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22     Chapter 2  Structure of  Thermodynamics


                                       obtained by use of  the operations of calculus. The third law states that the entropy
                                       of each pure element or substance in a perfect crystalline form is zero at absolute
                                       zero.
                                           The entropy provides  a criterion  of  spontaneous change  and equilibrium  at
                                       constant  U  and  V  because  (dS),.,  3 0. Thus the entropy  of  an isolated  system
                                       can only increase and has its maximum value at equilibrium. The internal energy
                                       also provides  a criterion for spontaneous change and equilibrium. That criterion
                                       is (dU),,,  6 0, which indicates that when spontaneous changes occur in a system
                                       described  by equation 2.2-1 at constant S  and V; U can only decrease  and has its
                                       minimum value  at equilibrium.
                                           The inequalities of  the previous paragraph are extremely important, but they
                                       are of little direct use to experimenters because there is no convenient way to hold
                                       U and S constant except in isolated  systems and adiabatic processes.  In  both  of
                                       these  inequalities,  the  independent  variables  (the  properties  that  are  held  con-
                                       stant) are all extensive variables. There is just one way to define thermodynamic
                                       properties  that  provide  criteria  of  spontaneous change  and  equilibrium  when
                                       intensive  variables  are  held  constant,  and  that  is  by  the  use  of  Legendre
                                       transforms. That can be illustrated  here with equation  2.2-1, but a more complete
                                       discussion  of  Legendre  transforms  is  given  in  Section  2.5.  Since  laboratory
                                       experiments  are  usually  carried  out  at  constant  pressure,  rather  than  constant
                                       volume, a new thermodynamic  potential, the enthalpy H, can be defined by
                                                                     H=U+PV                            (2.2-2)

                                       The differential of  the enthalpy is given by
                                                                dH = dU + PdV+  VdP                    (2.2-3)

                                       Substituting equation 2.2-1 yields
                                                                  dH = TdS + VdP                       (2.2-4)

                                       The use  of  a  Legendre  transform  has  introduced  an intensive property  P as an
                                       independent  variable.  It can be shown that the criterion for spontaneous change
                                       and equilibrium  is given by  (dH),,,  3 0.
                                           The temperature can be  introduced  as an independent  variable  by  defining
                                       the Gibbs energy G  with the Legendre transform
                                                                     G=H-TS                            (2.2-5)

                                       The differential of  the Gibbs energy is given by
                                                                dG = dH - TdS - SdT                     (2.2-6)

                                        Substituting equation 2.2-4 yields
                                                                  dG = -SdT+  VdP                       (2.2-7)

                                        The use of this Legendre transform  has introduced the intensive property  T as an
                                        independent  variable.  It can  be shown that the criterion for spontaneous change
                                        and equilibrium is given by (dG),,,  3 0. The Gibbs energy is so useful because  T
                                        and P  are convenient  intensive variables to hold constant and because, as we will
                                        see shortly, if G can be determined  as a function  of  T and P, then  S, V, H, and  U
                                        can all be calculated.
                                           Gibbs (1873) showed how to include the contributions of added matter to the
                                        fundamental  equation by  introducing  the concept  of  the chemical potential p, of
                                        species i and writing the fundamental equation for the internal energy of a system
                                        involving  PV work  and changes in the amounts n, of  species as
                                                                                 v<
                                                              dU = TdS - PdV+  2 pidni                  (2.2-8)
                                                                                i=  1
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