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28     Chapter 2  Structure of Thermodynamics


                                           Substituting the  integrated fundamental equation for  U (equation 2.2-14) in
                                       the Legendre transforms  defining H, A, and G  shows that

                                                                   H  = TS + Cp,n,                    (2.5 - 10)
                                                                   A  = -PV+  xprnr                   (2.5-1 1)
                                                                   G  = C&n,                          (2.5-12)

                                       The interesting thing about these equations is that only  the Gibbs energy  G can
                                       be  calculated  by  adding  contributions  from  individual  species.  These  ther-
                                       modynamic potentials can be determined as functions of other variables, but only
                                       when  they  are  determined as  functions of  natural  variables can  all  of  the  ther-
                                       modynamic properties be  obtained by taking partial derivatives. Equations 2.5- 10
                                       to  2.5-1 2  can  also  be  obtained  by  integrating  the  corresponding fundamental
                                       equations at constant values of  the intensive variables.
                                           The fundamental  equation for  the  Gibbs energy  (2.5-5) yields the  following
                                       Maxwell equations:

                                                                                                      (2.5-1  3)


                                                                                                      (2.5- 14)


                                                                                                      (2.5-15)


                                                                                                      (2.5-  16)

                                       where S,(i)  is the molar entropy of  species i and  V,(i)  is its molar volume.
                                           The Helmholtz energy is not very useful as a crterion for spontaneious change
                                       and equilibrium  in  biochemistry  because  experiments  are not  done at constant
                                       volume.  However,  the  enthalpy  is  important  in  biochemistry  because  it  is
                                       connected  with  heat  evolution  and the  change  of  the equilibrium  constant with
                                       temperature. The fundamental equation for the enthalpy is

                                                                                N \
                                                             dH = TdS+PdV+         p,dn,              (2.5- 17)
                                                                               r=l
                                       Since  the  enthalpy  is  defined  by  H  = U + PI!  its  total  differential  is  dH =
                                       dU + PdV+ VdP.  Substituting  the  equation  dU = dq - PdK  given  earlier  in
                                       Section 2.2, yields dH = dq + VdP. At  constant pressure the change in enthalpy
                                       AH  is equal to the heat  q absorbed by  the system  in  the  process, which  may be
                                       irreversible. Thus thc change in enthalpy AH can be determined calorimetrically.
                                       The  change  in  enthalpy  can  also  be  determined  using  the  Gibbs-Helmholtz
                                       equation, which is introduced in the next paragraph, without  using a calorimeter.
                                           Equations 2.5-1 and 2.5-3 show that G = H  - TS. Substituting the expression
                                       for S  from equation 2.5-7 yields

                                                                                                      (2.5-1  8)

                                       This is  referred  to as a  Gibbs-Helmholtz equation, and it  provides  a  convenient
                                       way to calculate H  if  G can be determined  as a function of  7: P, and  [nrj. There
                                       is  a  corresponding relation  between  the  internal energy  U and  the  Helmholtz
                                       energy, which  is defined by equation 2.5-2:


                                                                                                      (2.5-1 9)
                                                                                          P  In ;
                                       This is also referred  to as a Gibbs-Helmholtz  equation.
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