Page 35 - Introduction to Colloid and Surface Chemistry
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26  Kinetic properties

        Table 2.1  Diffusion  coefficients  and  Brownian displacements calculated  for uncharged
        spheres in water at  20°C

        Radius               D 2o°c/ m2s 1           He  after  I  h
                                     ~
                                                       3
         10~ 9  m  (1  nm)   2.1  x  10~ 10    1.23  x  10~  m (1.23  mm)
                                                       4
           8
         10~  m (10  nm)     2.1  x  10~  n   3.90  x  10~  m  (390  jim)
           7
                                                       4
         Hr rn(100nm)        2.1  x  10-  12  1.23  x  10~  m  (123  pm)
                                                       5
        10~ 6  (1  fxm)      2.1  x  KT 13    3.90  x  10~  m  (39  jutn)
                                                         23
        yielded  values  of N A  closer  to  the  accepted  6.02  x  10  mol  *;  for
                                                        23    1
        example,  Svedberg  (1911) calculated N A  =  6.09  x  10  moP  from
        observations  on monodispersed gold sols of known particle size in the
        ultramicroscope.  The  correct  determination  of Avogadro's  constant
        from  observations  on Brownian  motion  provides striking evidence  in
        favour  of .the  kinetic  theory
          As  a  icsult  of  Brownian  motion,  continual  fluctuations  of
        concentration  take  place  on  a molecular  or  small-particle  scale.  For
        this  reason,  the  second  law  of  thermodynamics is only valid  on  the
        macroscopic  scale.

        Translational diffusion

        Diffusion  is the  tendency  for  molecules  to  migrate  from  a  region  of
        high  concentration  to  a region  of lower concentration  and  is a  direct
        result  of  Brownian  motion.
          Pick's  first  law  of  diffusion  (analogous  with  the  equation  of  heat
        conduction)  states  that  the  mass  of  substance  dm  diffusing  in  the  x
        direction  in  a  time  At  across  an  area  A  is  proportional  to  the
        concentration  gradient  dc/dx  at  the  plane  in question:
                      dc
             dm = -DA—dt                                        (2.8) /
                      ,
                                                                \
                      dx
        (The  minus sign denotes that diffusion  takes place in the direction of
        decreasing  concentration.)
          The  rate  of change  of concentration  at  any given point  is given by
        an  exactly equivalent expression,  Pick's second  law:
                    2
             dc    d c
               = D   r-                                         (2  Q)
                                                                 -
             dt    dx 2                                        lz v;
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