Page 55 - Introduction to Computational Fluid Dynamics
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                                        MATERIAL  K 1    MATERIAL  K  2        1D HEAT CONDUCTION
                                                                         T
                                     i − 1       i       i  + 1           i       i  + 1/2    i + 1

                                                    i + 1/2
                            Figure 2.7. Interpolation of conductivity.

                            for example, may be evaluated in two ways:

                                     k i+1/2 = a + bT i+1/2 + cT 2  ,  T i+1/2 = 0.5(T i + T i+1 )  (2.52)
                                                             i+1/2
                            or

                                                  k i+1/2 = 0.5 [k (T i ) + k (T i+1 )] .      (2.53)
                               Both of these representations are pragmatically acceptable but neither can be
                            justified on the basis of the physics of conductance. To illustrate this point, let us
                            consider a composite medium consisting of two materials with constant conduc-
                            tivities k 1 and k 2 (see Figure 2.7). In this case, we lay the grid nodes i and i + 1
                            in such a way that the cell face i + 1/2 coincides with the location where the two
                            materials are joined. Thus, there is a discontinuity in conductivity at the i + 1/2
                            location.
                               Now, in spite of the discontinuity, the heat transfer Q i+1/2 on either side of
                            i + 1/2 must be the same. Therefore,

                                                             T i − T i+1/2
                                            Q i+1/2 = k 1 A i+1/2      ,     k 1 = k i ,       (2.54)
                                                              x i+1/2 − x i
                                                            T i+1/2 − T i+1
                                          Q i+1/2 = k 2 A i+1/2         ,    k 2 = k i+1 .     (2.55)
                                                            x i+1 − x i+1/2
                            Eliminating T i+1/2 from these equations gives
                                                                               −1

                                                     x i+1/2 − x i  x i+1 − x i+1/2
                                    Q i+1/2 = A i+1/2          +                  (T i − T i+1 ).  (2.56)
                                                         k i          k i+1
                               We recall, however, that our discretised equation was derived on the basis of
                            linear temperature variation between nodes i and i + 1 (see Equation 2.21). This
                            implies that

                                                         A
                                               Q i+1/2 =         k i+1/2 (T i − T i+1 ).       (2.57)
                                                         x
                                                            i+1/2
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