Page 380 - Air pollution and greenhouse gases from basic concepts to engineering applications for air emission control
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12.4  Carbon Capture Processes                                  359

              For an adiabatic constant pressure system, with the reactant temperature of
            T R = T 0 = 298 K, the left-hand side (LHS) of Eq. (12.15)

                                        b i  2        2    o
                  X
                      n i  a i ðT R   298 KÞþ  ðT  ð298 KÞ  þ h f ;i
                                            R
                                        2
                   R
                                                                        ð12:15Þ

                                            b i  2        2    o
                       X
                     ¼    n i  a i ðT a   298 KÞþ  ðT  ð298 KÞ  þ h f ;i
                                                a
                                             2
                        P
            becomes
                                    LHS ¼ h o  þ 2h o                       ð1Þ
                                           f ;CH 4  f ;O 2
            The right-hand side (RHS) of the equation is simplified as

                                           b CO 2  2       2    o
                  RHS ¼    a CO 2  ðT a   298 KÞþ  ðT  ð298 KÞ  þ h
                                                 a
                                             2                  f ;CO 2
                                                                            ð2Þ

                                              b H 2 O  2      2     o
                        þ 2   a H 2 O ðT a   298 KÞþ  ðT  ð298 KÞ  þ h f ;H 2 O
                                                    a
                                                2
            Looking into Table A.4, we can get the parameters needed (Table 12.4)
              Substituting these values into Eq. (1) and Eq. (2) leads to
              LHS ¼ 74;980 J=moleÞ
                            ð
                                         0:0073  2         2

              RHS ¼    44:3191ðT a   298Þþ     ðT  ð298 KÞ     394;088
                                                 a
                                           2

                                              0:00862  2        2
                     þ 2  32:4766ðT a   298 KÞþ     ðT  ð298 KÞ      242;174
                                                      a
                                                2
              Simplification of the equation gives
                                    2
                            0:01227T þ 109:2723 T a   837109 ¼ 0
                                    a
              Solving this equation we can get, T a = 4930.8 K. This calculated value is much
            higher that air-fuel combustion: T a ¼ 2341 K.

            Table 12.4 Parameters used in Example 1.22
            Species            h o f ;i  (J/mole)    C p (T) (J/mole · K)
                                                     a i                b i
            CO 2               −394,088              44.3191            0.0073
            H 2 O              −242,174              32.4766            0.00862
            O 2                0                     30.5041            0.00349
            CH 4               −74,980               44.2539            0.02273
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