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Handbook of air conditioning and refrigeration / Shan K

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2.4 HUMIDITY<br />

Humidity Ratio<br />

Relative Humidity<br />

Amplifier(s). The measured electric signal from the temperature sensor is amplified at the solid<br />

state amplifier to produce an output for indication. The number <strong>of</strong> amplifiers is matched with the<br />

number <strong>of</strong> the sensors used in the temperature indication system.<br />

Indicator. An analog-type indicator, one based on directly measurable quantities, is usually a<br />

moving coil instrument. For a digital-type indicator, the signal from the amplifier is compared with<br />

an internal reference voltage <strong>and</strong> converted for indication through an analog-digital transducer.<br />

The humidity ratio <strong>of</strong> moist <strong>air</strong> w is the ratio <strong>of</strong> the mass <strong>of</strong> water vapor m w to the mass <strong>of</strong> dry <strong>air</strong> m a<br />

contained in the mixture <strong>of</strong> the moist <strong>air</strong>, in lb/lb (kg/kg). The humidity ratio can be calculated as<br />

w � (2.14)<br />

Since dry <strong>air</strong> <strong>and</strong> water vapor can occupy the same volume at the same temperature, we can apply the<br />

ideal gas equation <strong>and</strong> Dalton’s law for dry <strong>air</strong> <strong>and</strong> water vapor. Equation (2.14) can be rewritten as<br />

m w<br />

m a<br />

w � m w<br />

m a<br />

� p wVR aT R<br />

P aVR wT R<br />

� (2.15)<br />

where Ra, Rw � gas constant for dry <strong>air</strong> <strong>and</strong> water vapor, respectively, ft�lbf/lbm�°R(J/kg�K). Equation<br />

(2.15) is expressed in the form <strong>of</strong> the ratio <strong>of</strong> pressures; therefore, pw <strong>and</strong> pat must have the<br />

same units, either psia or psf (Pa).<br />

For moist <strong>air</strong> at saturation, Eq. (2.15) becomes<br />

53.352<br />

� 0.62198<br />

85.778 pat � pw pat � pw where p ws � pressure <strong>of</strong> water vapor <strong>of</strong> moist <strong>air</strong> at saturation, psia or psf (Pa).<br />

(2.16)<br />

The relative humidity � <strong>of</strong> moist <strong>air</strong>, or RH, is defined as the ratio <strong>of</strong> the mole fraction <strong>of</strong> water vapor<br />

x w in a moist <strong>air</strong> sample to the mole fraction <strong>of</strong> the water vapor in a saturated moist <strong>air</strong> sample<br />

x ws at the same temperature <strong>and</strong> pressure. This relationship can be expressed as<br />

And, by definition, the following expressions may be written:<br />

p w<br />

w s � 0.62198<br />

� � x w<br />

x w �<br />

x ws �<br />

� R a<br />

R w<br />

p ws<br />

p at � p ws<br />

�T,p x ws<br />

n w<br />

n a � n w<br />

n ws<br />

n a � n ws<br />

p w<br />

p at � p w<br />

p w<br />

PSYCHROMETRICS 2.7<br />

(2.17)<br />

(2.18)<br />

(2.19)

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