Page 282 - Numerical Methods for Chemical Engineering
P. 282

Finite differences for a convection/diffusion equation              271



                       1
                               e  1
                               e  1
                               e  1
                              e  1


                    ϕ

                                                 increasin e


                     2
                     1

                               2                                 1

                  Figure 6.6 Analytical solution of a 1-D convection/diffusion equation at various Peclet numbers.


                  is dominant, and the flow (which is from left to right) “pushes” the incoming fluid at z = 0
                  downwind to the right and causes a sharp increase in ϕ near the exit outflow at z = 1.


                  Central difference scheme (CDS)

                  To solve this problem numerically, we apply the finite difference method for a grid of points,
                  0 < z 1 < z 2 <···< z N < L, and require the differential equation to be satisfied locally at
                  each point,
                                                         2

                                              dϕ        d ϕ
                                           − v      +         = 0                    (6.74)
                                               dz       dz 2
                                                  z j       z j
                  For simplicity, we place the grid points uniformly with  z = L/(N + 1), z j = j( z). For
                  the second derivative, we have the approximation
                                           2
                                          d ϕ     ϕ j−1 − 2ϕ j + ϕ j+1
                                                 ≈                                   (6.75)
                                          dz  2         ( z) 2
                                              z j
                  For the first derivative, we consider two alternatives. In the CDS, we choose the more
                  accurate approximation
                                            (CDS)
                                       dϕ        ϕ j+1 − ϕ j−1      2
                                               =            + O[( z) ]               (6.76)
                                       dz          2( z)
                                          z j
                  which yields the linear equation for grid point j,

                                      ϕ j+1 − ϕ j−1   ϕ j−1 − 2ϕ j + ϕ j+1
                                 − v             +                      = 0          (6.77)
                                        2( z)               ( z) 2
                                     2
                  We multiply by −2( z) /  to obtain
                                  v( z)
                                       [ϕ j+1 − ϕ j−1 ] − 2ϕ j−1 + 4ϕ j − 2ϕ j+1 = 0  (6.78)
   277   278   279   280   281   282   283   284   285   286   287