Page 39 - Basic Structured Grid Generation
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28  Basic Structured Grid Generation

                                              ∂h i
                                   [ii, j]=−h i  j  ,
                                              ∂x
                                      j      h i  ∂h i
                                       =−           ,(i, j different, no summation over i)  (1.186)
                                      ii        2  j
                                            (h j ) ∂x
                                                    ∂h i
                                   [ij, i]= [ji, i]= h i  j  ,
                                                    ∂x
                                      i     i   1 ∂h i
                                       =    ji  =     ,(i, j different, no summation over i)  (1.187)
                                      ij
                                                h i ∂x j
                                                k
                                   [ij, k]= 0,    = 0,(i, j, k all different).            (1.188)
                                                ij
                                                   2 m
                                                               m
                                                            ij
                        Exercise 16. Use the identity ∇ x =−g   (see eqn (1.111)) to prove the identities
                                                              ij
                                  1 ∂     h 2 h 3        1 ∂     h 3 h 1         1 ∂     h 1 h 2
                            2                      2                       2
                          ∇ ξ = √              ,  ∇ η = √             ,  ∇ ς = √              .
                                   g ∂ξ   h 1             g ∂η   h 2             g ∂ς    h 3
                                                                                          (1.189)
                          Note that these formulas can be substituted directly into eqn (1.150) to obtain an
                                                  2
                        expression for the Laplacian ∇ φ of a general scalar field φ in an orthogonal curvilinear
                        co-ordinate system.
                        Exercise 17. Use eqn (1.189) together with eqn (1.114) to show that there is a rela-
                        tionship between the orthogonal curvilinear co-ordinates and cartesian co-ordinates y k ,
                        k = 1, 2, 3, given by

                           ∂     h 2 h 3 ∂y k     ∂     h 3 h 1 ∂y k     ∂     h 1 h 2 ∂y k
                                        +               +                = 0,  k = 1, 2, 3. (1.190)
                          ∂ξ    h 1 ∂ξ     ∂η   h 2 ∂η     ∂ς   h 3 ∂ς


                          More identities may be obtained from the vanishing of the six independent compo-
                        nents of the curvature tensor given by eqn (1.181). These are the six Lam´e Equations:
                                      ∂     1 ∂h k     ∂     1 ∂h j     1  ∂h j ∂h k
                                                  +              +              = 0,
                                                                           i
                                                                       2
                                     ∂x j  h j ∂x j  ∂x k  h k ∂x k  (h i ) ∂x ∂x i
                                                                           2
                                                 1 ∂h i ∂h j  1 ∂h i ∂h k  ∂ h i
                                                          +            −        = 0,      (1.191)
                                                                 k
                                                                           j
                                                     j
                                                h j ∂x ∂x k  h k ∂x ∂x j  ∂x ∂x k
                        where in each equation i, j, k must all be different and taken in the cyclic order 1, 2, 3.
                        So the three scale parameters must satisfy six compatibility equations.
                           1.11 Tangential and normal derivatives –
                                   an introduction

                        The rates of change of scalar functions in directions tangential to co-ordinate curves and
                        normal to co-ordinate surfaces are often needed in grid-generation work in connection
                        with the formulation of boundary conditions. These derivatives may be obtained by
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