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Modern Engineering Thermodynamics

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2.7 Pressure and Temperature Scales 41<br />

WHO DEVELOPED THE IDEAL GAS EQUATION OF STATE?<br />

By 1662, the English chemist Robert Boyle (1627–1691) had conducted experiments establishing that the pressure of a gas<br />

varies inversely with the volume when the temperature is held constant. In the early 1800s, the French physicists Jacques<br />

Charles (1746–1823) and Joseph Gay-Lussac (1778–1850) independently determined that the volume V of a gas increases<br />

linearly with temperature when the pressure is held constant. The Charles/Gay-Lussac relation can be written as<br />

V<br />

= 1 + αT<br />

V 0<br />

where T is in °C and V 0<br />

is the volume of the gas at 0°C. The empirical constant α is the coefficient of thermal expansion of<br />

the gas and was found to have the same value for all gases as the pressure approached zero.<br />

α = 0:003661°C − 1 1<br />

=<br />

273:15 °C − 1<br />

Since α is the same for all gases at low pressure, the Charles/Gay-Lussac equation provides a single calibration point (at V 0<br />

)<br />

temperature scale that is independent of the type of gas used, plus it defines the “size” of the degree (αV 0<br />

) on the scale.<br />

By 1820, the Boyle and Charles/Gay-Lussac results had been combined to produce the “ideal” gas equation of state:<br />

h<br />

pV = mR Tðin °CÞ + 1 i<br />

= mR½Tðin °CÞ + 273:15Š<br />

α<br />

and by then it was generally accepted that T (in °C) + 273.15 corresponded to some sort of ideal gas absolute temperature<br />

scale. However, the problem remained that this scale still appeared to depend on the thermometric measuring material (an<br />

ideal gas) and therefore did not constitute a genuine “thermodynamic” absolute temperature scale.<br />

Since the concept of an absolute temperature scale was not firmly established until 1848 by Lord Kelvin, it is remarkable<br />

that the ideal gas equation of state, which depends on the use of an absolute temperature scale, was in use a full 30 years<br />

earlier. However, historically, we find that empirical equations often precede theoretical explanations.<br />

HOW IS GAUGE PRESSURE RELATED TO ABSOLUTE PRESSURE?<br />

Absolute pressure = Gauge pressure + Local atmospheric pressure<br />

HOW DO I KNOW IF A GIVEN SI PRESSURE IS ABSOLUTE OR GAUGE?<br />

When an SI pressure appears in a textbook without such an identifier (e.g., 3.75 MPa), assume that it is an absolute<br />

pressure (i.e., 3.75 MPa-absolute). Gauge pressures should always be identified as “gauge” to avoid confusion.<br />

Temperature level<br />

Pressure<br />

level 2<br />

Freezing point<br />

of water<br />

Relative<br />

temperature<br />

Absolute<br />

temperature<br />

Atmospheric<br />

pressure<br />

Pressure<br />

level 1<br />

Gauge<br />

pressure 2<br />

Vacuum 1<br />

Absolute<br />

pressure 2<br />

Absolute<br />

pressure 1<br />

Absolute<br />

zero temperature<br />

Absolute<br />

zero pressure<br />

(a) Temperature<br />

(b) Pressure<br />

FIGURE 2.5<br />

Relative and absolute temperatures and pressures.

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