Equation of state for a perfect gas
The pressure (p), specific volume (V, volume per gram), and temperature (T) of a perfect gas are related by the equation of state:
where m is the molecular weight of the gas and R∗ is known as the universal gas constant, 8.3144 × 107 erg g−1 K−1. This equation reflects the observations of experiments with gases embodied in Boyles’ Law i.e., PV = constant at constant temperature, Charles’ law, i.e. any gas at a given pressure expands uniformly with temperature, and Avagadro's hypothesis which states that at normal temperature and pressure (273.15 K and 1013 mbar) the molecular volume is the same for all gases, namely 22.415 × 103 cm3. These three laws, as well as being true for a perfect gas, are nearly true for atmospheric gases.
Dalton's law states that in a mixture of gases, the total pressure is equal to the sum of the pressures which would be exerted by each gas if it filled the volume under consideration at the same temperature. Hence a...
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© 1998 Kluwer Academic Publishers
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Collier, C.G. (1998). Atmospheric processes associated with water in the atmosphere. In: Hydrology and Lakes. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4513-1_25
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