Page 70 - Adsorption Technology & Design, Elsevier (1998)
P. 70

Rates of adsorption of gases and vapours by porous media  67


            per unit time. If M is the molecular mass of the gas in question, p its pressure
            and  T the absolute temperature, the rate (measured in kg m -2 s -1) at which
            molecules strike the surface may be expressed as

                                                                        (4.1)
              Rm  "" p( M/2trRg T) '/~
            We compare the intrinsic rate of adsorption of nitrogen with an experiment-
            ally observed rate of adsorption of nitrogen at 6 bar and 25~  (Crittenden et
            al.  1995). Appropriate  substitution  of numerical values into equation  (4.1)
            gives the maximum intrinsic rate of adsorption as 2 x  10 4 kg  m -2 s -1. On the
            other  hand,  the  experimentally  observed  rate  is  approximately  4  x
            10 -8 kg m -2 s -1  (c.  0.33 mol s -l  at 6 bar, 25~  onto  a surface  of 250 m E g-l).
            Thus  the  intrinsic  rate  of  adsorption  is  some  1012  times  faster  than  the
            observed  rate  of adsorption.  It  is generally  acknowledged  throughout  the
            literature on physical adsorption processes that the dominant rate-control-
            ling  step  is  not  the  actual  physical  attachment  of  adsorbate  to  adsorbent
            (normally referred to as very rapid) but rather intraparticle transport of gas
            within  the  porous  structure  of  the  adsorbent  to  its  available  surface.
            Interparticle transport from bulk fluid to the external surface of the porous
            adsorbent  may also have  an effect on the  overall rate  of adsorption  under
            some circumstances.
              Transport resistances which influence the overall rate of adsorption are:

                (1)  mass and heat transfer of adsorbate to and from the exterior surface
                   of the adsorbent (known as interparticle transport);
                (2)  Maxwellian  diffusion  (bulk  molecular  diffusion)  in  moderately
                   large  pores  (macropores)  or  Knudsen  diffusion  in  pores  (micro-
                   pores) which have a diameter smaller than the mean free path of the
                   adsorbate molecules;
                (3)  intracrystalline diffusion within the channel and cage-like structure
                   of molecular sieve materials such as zeolites and silicalites;
                (4)  surface  diffusion  when  adsorbate  molecules  move freely over the
                   internal  surface  of  adsorbents  in  parallel  with  intraparticle  diffu-
                   sion;
                (5)  heat  transfer  within  the  interior  of  particles  occasioned  by  the
                   exothermic nature of adsorption.


            The relative importance of these resistances largely depends on the nature of
            the adsorbent and adsorbate and the conditions of temperature and pressure
            in  which  the  adsorption  occurs.  As  shown  in  Chapter  6  any  model
            representing an adsorber must include mass and heat balances for the fluid
            phase and also transport processes within the porous particles.
   65   66   67   68   69   70   71   72   73   74   75