Page 219 - Introduction to Colloid and Surface Chemistry
P. 219

208  Charged  interfaces

                 epA£
             / s =-^                                           (7.29)
                  7)/
        where A  is the  cross-sectional  area  of the  capillary.
          The  streaming current and  the  streaming potential are related by
         Ohm's law,
                  JJ_
             E  =
               S
                  M
        where fc () is the  conductivity of the  electrolyte solution. Therefore,
                  ep£
             E s =-^                                           (7.30)
                  rjk 0
          k 0  can  be  corrected  to  include a surface conductivity term  & s and
        equation  (7.30)  becomes






          A  more  general  derivation 90  for  porous  plugs  also  leads  to
        equations  (7.29)  and  (7.30).  However,  for porous  plugs, there  is no
        satisfactory  method  of correcting  streaming potential  data for surface
        conductance.  If equation  (7.31)  is used  with  a equal to  the  average
        pore  radius,  the  calculated  zeta  potentials  are  too  low.  The
        importance  of surface  conductance  can  be  investigated  qualitatively
        by  comparing  the  conductivity  ratio  of  two  relevant  electrolyte
        concentrations  in  bulk  and  in the  plug. A  knowledge of the surface
        conductance  is not  required  when  relating streaming current  to zeta
        potential.  The  situation in porous  plugs may also be more complicated
        than  accounted  for  above if (a)  the  effective  area  of the  plug for  the
        streaming current differs  from  that for the  leak current as a result of
        the  different mechanisms  involved,  and  (b)  the  plug is compressible
        and the  applied pressure  affects  the average pore size. The validity of
        all  zeta  potentials  calculated  from  streaming (and  electro-osmotic)
        measurements  on  porous plugs is somewhat  dubious.
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