joules), units representing degrees of temperature on an absolute scale (such as Kelvin or Rankine), and any system of units designating a mole or a similar pure number that allows an equation of macroscopic mass and fundamental particle numbers in a system, such as an ideal gas (see Avogadro constant).
Instead of a mole the constant can be expressed by considering the normal cubic meter.
Otherwise, we can also say that:
Therefore, we can write R as:
And so, in SI base units:
The Boltzmann constant k_{B} (alternatively k) may be used in place of the molar gas constant by working in pure particle count, N, rather than amount of substance, n, since
where N_{A} is the Avogadro constant. For example, the ideal gas law in terms of the Boltzmann constant is
where N is the number of particles (molecules in this case), or to generalize to an inhomogeneous system the local form holds:
where ?_{N} is the number density.
As of 2006, the most precise measurement of R had been obtained by measuring the speed of sound c_{a}(P, T) in argon at the temperature T of the triple point of water at different pressures P, and extrapolating to the zero-pressure limit c_{a}(0, T). The value of R is then obtained from the relation
where:
However, following the 2019 redefinition of the SI base units, R now has an exact value defined in terms of other exactly defined physical constants.
R_{specific} for dry air |
Units |
---|---|
287.058 | J?kg^{-1}?K^{-1} |
53.3533 | ft?lbf?lb^{-1}?°R^{-1} |
1,716.49 | ft?lbf?slug^{-1}?°R^{-1} |
Based on a mean molar mass for dry air of 28.9645 g/mol. |
The specific gas constant of a gas or a mixture of gases (R_{specific}) is given by the molar gas constant divided by the molar mass (M) of the gas or mixture.
Just as the ideal gas constant can be related to the Boltzmann constant, so can the specific gas constant by dividing the Boltzmann constant by the molecular 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 perfect gas and a thermally perfect gas.
where c_{p} is the specific heat capacity for a constant pressure and c_{v} is the specific heat capacity for a constant volume.^{[9]}
It is common, especially in engineering applications, to represent the specific gas constant by the symbol R. In such cases, the universal gas constant is usually given a different symbol such as R to distinguish it. In any case, the context and/or units of the gas constant should make it clear as to whether the universal or specific gas constant is being referred to.^{[10]}
The U.S. Standard Atmosphere, 1976 (USSA1976) defines the gas constant R^{*} as:^{[11]}^{[12]}
Note the use of kilomole units resulting in the factor of 1,000 in the constant. The USSA1976 acknowledges that this value is not consistent with the cited values for the Avogadro constant and the Boltzmann constant.^{[12]} This disparity is not a significant departure from accuracy, and USSA1976 uses this value of R^{*} for all the calculations of the standard atmosphere. When using the ISO value of R, the calculated pressure increases by only 0.62 pascal at 11 kilometers (the equivalent of a difference of only 17.4 centimeters 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).
Also note that this was well before the 2019 SI redefinition, through which the constant was given an exact value.