Page 284 - Introduction to Colloid and Surface Chemistry
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Emulsions  and foams  273

        affect  the equilibrium film thickness that a balance between the above
        forces  would  otherwise  determine.
          Experimental  studies  on  non-draining,  horizontal  liquid films in
        which the equilibrium film thickness is measured  as a function of ionic
        strength  and  applied  hydrostatic  pressure  (or  suction)  provides  a
                                            98 225 226
        means  of  investigating the  above forces '  "  .  Figure  10.3  shows
        an apparatus  used  by Deryagin and Titijevskaya 225 .  A flat liquid film
                             2
        with an  area  of c.  I  mm  is formed between cups A  and B which are
        connected  via tube  C to  equalise  bubble  pressures.  The  pressure  in
        the  bubbles in excess  of that  in the  liquid film is calculated  from  the
        manometer  reading  A/z.  Deryagin  called  this  excess  pressure  the
        disjoining  pressure.  An elaborate  optical  device (not shown) permits
        measurement  of the film thickness.











        Ah T"
           JE»  —  «"






        Figure  10.3  Apparatus for  measuring the  disjoining pressure  of  free  films  as  a
                           225
        function  of their  thickness  (After  B.V. Deryagin and A.S. Titijevskaya)

          Figure  10.4 shows  the  results of  some  measurements  on  aqueous
        sodium oleate  films.  The sensitivity of  the equilibrium film thickness
        to  added  electrolyte  reflects  qualitatively  the  expected  positive
        contribution  of  electric  double  layer  repulsion  to  the  disjoining
        pressure.  However,  this sensitivity to  added  electrolyte  is much less
        than  that  predicted  from  electric  double  layer  theory  and  at  high
        electrolyte  concentration  an equilibrium film thickness of c.  12 nm is
        attained  which  is  almost  independent  of  the  magnitude  of  the
        disjoining  pressure.  To  account  for  this observation,  Deryagin and
        Titijevskaya  have  postulated  the  existence  of  hydration  layers
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