Page 144 - Thermodynamics of Biochemical Reactions
P. 144

142     Chapter 8  Phase  Equilibrium in Aqueous  Systems


                                       extensive degrees of freedom  D  have been discussed in Chapter 3, and F'  and D'
                                       at specified  pH have  been  discussed  in  Chapter 4. That discussion  is  continued
                                       here.  The  distribution  of  carbon  dioxide  between  the  gas  phase  and  aqueous
                                       solution  is discussed as a function of  pH and ionic strength.


                                          8.1  TWO-PHASE SYSTEMS WITHOUT CHEMICAL
                                               REACTIONS

                                       One Species, Two Phases
                                       This system is not  useful for representing a biochemical  system  but  is needed  as
                                       a foundation. The fundamental equation for G for a system containing alpha and
                                       beta phases

                                                        dG = - SdT+  VdP + pAzd/TA1 + pAgdMA,j         (8.1-1)
                                       This  shows  that  the  natural  variables  for  G  for  this  system  before  phase
                                       equilibrium is established are 7; P, nAa, and t7!,.  When A  is transferred  from one
                                       phase  to  the  other. di?,,  = - dnA8. Substituting  this  conservation  relation  into
                                       equation 8.1  -1 yields
                                                         dG  = - SdT+ VdP + (~1.4~ - /L,%p)dlZA1       (8.1 -2)

                                       which  shows that /iAS = pAO = p,  at phase equilibrium. Substituting  this equilib-
                                       rium  condition in equation 8.1-1 yields

                                            dG = - SdT+  VdP + p,(dn,,  + drtA0) = - SdT+  VdP + /[,d/l,q   (8.1-3)
                                       where  IZ,, is  the  amount  of  component  A  in  the  two-phase  system.  This
                                       fundamental equation  shows  that  the  system  at  phase  equilibrium  has  D  = 3
                                       natural variables,  which  seems to suggest  7;  P, and ncA. However, we  will  see in
                                       the  next  paragraph  that  this  is  not  a  suitable  choice  of  natural  variables.  The
                                       Gibbs-Duhem equations for the two phases at phase equilibrium are

                                                             0 =  S,dT+  ljdP - nA,d/lA                (8.1-4)
                                                                 ~
                                                             0 = - S,dT+  VOdP  - ltAadL1,             (8.1-5)

                                       Eliminating dp,  between  these two equations yields the Clapeyron equation
                                                                    dP    AH,,
                                                                        -                              (8.1 -6)
                                                                    d T   TA V,,

                                       where AH  = HmAa - H,,,   = T(S,,,   - S,,&  is the change in molar enthalpy and
                                       AVm is  the  change  in  molar volume in  the  phase  change. Thus the  pressure  can
                                       be  taken  to be a function of the temperature, or the temperature can be taken  to
                                       a  function  of  the  pressure.  This indicates that  a two-phase  system  with  a  single
                                       species has a single independent  intensive variable, in  agreement  with  the  phase
                                       rule F  = C -p + 2  = 1  - 2 + 2= 1.
                                           Using  the  Clapeyron  equation  to  eliminate  dP from  equation  8.1-1  and
                                       substituting /iAa = 1-1,~~ yields

                                                                                                       (8.1-7)


                                       This form  of  the fundamental equation, which  applies  at  equilibrium,  indicates
                                       that the natural variables for this system are 7: nAar and nA8. Alternatively, P, nAZ,
                                       and nAp could  be  chosen. Specification of  the natural variables  gives a complete
                                       description of  the extensive state of  the system at equilibrium, and so the criterion
                                       of  spontaneous change and equilibrium  is dG < 0 at constant  7; it4z, and  H,,,~ or
   139   140   141   142   143   144   145   146   147   148   149