Page 72 - Pressure Swing Adsorption
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i.  I
 46   PRESSURE SWING ADSORPTION   FUNDAMENTALS OF ADSORPTION           47

 10-2~-----------,







 10- 3
                     10·6

                  -
                  <11
                  N
                  E
                   u
 N : E:6.5 kcal/mole   o'
 2


                      10· 1
 10-5'--...!---'----'----'--'
 10   3.2   3.4   3.6
 10; IT  (K"')
 (a)
 Figure  2.18  Arrhenms  piot  showing  t11e  temperature  dependence  of  m1cropore
 diffus1vities  for  (a)  0  2   and  N 2   in  Bergbau  carbon  molecular  s1eves 35   and  (b)  for
 several light gases in  5A and 13X zeolite crystals. 50   3
                                     10 /T  (K"l
                                          (b)
                                Figure 2.18  (Contmued).
 which has the same form  as Eq.  2.38a with  the  effective diffus1v1ty  given  by:

            2.3.8  Heat Transfer Control
 (2.44a)
          Since adsorption or ctesorot1on  1s  generally associateQ  with  a s1gnificam  heat
          effect  (exothermic  for  adsorotion),  sorption/desorot10n  rates  may  be  influ-
 The sorptlon curve 1s  then of the same form as Eu. 2.38a but with  D replaced   enced  or even  controlled  by  the  rate  of heat  dissipation.  Such  effects  have
 by D~  and  r  replaced by  Rr. Since  K  vanes with  temperature  m  accordance   heen  mvest1gated  both  theoretically  and  expcnmentally.  45 4
                                                          · ri  In  the  limitmg
 with  Eq.  2.38b,  the  uptake  behavior  gives  the  appearance  of an  activated
          situation  in  which  all  mass  transfer  processes  are  rapid,  the  sorpt1on  rate  1s
 diffusion  process  with  £  ~ -6.H.  The  case  of  a  nonlinear  eauilibrium
          controlled  entirely  by  the  rate of heat dissmation,  and  the  sorpt1on/desoro-
 relationship 1s  more complex and corresoonds formally with a concentrat1on-
          tion curve assumes a very  s1mpie  form:
 cteoendent effective difl'us1v1ty  given  by:
               m.         B      I   ha   t   \
                    1
               m:  ~  - l  + B exp l - C,  (1  + B)  j              (2.45)
 (2.44b)
          The  exoenmental  adsorot1on/desorpt1on  curves  for  carbon  dioxide  m  5A
          zeolite  crystals,  presented  m  Figure  2.19,  conform  to  this  s1moie  model.  As
 where f'(c)  represents  the slope of the equilibnum isotherm (dq* /de).   with the diffusion or surface resistance mass transfer models, the approach to
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