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18.2 LIQUEFACTION BY EXPANSION – METHOD (II)          435






                  800


                                                  Higher inversion temperature
                 T / K
                  600                        Cooling always occurs
                 Inversion temperature,   400    in this region







                  200
                                                  Lower inversion temperature


                   0
                     0          50        100        150       200        250       300        350
                                                     Pressure / bar

               FIGURE 18.9
               Higher and lower inversion temperatures for air.


               give 224 K and 24.9 K respectively for the maximum and minimum inversion temperatures. The
               maximum pressure at which inversion can be achieved is 117 bar.
                  The inversion curve goes through the lines of constant enthalpy at the point where (vT/vp) h ¼ 0. To
               the left of the inversion curve cooling always occurs; to the right heating or cooling occurs depending
               on the values of the pressure.
                  Figure 18.9 may be drawn in a more general manner by replotting it in terms of the reduced
               pressure (p R ) and temperature (T R ) used in the Law of Corresponding States (see Chapter 8, Section
               8.3). This generalised diagram is shown in Fig. 18.10. Also shown on that diagram is the saturation line
               for water plotted in nondimensional form. For a gas to be cooled using the Joule–Thomson effect, it is
               necessary that its state lies in the region shown on Fig. 18.10. Consideration of Table 18.1 shows that
               for oxygen and nitrogen at atmospheric temperature the values of reduced temperature are 2.10 and
               2.38 respectively. Hence, these gases can both be liquefied at pressures up to 8p c , i.e. approximately
               400 and 270 bar respectively. However, hydrogen at atmospheric temperature has a T R value of 10, and
               lies outside the range of the Joule–Thomson effect. To be able to liquefy hydrogen by this method, it is
               necessary to precool it by using another fluid, e.g. liquid nitrogen when the value of T R could become
               as low as 4.2, which is well within the range of inversion temperatures.


               18.2.3 LINDE LIQUEFACTION PLANT
               Many gases are liquefied using the Joule–Thomson effect. This approach is embodied in the Linde
               liquefaction process, and a schematic of the equipment is shown in Fig. 18.11(a), while the thermo-
               dynamic processes are depicted in Fig. 18.11(b). The Linde process is similar to a refrigerator
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