Page 196 - Physical chemistry understanding our chemical world
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THERMODYNAMICS AND THE EXTENT OF REACTION       163

                   +
             + H 3 O . This reaction has an equilibrium constant K of about 2 ×
             10 −5  at room temperature (298 K) when formulated in the usual units  The correct use of the
                                  −3                                      van’t Hoff isotherm
             of concentration (mol dm ). What is the associated change in Gibbs
             function of this reaction?                                   necessitates using the
                                                                          thermodynamic tem-
                                                                          perature (expressed
                                                                          in kelvin).
             Inserting values into the van’t Hoff isotherm (Equation (4.55)):
                                                              −5
                       O
                     G =−8.314 J K  −1  mol −1  × 298 K × ln(2 × 10 )
                       O
                     G =−2478 J mol   −1  ×−10.8                          A process occurring
                                                                          with a negative value
                                       −1
                       O
                     G =+26 811 J mol
                                                                          of  G is said to be
                                                                          exogenic. A process
             so
                                                                          occurring with a posi-
                                           O
                                         G =+26.8 kJ mol  −1              tive value of  G is said
                                                                          to be endogenic.
                         O
             Note how  G is positive here. We say it is endogenic.
                                     Justification Box 4.6

                We start with Equation (4.49):

                                                  O
                                          G =  G + RT ln Q
                At equilibrium, the value of  G is zero. Also, the value of Q is called K:

                                               O
                                        0 =  G + RT ln K                        (4.56)
                Subtracting the ‘−RT ln K’ term from both sides yields the van’t Hoff isotherm
                (Equation (4.55)):
                                              O
                                            G =−RT ln K
                                                                             O
                This derivation proves that equilibrium constants do exist. The value of  G depends
                on T , so the value of K should be independent of the total pressure.



                                                                        O
             We sometimes want to know the value of K from a value of  G , in which case
             we employ a rearranged form of the isotherm:

                                                   − G  O
                                         K = exp                                  (4.57)
                                                     RT
             so a small change in the Gibbs function means a small value of K. Therefore, a weak
             acid is weak simply because  G is small.
                                          O
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