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Modern Engineering Thermodynamics

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424 CHAPTER 12: Mixtures of Gases and Vapors<br />

EXAMPLE 12.8 (Continued )<br />

which, with T WB = 60.0°F and T DB = 70.0°F, the psychrometric chart, Chart D.5, gives approximately<br />

ω 1 = 61 grains of water per lbm of dry air<br />

which is essentially the same as that calculated from Eq. (12.31).<br />

Exercises<br />

18. If the dry bulb temperature in the room discussed in Example 12.8 is 80.0°F rather than 70.0°F, calculate the humidity<br />

ratio in the room and compare your answer with that obtained from the psychrometric chart. Answer: ω 1 = 45.2 grains<br />

of water per lbm of dry air.<br />

19. Rework Example 12.8 for wet and dry bulb temperatures of 65.0°F and 85.0°F, respectively. Answer: ω 1 = 60.2 grains of<br />

water per lbm of dry air.<br />

20. Using the method of your choice, determine the relative humidity ratio in the room discussed in Example 12.8 when the<br />

wet and dry bulb temperatures are 18.0°C and 22.0°C, respectively. Answer: ω = 0.0115 kg of water per kg of dry air.<br />

6 The grain is the smallest of the ancient Egyptian measures of weight (see Chapter 1) and originally represented the average weight of a grain of barley<br />

corn. Today, it is still used in some engineering fields (e.g., in the heating, ventilating, and air conditioning field) as a mass unit, with 7000 grains =<br />

1 lbm.<br />

Equation (12.31) gives essentially the same values as obtained from the psychrometric chart, but the chart is<br />

much easier and quicker to use.<br />

12.7 AIR CONDITIONING<br />

Complete air conditioning involves producing an environment with desired pressure, temperature, humidity,<br />

purity, and circulation characteristics. In this section, we are concerned only with altering the temperature and<br />

the humidity in typical air conditioning applications.<br />

In Example 12.8, we see how winter air is severely dehumidified if it is simply heated up to room temperature.<br />

Water vapor must be added to bring its humidity up into the 40 to 50% relative humidity range. This can easily<br />

be done by blowing the heated air across a moist surface, as shown in Figure 12.6. This is the technique used in<br />

a common room humidifier.<br />

The humidification process 2–3 shown in Figure 12.6 is also an example of evaporative cooling. When unsaturated<br />

air is brought into contact with liquid water at the same (dry bulb) temperature, some of the water evaporates<br />

(thus cooling the mixture) and the resulting air–water vapor mixture moves upward along the T WB =<br />

constant line, as shown in Figure 12.6b. The minimum dry bulb temperature that can be produced by evaporative<br />

cooling occurs when the outlet air becomes saturated with water vapor (ϕ = 100%), then T DB = T WB .This<br />

concept is illustrated in the following example.<br />

Electrical work<br />

input<br />

Liquid water<br />

input<br />

Cold<br />

outside<br />

air<br />

1 2 3<br />

Heater Fan Moist<br />

screen<br />

(a)<br />

Warm<br />

conditioned<br />

air<br />

p w<br />

φ 1<br />

T WB<br />

φ 1 > φ 2<br />

3 ω<br />

1<br />

2<br />

φ 2<br />

T DB<br />

φ = 100%<br />

(b)<br />

Humidification<br />

and cooling<br />

2–3<br />

Heating<br />

1–2<br />

FIGURE 12.6<br />

Temperature and humidity conditioning of cold winter air.

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