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Modeling a tubular chemical reactor with dispersion                 279



                            cte cncentratins   c (z)
                                              j
                  inet        A + B → C  r R1  = k c c  tet
                                            1 A B
                              C + B → D  r R2  = k c c
                                            2 B C
                     z = 0                          z = L
                  Figure 6.10 Tubular chemical reactor with dispersion.

                                    2
                  Parabolic equations, b − 4ac = 0
                  Here, there exists only one real characteristic line. Consider the time-varying 1-D diffusion
                  equation
                                                         2
                                                 ∂ϕ     ∂ ϕ
                                                    =                               (6.114)
                                                 ∂t     ∂z 2
                                                2
                  that, with a = 0, b = 0, c =   has b − 4ac = 0. The slope of the single characteristic
                  line is indeterminate as a = 0, and thus corresponds to a vertical line running through P in
                  the space-time diagram. Therefore, we find that each point P influences all points in space
                  at all future times, and is influenced in turn by the field values at all spatial positions at all
                  past times. Past numerical errors therefore are smoothed out with increasing time.


                  Modeling a tubular chemical reactor with dispersion; treating
                  multiple fields

                  Many problems of interest involve multiple fields, each with its own governing equation.
                  Consider a tubular chemical reactor of length L (Figure 6.10) with the reactions A + B → C
                  and B + C → D.AfluidmediumcomprisinginitiallyonlyAandBflowsthroughthereactor
                  with a mean axial velocity v z . In addition to convection, we also have a diffusive-like mixing,
                  known as dispersion, due to the coupling of diffusion to inhomogeneities in the velocity
                  field. We employ a common dispersion coefficient D as an effective axial diffusivity for
                  each species. Dispersion is usually of minor importance compared with convection, with
                  high values observed for the Peclet number
                                                       v z L
                                                  Pe =                              (6.115)
                                                        D
                    The concentration fields of A, B, C, and D at steady state are governed by the coupled
                  set of PDEs
                                                        2
                                      ∂c A      ∂c A   ∂ c A
                                          =− v z    + D     − k 1 c A c B = 0
                                       ∂t       ∂z      ∂z 2
                                                    2
                                  ∂c B      ∂c B   ∂ c B
                                      =− v z   + D    2  − k 1 c A c B − k 2 c B c C = 0
                                   ∂t       ∂z      ∂z
                                                                                    (6.116)
                                                    2
                                  ∂c C      ∂c C   ∂ c C
                                      =− v z   + D      + k 1 c A c B − k 2 c B c C = 0
                                   ∂t       ∂z      ∂z 2
                                                            2
                                          ∂c D      ∂c D   ∂ c D
                                              =− v z   + D    2  + k 2 c B c C = 0
                                           ∂t       ∂z      ∂z
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