Page 138 - Introduction to Colloid and Surface Chemistry
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128  The solid—gas  interface


        Isotherm equations

        Numerous  attempts  have  been  made  at  developing  mathematical
        expressions from  postulated adsorption  mechanisms to fit the  various
        experimental  isotherm  curves.  The  three  isotherm  equations  which
        are  most  frequently used  are those due to Langmuir, to Freundlich,
        and  to  Brunauer,  Emmett  and Teller (BET).

         The Langmuir  adsorption  isotherm

        Before  1916,  adsorption theories postulated either a condensed liquid
        film  or a compressed gaseous layer which decreases in density as the
        distance  from  the  surface  increases.  Langmuir  (1916)  was  of  the
        opinion that, because  of the rapidity with which intermolecular forces
        fall  off with distance,  adsorbed  layers are  not  likely to  be more than
        one  molecular layer in thickness.' This  view is generally accepted  for
        chemisorption  and  for  physical  adsorption  at  low  pressures  and
        moderately  high  temperatures.
          The  Langmuir  adsorption  isotherm  is based  on  the  characteristic
        assumptions  that  (a) only monomolecular adsorption takes place,  (b)
        adsorption  is localised  and  (c) the  heat of adsorption  is  independent
        of  surface  coverage.  A  kinetic  derivation  follows  in  which  the
        velocities  of adsorption  and  desorption  are  equated  with  each  other
        to  give an expression  representing adsorption  equilibrium.
          Let  V equal the equilibrium volume of gas adsorbed  per unit  mass
        of adsorbent  at a pressure p and V m equal the volume of gas required
        to  cover  unit mass  of adsorbent  with  a complete  monolayer.
          The  velocity  of  adsorption  depends on:  (a)  the  rate  at  which  gas
        molecules  collide  with the  solid  surface, which is proportional  to  the
        pressure;  (b)  the  probability of striking a vacant site  (1 — V/V m);  and
        (c) an activation term exp  [—E/RT],  where E is the activation energy
        for  adsorption.
          The  velocity  of  desorption  depends  on:  (a)  the  fraction  of
        the  surface  which  is  covered,  V/V m;  and  (b)  an  activation  term
        exp  [—E'/RT\,  where  E'  is the  activation energy for  desorption.
          Therefore,  when adsorption  equilibrium is established,



                ~ VI  V m )exp[-E / RT] = k(V I V m )exp[-£' / RT]
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