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Handbook of air conditioning and refrigeration / Shan K

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2.8 CHAPTER TWO<br />

Degree <strong>of</strong> Saturation<br />

where n a � number <strong>of</strong> moles <strong>of</strong> dry <strong>air</strong>, mol<br />

n w � number <strong>of</strong> moles <strong>of</strong> water vapor in moist <strong>air</strong> sample, mol<br />

n ws � number <strong>of</strong> moles <strong>of</strong> water vapor in saturated moist <strong>air</strong> sample, mol<br />

Moist <strong>air</strong> is a binary mixture <strong>of</strong> dry <strong>air</strong> <strong>and</strong> water vapor; therefore, we find that the sum <strong>of</strong> the mole<br />

fractions <strong>of</strong> dry <strong>air</strong> x a <strong>and</strong> water vapor x w is equal to 1, that is,<br />

x a � x w � 1 (2.20)<br />

If we apply ideal gas equations p wV � n wR oT R <strong>and</strong> p aV � n aR oT R, by substituting them into<br />

Eq. (2.19), then the relative humidity can also be expressed as<br />

(2.21)<br />

The water vapor pressure <strong>of</strong> saturated moist <strong>air</strong> p ws is a function <strong>of</strong> temperature T <strong>and</strong> pressure p,<br />

which is slightly different from the saturation pressure <strong>of</strong> water vapor p s. Here p s is a function <strong>of</strong><br />

temperature T only. Since the difference between p ws <strong>and</strong> p s is small, it is usually ignored.<br />

The degree <strong>of</strong> saturation � is defined as the ratio <strong>of</strong> the humidity ratio <strong>of</strong> moist <strong>air</strong> w to the humidity<br />

ratio <strong>of</strong> the saturated moist <strong>air</strong> w s at the same temperature <strong>and</strong> pressure. This relationship can be<br />

expressed as<br />

(2.22)<br />

Since from Eqs. (2.15), (2.20), <strong>and</strong> (2.21) w � 0.62198 x w/x a <strong>and</strong> w s � 0.62198 x ws/x a, Eqs. (2.20),<br />

(2.21), <strong>and</strong> (2.22) can be combined, so that<br />

�<br />

(2.23)<br />

1 � (1 � �)x ws 1 � (1 � �)( pws /pat) In Eq. (2.23), pws�� pat; therefore, the difference between � <strong>and</strong> � is small. Usually, the maximum<br />

difference is less than 2 percent.<br />

2.5 PROPERTIES OF MOIST AIR<br />

Enthalpy<br />

� �<br />

The difference in specific enthalpy �h for an ideal gas, in Btu/lb (kJ/kg), at a constant pressure can<br />

be defined as<br />

where c p � specific heat at constant pressure, Btu/lb�°F (kJ/kg�K)<br />

T 1, T 2 � temperature <strong>of</strong> ideal gas at points 1 <strong>and</strong> 2, °F (°C)<br />

�<br />

� � p w<br />

� � w<br />

�T,p pws �h � c p (T 2 � T 1) (2.24)<br />

As moist <strong>air</strong> is approximately a binary mixture <strong>of</strong> dry <strong>air</strong> <strong>and</strong> water vapor, the enthalpy <strong>of</strong> the moist<br />

<strong>air</strong> can be evaluated as<br />

w s<br />

h � h a � H w<br />

� T,p<br />

�<br />

(2.25)

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