Page 46 - Introduction to Colloid and Surface Chemistry
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Kinetic properties  37

        where  dc/d*'  is the  concentration  gradient  at  the  meniscus,  c'  the
        concentration  at  the  meniscus  and  x'  the  distance  of  the  meniscus
        from  the axis of  rotation.

        Charge  effects

        The  treatment  of  sedimentation  and  diffusion  is  a  little  more
        complicated  when the particles under consideration  are charged.  The
        smaller counter-ions  (see Chapter  7) tend to sediment  at a slower rate
        and lag behind the sedimenting colloidal  particles.  A potential  is thus
        set  up  which  tends  to  restore  the  original  condition  of  overall
        electrical  neutrality  by  accelerating  the  motion  of  the  counter-ions
        and  retarding the  motion  of the  colloidal  particles.
          The reverse  situation applies to diffusion.  The smaller counter-ions
        tend to diffuse  faster than the colloidal particles and drag the  particles
        along with them  and  increase  their  rate  of  diffusion.
          These  effects  can be overcome  by employing swamping electrolyte
        concentrations.  Any potentials  which might develop  are then readily
        dissipated by a very small displacement of a large number of counter-
        ions.



        Osmotic pressure

        The  measurement  of  a  colligative  property  (i.e. lowering of vapour
        pressure,  depression  of  freezing  point,  elevation  of  boiling point  or
        osmotic  pressure)  is  a  standard  procedure  for  determining  the
        relative molecular mass of a dissolved substance.  Of these  properties,
        osmotic  pressure  is the only one with a practical value in the study of
        macromolecules.  Consider,  for  example,  a  solution  of  1  g  of
        macromolecular material of relative molecular mass 50 000 dissolved
                 3
        in  100 cm  of  water.  Assuming ideal  behaviour,  the  depression  of
        freezing  point would be 0.0004  K and the  osmotic  pressure  (at  25°C)
                         2
        would be 500 Nm~  (i.e. 5 cm water). This freezing point depression
        would  be  far  too  small  "to be  measured  with  sufficient  accuracy  by
        conventional methods and, even more important, it would be far too
        sensitive to small amounts of low relative molecular mass impurity; in
        fact,  it would be doubled by the  presence  of just  1 mg of impurity of
        relative molecular mass 50. Not only does osmotic pressure provide a
        measurable  effect,  but  also  the  effect  of  any  low relative molecular
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