Page 113 - Adsorption by Powders and Porous Solids
P. 113

98                            ADSORPTION  BY POWDERS AND POROUS SOLIDS

   Here the pre-exponential factor, K, is equal to the ratio of the adsorption and desorp
   tion coefficients, alp. Alternatively, b may be regarded as a function of the enthalpy
   and entropy of  adsorption (Everett, 1950; Barrer, 1978, p. 117).
     In his early treatment, Langmuir assumed that the energy of adsorption for the first
   layer is generally considerably larger than  for the  second  and  higher layers, and
   therefore multilayer formation is possible only at much greater pressures than the
   pressure required for monolayer completion. Thus, the formation of second or higher
   layers would be indicated by the appearance of a discontinuous isotherm. In fact, this
   situation does arise in the case of a stepwise, Type VI, isotherm. However, the lateral
   adsorbate-adsorbate  interactions,  which  are  associated with  all known  stepwise
   isotherms, are not compatible with the Langmuir model.
     It is evident that Equation (4.1 1) is of  a very  general mathematical form (i.e. a
   hyperbolic function). At low 0 it reduces to Henry's law; at high surface coverage, a
   plateau  is reached  as 0+  1. Other equations  of  the  same mathematical form as
   Equation  (4.1 1) have  been  derived  from  a  classical  thermodynamic  standpoint
   (Brunauer,  1945) and  by  application  of  the  principles of  statistical  mechanics
   (Fowler, 1935).
     Equation (4.1 1) is usually applied in the linear form

                            pin = 11% b +pin,                    (4.13)
   where n is the specific amount of gas adsorbed at the equilibrium pressure p and n,
   is the monolayer capacity (as before, 8 = n/n,).
     Many systems give linear plots of pin against p over a limited ranges of pressure,
   but such linearity does not by itself imply conformity with the Langmuir model. As
   already indicated, a second condition is that the energy of adsorption should be inde-
   pendent of  surface coverage. Thirdly, the differential entropy of adsorption should
   vary  in  accordance with  the  ideal localized model (Everett, 1950). That  no  real
   system has been found to satisfy all these requirements is not surprising in view of
   the complexities noted here and in subsequent chapters.
     Various attempts have been made to modify the Langmuir model. One of the best
   known is that  of  Fowler and Guggenheim  (1939), which  allowed for adsorbate-
   adsorbate interactions in a localized monolayer on a uniform surface. However, on an
   empirical basis the Fowler-Guggenheim  equation turns out to be no more successful
   than  the  original Langmuir isotherm.  The highly  complex  problem  of  localized
   adsorption on heterogeneous surfaces has been discussed by Rudzinski and Everea
   (1992).


   4.2.4.  The Brunauer-Emmett-Teller  (BET) theory
   By introducing a number of simplifying assumptions, Brunauer, Emmett and Teller
   (1938) were able to extend the Langmuir mechanism to multilayer adsorption and
   obtain an isotherm equation (the BET equation), which has Type I1  character. The
   original BET treatment  involved  an extension of  the Langmuir kinetic  theory of
   monomolecular adsorption to the formation of an infinite number of adsorbed layers.
     According to  the  BET model, the  adsorbed molecules  in  one  layer can act as
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