Page 93 - Introduction to Colloid and Surface Chemistry
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Liquid-gas and liquid-liquid  interfaces  83

          The  Gibbs equation in this form could be applied to a solution of a
        non-ionic  surfactant.  For  a  solution  of  an  ionic  surfactant  in  the
                                                            3 151
        absence  of  any other  electrolyte,  Haydon  and  co-workers '   have
        argued that equations (4.20) and  (4.21) should be  modified  to  allow
        for  the  fact that both the anions and the cations of the  surfactant  will
        adsorb  at  the  solution  surface  in  order  to  maintain  local  electrical
        neutrality (even though not  all of these ions are surface-active in the
        amphiphilic sense). For a solution of a 1:1 ionic surfactant a factor of
        2 is required to allow for this simultaneous adsorption of cations and
        anions,  and  equation (4.21) must be  modified  to


             p  _   @_   j_                                    it  -y)\
             i  _                                              ^4,ZZJ
                  2RT  dc B
         In  the  presence  of  excess  inert  electrolyte,  however,  an  electrical
        shielding  effect  will operate  and  equation (4.21) will apply.

         Experimental verification of the Gibbs equation

        The  general  form  of  the  Gibbs  equation  (dy  =  —2  F/d/i,,)  is
        fundamental  to  all  adsorption  processes.  However,  experimental
        verification of the equation derived for simple systems is of interest in
        view  of  the  postulation  which  was made concerning the  location of
        the boundary surface.
          McBain  and  Swain 152  succeeded  in  verifying  the  validity of  the
        Gibbs equation  by means of a very direct and ingenious experiment.
        Surface layers of about 0.1 mm thickness were shaved off solutions of
        surface-active  materials,  such  as  phenol  and  hydrocinnamic  acid,
        contained  in a long rectangular trough, by means of a rapidly moving
        microtome  blade.  The  material  collected  was analysed  and  experi-
        mental surface excess  concentrations  were calculated. These  compared
        well with the corresponding  surface excess concentrations calculated
        from  surface tension  data.
                                                                47
          Surface  concentrations  have also  been  successfully measured  by
        labelling  the  solute  with  a  ^-emitting  radioactive  isotope  (e.g.
        3  14   35    45
         H, C,   S  or  Ca)  and  measuring  the  radiation  picked  up  by a
        Geiger counter placed  immediately above the surface of the solution.
        As  /8-rays  are  rapidly  attenuated  in  the  solution,  the  measured
        radiation  corresponds  to the  surface  region  plus only a thin  layer of
        bulk  region.  Direct  measurement  of  surface  concentrations  is
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