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212  Chapter 8: Catalysis and Catalytic Reactions

                             The result for  ATP,,,, contained in equation 8.540 can be obtained from the follow-
                           ing energy balance for a control surface or a core of radius  Y:

                                           rate of thermal conduction across control surface
                                         = rate of enthalpy consumption/generation within core
                                       = rate of diffusion of A across control surface X (-AH&  (8.5-41)

                           That is, from Fourier’s and Fick’s laws,

                                                                                              (8.542)


                           Integration of equation 8.5-42 from the center of the particle (r  = 0, T =  T,, cA  =
                           cAO) to the surface  (r =  R, T = T,, CA  = c&,  with  k,, D,, and (-AURA)  constant, re-
                           sults in


                                              ATp =  T,  -  To  =  D,(-AHRA)  (cAs   - CAo)   (8.5-43)
                                                                  k
                                                                   e
                           or, with CA0 + 0,and AT,, -+ AT,,,,,

                                                     qvnlzx =  D~(-AHRA)CA~
                                                                    k
                           as used in equation 8.5-40.
                             Some of the results of Weisz and Hicks (1962) are shown in Figure 8.12 for  y  = 20,
                           with  n  as a function of  4  and  p  (as a parameter). Figure 8.12 confirms the conclusions
                           reached qualitatively above. Thus,  vex0  (p 3 0) > qisorh (/3 =’ 0), and  vex0  > 1 for rel-
                           atively high values of p  and a sufficiently low value of 4; nendO < visorh  <  1. At high
                           values of /?  and low values of 4,  there is the unusual phenomenon of three solutions
                           for  n  for a given value of p  and of  4;  of these, the high and low values represent stable
                           steady-state solutions, and the intermediate value represents an unstable solution. The
                           region in which this occurs is rarely encountered. Some values of the parameters are
                           given by HlavaCek  and  KubiCek  (1970).


      8.56   Overall Effectiveness Factor  q0
                           The particle effectiveness factor n defined by equation 8.5-5 takes into account con-
                           centration and temperature gradients within the particle, but neglects any gradients
                           from bulk fluid to the exterior surface of the particle. The overall effectiveness factor
                           q0  takes both into account, and is defined by reference to bulk gas conditions  (c&,   T,)
                           rather than conditions at the exterior of the particle  (c,,+  T,):


                                                   q. = t-A(ObSH-Ved)/?-,(C~g,  Tg)          (8.5-45)


                           Here, as in Section 8.5.4, we treat the isothermal case for  r),,  and relate r10  to  7.  no  may
                           then be interpreted as the ratio of the (observed) rate of reaction with pore diffusion
                           and external mass transfer resistance to the rate with neither of these present.
                             We first relate  no to q,  kA,  and kAs, the last two characterizing surface reaction and
                           mass transfer, respectively; mass transfer occurs across the gas film indicated in Figure
                           8.9. Consider a first-order surface reaction. If (-rA)  is the observed rate of reaction,
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