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230  Chapter 9: Multiphase Reacting Systems

                            “blurring” is significant, a more general model (Section 9.1.2.2) may have to be used.
                            The SCM differs from a general model in one important aspect, as a consequence of
                            the sharp boundary. According to the SCM, the three processes involving mass transfer
                            of A, diffusion of A, and reaction of A with B at the surface of the core are in series.
                            In the general case, mass transfer is in series with the other two, but these last two
                            are not in series with each other-they occur together throughout the particle in some
                            manner. This, together with a further assumption about the relative rates of diffusion
                            and movement of the reaction surface, allows considerable simplification of the solution
                            of equation 9.1-5. This is achieved in analytical form for a spherical particle in Example
                            9-1. Results for other shapes can also be obtained, and are explored in problems at the
                            end of this chapter. The results are summarized in Section 9.1.2.3.2.
                              In Figure 9.2,  c.+ is the (gas-phase) concentration of A in the bulk gas surrounding
                            the particle,  cAs  that at the exterior surface of the particle, and  cAc  that at the surface of
                            the unreacted core of B in the interior of the particle; R is the (constant) radius of the
                            particle and rC is the (variable) radius of the unreacted core. The concentrations CA8
                            and  cAs are constant, but cAc decreases as t increases, as does r,, with corresponding
                            consequences for the positions of the profiles for  cn, on the left in Figure 9.2(a)  and (b),
                            and cA, on the right.






                            For a spherical particle of species B of radius  R  undergoing reaction with gaseous species
                            A according to 9. l-l, derive a relationship to determine the time t required to reach a
                            fraction of B converted,  fn,  according to the SCM. Assume the reaction is a first-order
                             surface  reaction.


       SOLUTION

                             To obtain the desired result,  t  =  t(fB),  we could proceed in either of two ways. In one,
                             since the three rate processes involved are in series, we could treat each separately and add
                             the results to obtain a total time. In the other, we could solve the simplified form of equation
                             9.1-5 for all three processes together to give one result, which would also demonstrate the
                             additivity of the individual three results. In this example, we use the second approach (the
                             first, which is simpler, is used for various shapes in the next example and in problems at
                             the end of the chapter).
                               The basis for the analysis using the SCM is illustrated in Figure 9.3. The gas film,
                             outer product (ash) layer, and unreacted core of B are three distinct regions. We derive the
                             continuity equation for A by means of a material balance across a thin spherical shell in
                             the ash layer at radial position Y  and with a thickness dr. The procedure is the same as that
                             leading up to equation 9.1-5,  except  that there is no reaction term involving  (-   r,&  since
                             no reaction occurs in the ash layer. The result corresponding to equation 9.1-5 is


                                                                                               (9.1-17)


                               Equation 9.1-17 is the continuity equation for unsteady-state diffusion of A through the
                             ash layer; it iS unsteady-state because  CA  = cA(r,   t). To simplify its treatment further, we
                             assume that the (changing) concentration gradient for A through the ash layer is established
                             rapidly relative to movement of the reaction surface (of the core). This means that for an
                             instantaneous “snapshot,” as depicted in Figure 9.3, we may treat the diffusion as  steady-
                             state diffusion for a fixed value of r,y i.e.,  CA  = CA(r).  The partial differential equation,
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