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144     Chapter 8  Phase Equilibrium in Aqueous  Systems


                                          8.2  TWO-PHASE SYSTEM WITH A CHEMICAL
                                               REACTION AND A SEMIPERMEABLE MEMBRANE


                                       Consider an aqueous two-phase  system containing A, B, C, and solvent H,O  in
                                       which  the  reaction  A + B = C  occurs.  The  two  phases  are  separated  by  a
                                       membrane, and the membrane is permeable  to all four species. The fundamental
                                       equation for the Gibbs energy of  the a phase is
                                           dG,  = - S,dT+  KdP + p,&nAa  +       +        + PH2ordnH2Oa (8.2-1)

                                       The corresponding equation for the fl phase is

                                            dG,  = - 'fldT+   'OdP   + p.4/JdnAB $-  pBBdnBB  + k/ldnCB  + !-lH20/ld?1H20fl
                                                                                                       (8.2-2)

                                       These equations can be used to show that at chemical equilibrium pAa + pBz = pcX
                                       and  pAa + pss = pea.  Substituting  these  equilibrium  conditions  into  equation
                                       8.2-1 yields

                                                dGa   - S~dT+ KdP + pAidncAa + pBadncBa + pH20rdnHzOz   (8.2-3)
                                       where the amount of the A component is ncAn = nAa + n,,  and the amount of the
                                       B  component  is  ncBa = nsz + nCz. The  corresponding fundamental equation for
                                       the fl phase is

                                                dG,  = -       bdP + pA/jdnc,4/, f pB/jdncB8 + pH20/jdnH20/j  (8.2-4)
                                          The  fundamental equation for  the  Gibbs energy  of  the  system  at  chemical
                                       equilibrium in each phase is the sum of equations 8.2-3 and 8.2-4:

                                                 dc  = - SdT+  VdP + ~.dncAa+ pBzdnci5,  + pH2OdnHzOa
                                                      + ~Agdn,AiI + iunpdr~cnp + 1-1H~oodnH,Op         (8.2-5)
                                       This  equation  can  be  used  to  show  that  pAa = pA0 = pA, pB, = pBB = p,,  and
                                       pHZOa
                                            = ,uHZoB = pHzo. When  these  phase  equilibrium  conditions  are inserted  in
                                       equation 8.2-5, it becomes
                                                   dC = - SdT+  VdP + ,uAdncA + ,uBdnCB + pHzOdncHz0   (8.2-6)

                                       where  nci represents  the  amount  of  component  i in  the  system.  The amount  of
                                       component A  in  the system is represented  by  ncA = ncAz + ncAp, and the amount
                                       of  the solvent is  represented  by  ncHzOn = nHzOB + itHzo,. Equation  8.2-6 indicates
                                       that there  are D  = 5 natural  variables,  and that they might  be taken  to be  7;  P,
                                       ncA, itcB, and   in the criterion of spontaneous change and equilibrium: dG < 0
                                       at constant 7: P, ncA, ncB, and ncllz0.
                                           The Gibbs-Duhem equations for the two phases at equilibrium can be derived
                                       from equations 8.2-3 and 8.2-4:

                                                    = - 'ndTf   'zdP   - ncAzdblA  - ncBadpB  - IZHzOzdpH,O   (8.2-7)
                                                  0 = - S,dT+  VodP - nCApdpA - ncBBdpB - nHzOBdpHzO  (8.2-8)
                                       where the phase subscripts on the chemical potentials have been dropped because
                                       of phase  equilibrium. dp(H20 can be eliminated between  these two equations, and
                                       the resulting equation can be solved for dpB, which is a function of  7: P, and pA.
                                       Thus  there  are  three  independent  intensive  properties,  in  agreement  with
                                       F  = C  ~  p  + 2 = 3 - 2 + 2 = 3.  This  is  in  agreement  with  D  = F  + p  =
                                       3 + 2 = 5. The  natural  variables  for  the  expression  of  the  criterion  for  sponta-
                                       neous change and equilibrium based  on G might  bc taken  to be  7: P, ncAlinCH, 17,.
                                       and nB, where  it,  = nA, + tiBa + igcz  + nSz. Then  the equilibrium condition  would
                                       be dC d 0 at constant  '17  P, ncA/ncR, n,,  and nil,.
                                           If the phases are both dilute aqueous solutions and the membrane separating
                                       the phases  is  permeable  to all  species, the  species will  have the  same concentra-
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