Page 125 - Adsorption by Powders and Porous Solids
P. 125

110                           ADSORPTION BY POWDERS AND POROUS SO~D~

   Langmuir equation contains the two disposable constants, n,  and b, which cannoth
   evaluated by  any independent method.
     It is now generally accepted that there is no sound reason why isotherms on micra.
   porous solids should conform any more closely to the classical Langmuir mechanism
   than  isotherms on non-porous  or mesoporous  adsorbents. Indeed,  a considerable
   amount of the evidence now available gives strong support to the view that the limit.
   ing uptake is controlled rather by the accessible micropore volume than by the inter,
   nal surface area (Gregg and Sing, 1982).
     In the context of gas separation (see Yang, 1987) or for some other purposes, it
   may be expedient to apply an equation of  the Langmuir form; but we consider it
   advisable to treat this as empirical relation. Thus, we may write




   where the parameters n, and b are to be regarded as empirical constants within stated
   ranges of p and T.
     We have concluded that the limiting uptake at the plateau of a Type I isotherm is
   not  directly related  to  the surface area. However, it  is now appropriate to return
   briefly to the initial stage of  physisorption by  microporous solids and consider the
   question: does monolayer adsorption ever precede micropore filling ?
     Some time ago Brunauer (1970) argued that monolayer adsorption of nitrogen and
   other  small molecules does  occur  on  the  walls  of  micropores  wider  than  about
   0.7 nm. Although as we have seen, Brunauer's original theory is now questionable,
   some recent evidence does support his view that monolayer adsorption can take place
   on the walls  of  the wider  micropores before secondary micropore filling occurs.
   These aspects are discussed in later chapters.

   4.4.4.  The Dubinin-Stoeckli  theory

   Dubinin was the pioneer of the concept of micropore filling. His approach was based
   on the early potential theory of  Polanyi, in which the physisorption isotherm data
   were expressed in the form of a temperature-invariant 'characteristic curve'.
     In 1947 Dubinin and Radushkevich put forward an equation for the characteristic
   curve in terms of the fractional filling, W/W,,  of the micropore volume, W,. This rela-
   tion is usually expressed in the form
                           W/W, = exp [ - (A/EI2I                (4.39)
   where A, the Polanyi 'adsorption potential',  is an adsorption affinity,
                             A = -RT  In (p/pO)                  (4.40)
   and E is a characteristic energy for the given system.
     The isotherm equation is obtained by combining Equations (4.39) and (4.40). With
   the introduction of a scaling factor, j3, it becomes
                     ~1% exp{ - [RT In (pO/p)l   BE,)^ I         (4.41)
                          =
   where Eo is a 'characteristic energy'.
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