Application to Gases.--In the case of ideal gases obeying the law aPV =RT, it follows directly from the general relations (3) that the difference S—s is constant and equal to R. It will be shown later that the specific heats of such gases cannot vary with pressure, though they may vary considerably with temperature, while the difference S—s remains constant, as in the case of hydrogen. (See HEAT.) On the other hand, vapours, like steam, though they usually approximate closely to the law aPV =RT at low pressures, show large deviations from the gas-laws at high pressures near'saturation, and the value of S shows a wide range of variation with pressure, especially near the critical point. Fortunately these variations can be deduced from the thermo dynamical relations given in a later section of this article.
Laplace subsequently showed (see HEAT) that the rate of drop of pressure dP/dV in the adiabatic expansion of a gas must exceed that for the same state at constant temperature, in the ratio, S/s=7, of the specific heats. Assuming Boyle's law for a gas at constant temperature, and y =constant in adiabatic ex pansion, it followed that the adiabatic equation must be of the form, PVC' = constant for a gas.
The adiabatic equation of Laplace and Poisson for a gas, was established long before the first law of thermodynamics was formulated, and has proved to be the most convenient type of equation for the purpose. But with the assistance of the laws of thermodynamics, the scope of the adiabatic equation in this form may be considerably extended. Thus with the assistance of the first law, in the form in which it is usually employed for mathematical purposes, namely Experimental Verification of the Adiabatic.—The most direct way of testing the adiabatic equation is to use a cylinder containing a constant charge of gas or vapour which is alternately compressed and expanded by a reciprocating piston. Indicator cards give fairly accurate values of the actual volume and pres sure, if the clearance is carefully measured, the pressure scale calibrated, and everything in perfect adjustment. But in working over large ranges of pressure, as is necessary for a satisfactory verification, there are formidable difficulties due to the wide variation of heat exchanges between the charge and the walls of the cylinder at different points of the stroke. These effects are further complicated by accidental leakage past the piston, and, in the case of steam, by the risk of condensation, both of which affect V indirectly by reducing the apparent mass of the charge. The most complete method of eliminating these uncer tain sources of error, which profoundly affect the uniformity of V throughout the cylinder, is to observe, instead of the relation between P and V, the relation between T and P, as given by the adiabatic equation in the form (io), deduced from the second law. In this case the temperature observed in the middle of the cylinder will be practically unaffected by the action of the walls, and is determined solely by the actual pressure as observed with the indicator. We are no longer concerned with the theoretical pressure, corresponding to the compression ratio by volume, which might be realized in the absence of condensation or leak age or heat-loss to the walls. These effects will still reduce the observed pressure below the theoretical value, but will not affect the relation between pressure and temperature. The success of the thermometric method depends on the construction of a ther mometer sufficiently sensitive to follow the rapid variations of temperature without appreciable lag, and on obtaining simul taneous readings of the relative values of the pressure with the same order of accuracy at the maximum and minimum points of the cycle. It is easy to cover the range of temperature with a single thermometer, but, the pressure range being upwards of o/i, it is necessary to use a separate indicator with a light spring for the low pressures. Applied in this manner the method is particularly suited to give the best average value of the index over large ranges of pressure and temperature. The procedure may be varied when it is desired to obtain the value of the index at some particular point of the scale, e.g., at high or low tem peratures.