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CHAPTER 13 Gas – Vapor Mixtures and Air-Conditioning
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-1 FIGURE 13-1 The C p of air can be assumed to be constant at 1.005 kJ/(kg · °C) in the temperature range - 10 to 50°C with an error under 0.2 percent.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. FIGURE 13-2 At temperatures below 50 C, the h = constant lines coincide with the T = constant lines in the superheated vapor region of water. 13-2
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-3 FIGURE 13-4 For saturated air, the vapor pressure is equal to the saturation pressure of water.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-4 FIGURE 13-5 Specific humidity is the actual amount of water vapor in 1 kg of dry air, whereas relative humidity is the ratio of the actual amount of moisture in the air to the maximum amount of moisture air can hold at that temperature.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-5 FIGURE 13-6 The enthalpy of moist (atmospheric) air is expressed per unit mass of dry air, not per unit mass of moist air.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-6 FIGURE 13-8 Constant- pressure cooling of moist air and the dew-point temperature on the T-s diagram of water.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-7 FIGURE 13-11 The adiabatic saturation process and its represen-tation on a T-s diagram of water.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-8 FIGURE 13-12 A simple arrangement to measure the wet- bulb temperature.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-9 FIGURE 13-14 Schematic for a psychrometric chart.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-10 FIGURE 13-15 For saturated air, the dry-bulb, wet- bulb, and dew- point temperatures are identical.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-11 FIGURE 13-20 Various air- conditioning processes.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-12 FIGURE 13-21 During simple heating, specific humidity remains constant, but relative humidity decreases.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-13 FIGURE 13-22 During simple cooling, specific humidity remains constant, but relative humidity increases.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-14 FIGURE 13-23 Heating the humidification.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-15 FIGURE 13-24 Schematic and psychrometric chart for Example 13–5.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-16 FIGURE 13-25 Schematic and psychrometric chart for Example 13–6.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-17 FIGURE 13-27 Evaporative cooling.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-18 FIGURE 13-29 When two airstreams at states 1 and 2 are mixed adiabatically, the state of the mixture lies on the straight line connecting the two states.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-19 FIGURE 13-31 An induced-draft counterflow cooling tower.
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Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 13-20 Photo credit: Yunus Çengel FIGURE 13-33 A spray pond.
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