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Modern Engineering Thermodynamics

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12.4 Psychrometrics 419<br />

EXAMPLE 12.6<br />

On a particular day, the weather forecast states that the relative humidity is 56.8% when the atmospheric temperature and<br />

pressure are 25.0°C and 0.101 MPa, respectively. Determine:<br />

a. The partial pressure of the water vapor in the atmosphere.<br />

b. The humidity ratio of the atmosphere.<br />

c. The dew point temperature of the atmosphere.<br />

Solution<br />

a. From Table C.1b, we find that<br />

p sat ð25:0°CÞ = 0:003169 MPa<br />

and, from Eq. (12.24), we can calculate the partial pressure of the water vapor present in the mixture as<br />

p w = ϕp sat = 0:568ð0:003169 MPaÞ = 0:00180 MPa = 1:80 kPa<br />

b. From Dalton’s law for partial pressure, we can find the partial pressure of the dry air in the mixture as<br />

p a = p m − p w = 101 − 1:8 = 99:2 kPa<br />

then, Eq. (12.26a) gives the humidity ratio ω as<br />

ω = 0:622ðp w /p a Þ = 0:622ð1:80/99:2Þ = 0:0113 kg H 2 O per kg of dry air<br />

Note that, since the value of ω is not constrained to lie between 0 and 1, it is not reported as a percentage.<br />

c. Using Eq. (12.27) and Table C.2b, we find the dew point temperature to be<br />

T DP = T sat ð0:00180 MPaÞ = 15:8°C<br />

Exercises<br />

12. If the relative humidity in Example 12.6 is 45.0% rather than 56.8% and all the remaining variables are the same,<br />

determine the new dew point temperature. Answer: T DP = 12.1°C.<br />

13. Suppose the atmospheric temperature in Example 12.6 is 20.0°C rather than 25.0°C and all other variables remain the<br />

same. Determine the humidity ratio of this mixture. Answer: ω = 0.00830 kg H 2 O per kg of dry air.<br />

14. Rework Example 12.6 for a relative humidity of 35.0%, an atmospheric temperature of 20.0°C, and an atmospheric<br />

pressure of 0.101 MPa. Answer: (a) p w = 0.820 kPa, (b) ω = 5.00 × 10 −3 kg H 2 O per kg of dry air, (c) T DP = 4.00°C.<br />

The steady state, steady flow, isothermal boundary energy and entropy rate balances for a mixture of dry air and<br />

water vapor with negligible flow stream kinetic and potential energies can be written either on an unmixed<br />

component basis as<br />

_Q − _W + _m a ðh 1 − h 2 Þ a<br />

+ _m w ðh 1 − h 2 Þ w<br />

= 0 (12.28)<br />

and<br />

_Q /T b + _m a ðs 1 − s 2 Þ a + _m w ðs 1 − s 2 Þ w + _S p = 0 (12.29)<br />

or on a premixed mixture basis as<br />

_Q − _W + _m m ðh 1 − h 2 Þ m = 0<br />

and<br />

_Q /T b + _m m ðs 1 − s 2 Þ m<br />

+ _S p = 0<br />

where the mixture enthalpy and entropy changes are given by<br />

ðh 1 − h 2 Þ m<br />

= w a ðh 1 − h 2 Þ a<br />

+ w w ðh 1 − h 2 Þ w<br />

and<br />

ðs 1 − s 2 Þ m<br />

= w a ðs 1 − s 2 Þ a<br />

+ w w ðs 1 − s 2 Þ w

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