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Thermodynamics

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cen84959_ch03.qxd 4/25/05 2:47 PM Page 116116 | <strong>Thermodynamics</strong>Use actual data from the experimentshown here to obtain the latent heatof fusion of water. See end-of-chapterproblem 3–146.© Ronald MullisenTABLE 3–1EXPERIMENTSaturation (boiling) pressure ofwater at various temperaturesSaturationTemperature, pressure,T, °C P sat , kPa10 0.265 0.400 0.615 0.8710 1.2315 1.7120 2.3425 3.1730 4.2540 7.3950 12.35100 101.4150 476.2200 1555250 3976300 8588practically all substances. A partial listing of such a table is given inTable 3–1 for water. This table indicates that the pressure of water changingphase (boiling or condensing) at 25°C must be 3.17 kPa, and the pressure ofwater must be maintained at 3976 kPa (about 40 atm) to have it boil at250°C. Also, water can be frozen by dropping its pressure below 0.61 kPa.It takes a large amount of energy to melt a solid or vaporize a liquid. Theamount of energy absorbed or released during a phase-change process iscalled the latent heat. More specifically, the amount of energy absorbedduring melting is called the latent heat of fusion and is equivalent to theamount of energy released during freezing. Similarly, the amount of energyabsorbed during vaporization is called the latent heat of vaporization andis equivalent to the energy released during condensation. The magnitudes ofthe latent heats depend on the temperature or pressure at which the phasechange occurs. At 1 atm pressure, the latent heat of fusion of water is 333.7kJ/kg and the latent heat of vaporization is 2256.5 kJ/kg.During a phase-change process, pressure and temperature are obviouslydependent properties, and there is a definite relation between them, that is,T sat f (P sat ). A plot of T sat versus P sat , such as the one given for water inFig. 3–12, is called a liquid–vapor saturation curve. A curve of this kindis characteristic of all pure substances.It is clear from Fig. 3–12 that T sat increases with P sat . Thus, a substanceat higher pressures boils at higher temperatures. In the kitchen, higher boilingtemperatures mean shorter cooking times and energy savings. A beefstew, for example, may take 1 to 2 h to cook in a regular pan that operatesat 1 atm pressure, but only 20 min in a pressure cooker operating at 3 atmabsolute pressure (corresponding boiling temperature: 134°C).The atmospheric pressure, and thus the boiling temperature of water,decreases with elevation. Therefore, it takes longer to cook at higher altitudesthan it does at sea level (unless a pressure cooker is used). For example,the standard atmospheric pressure at an elevation of 2000 m is 79.50kPa, which corresponds to a boiling temperature of 93.3°C as opposed to100°C at sea level (zero elevation). The variation of the boiling temperatureof water with altitude at standard atmospheric conditions is given inTable 3–2. For each 1000 m increase in elevation, the boiling temperatureP sat , kPa600400FIGURE 3–12The liquid–vapor saturation curve of apure substance (numerical values arefor water).2000 0 50 100 150 200T sat ,°C

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