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8.3 Two-Phase System with  a  Membrane  Permeable  by a Single Ion   145


         tions in the two phases, and an equilibrium  relation  of the form

                                                                         (8.2-9)


         will be satisfied in each phase  and in the system  as a whole.


            8.3  TWO-PHASE SYSTEM WITH A  MEMBRANE
                  PERMEABLE BY  A SINGLE ION

         When  two  different phases  are separated  by  a membrane  permeable  by  a single
         ion  and  that  ion  has  different  activities  on  the  two  sides  of  the membrane,  an
         electric potential difference will be set up at equilibrium  (Alberty, 1995a, d, 1997).
         We first consider a two-phase system with an aqueous solution of a single salt on
         both sides of  a membrane  that is permeable  only to cation C. When electrolytes
         are involved, it is  necessary  that counterions be  present  because bulk phases are
         electrically  neutral.  When  cation  C  diffuses  through  the  membrane  into  the  fi
         phase,  the  fi  phase  becomes  positively  charged  with  respect  to  the  a  phase.
         Diffusion  stops  when  a  sufficient difference in  electric potential  has  been  estab-
         lished. When  a conductor is charged, the charge migrates  to the surface, and for
         an aqueous  solution  of  a  salt  this  occurs in the charge relaxation time of  about
         one nanosecond. Thus a positively  charged layer is  formed  at the surface of  the
         membrane  toward the fi  phase  and a negatively  charged  layer is formed  at the
         surface of  the membrane  toward  the  2 phase. The thickness  of  the layer in each
         aqueous  phase is the Debye length of  about  1 nm  at an ionic strength of  0.1 M.
         The amount of charge required to set up a significant potential difference between
         the phases is very small. Many biological membranes have capacitances of about
         one  microfarad  per  square  centimeter  (Weiss,  1996). The  charge  transfer  per
         square centimeter  required  to set  up a  potential  difference of  0.1  V  is  therefore
               mol of  singly charged ions. As the electric potential of the fi phase increases
         due to the diffusion of cation C, the process of diffusion slows and an equilibrium
         potential  difference is reached.
             The fundamental  equations  for  G for the phases  on either  side of  the center
         of the membrane  are
                          dG,  = - S,dT+  V,dP + ,ucadnC, + +,dQ,        (8.3-1)

                          dG,  = - S,dT+  5dP + p,,dn,,  + +,dQB         (8.3 -2)
         where n,,  is the amount of cation C in the a phase and Q is the amount of charge
         transferred  across  the  center  of  the  membrane.  No  term  is  included  for  the
         monovalent anion A  because its concentration  in the bulk phase is equal to that
         of  the monovalent  cation C. Since dnAa = dnCa, the inclusion  of  a term  for A in
         equation  8.3-1 would yield (pC, + ,uAn)dnCa. However, since the chemical potential
         can be defined for an arbitrary reference potential (cf, AfGP), ,uAor can be set equal
         to zero.
             Since  -dQ,  = dQ,  = dQ, the fundamental equation for G for this two-phase
         system  prior  to  the  establishment  of  phase  equilibrium  is  the  sum  of  equation
         8.3-1 and 8.3-2:

                    dG = - SdT+ VdP + ,uCndnCa + ,u,,dn,,  + ($,  - 4,)dQ   (8.3-3)
         There is difference in electric potential across the membrane. So there is an electric
         field in the membrane, but there are no electric fields in the two bulk phases. The
         electrical work required  to move charge dQ across the center of the membrane is
          (&   ~  4,)dQ.  The polarization  of  the membrane does not change in this  process
          of  charge  transport  because  the  potential  difference  is  constant.  Since
          dnC, = - dn,,,  equation  8.3-3 can  be  used  to  show  that  at  phase  equilibrium,
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