Page 158 - Basic Structured Grid Generation
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Differential models for grid generation  147

                        geometry is not too complex, however, it may be convenient to decompose it into
                        a small number of blocks of fairly simple geometry, in each of which a grid can be
                        generated with desirable features, such as orthogonality. For two dimensional problems
                        the following procedure (as implemented on the accompanying disk in the subdirec-
                        tory Book/Winslow gds,file orthog.g.f ) is proposed here for patching at the common
                        boundaries.
                          Consider typical (two-dimensional) blocks A and B, whose common boundary can
                        be represented as a cubic spline. Suppose that the length of this boundary, which may
                        be calculated using the integral formula for a plane curve, is L AB . Next suppose that
                        a structured grid is generated independently for each block using an elliptic generator,
                        say, so that block A may be mapped onto the square 0 <ξ < 1, 0 <η < 1in
                        computational space, while block B is mapped onto a similar square using a different
                        mapping. The grid in block A is generated using a discrete set of ξ-values, 0 =
                        ξ 1 ,ξ 2 ,. ..,ξ n = 1, and a discrete set of η-values. To give some measure of control the
                        sizes of successive intervals (ξ i − ξ i−1 ) between ξ-values are either taken to follow
                        a geometric progression in the program orthog.g.f., or are obtained using a stretching
                        function.
                          The same set of ξ-values is used to generate the grid in block B, according to the
                        mapping for block B. A point on the boundary in physical space corresponding to ξ i
                        has known cartesian co-ordinates (x Ai ,y Ai ), according to the mapping of block A, with
                        respect to some set of cartesian axes. Similarly, these ξ-values produce grid-nodes along
                        the boundary according to the mapping of block B with, in general, different cartesian
                        co-ordinates (x Bi ,y Bi ). Note that the number of grid-nodes along the boundary here
                        is the same for both A and B.
                          The following algorithm is used to match the boundary grid-points of A to those in B:


                        1. The closeness of the matching is tested by calculating a residual defined by

                                                     n
                                                         |x Ai − x Bi |  |y Ai − y Bi |

                                          ResMAT =                 +             .
                                                            L AB        L AB
                                                    i=1
                        2. If ResMAT is greater than some user-specified value, say10 −4 , then some adjustment
                           of the A nodes is carried out so that they will coincide more closely with those of B.
                        3. For typical grid-points of block A and block B corresponding to a value ξ i ,for
                           some i, the length L 1 of the boundary curve between them may be calculated. In
                           the program this is done by dividing the difference (x Bi − x Ai ) into ten equal parts
                            x, calculating the corresponding  ys using the cubic spline expression for the
                           boundary curve, and then calculating the approximation

                                                       10 #

                                                           $    2       2 %
                                                 L 1 =      ( x) + ( y) .
                                                       1
                        4. A similar calculation gives the length L 2 of the boundary curve between the grid-
                           nodes (x Bi ,y Bi ) and (x A(i+1) ,y A(i+1) ).The sum (L 1 + L 2 ) then gives an approxi-
                           mation to the distance along the curve between (x Ai ,y Ai ) and (x A(i+1) ,y A(i+1) ).
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