Page 74 - Basic Structured Grid Generation
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Differential geometry of surfaces in E 3  63

                                                     z



                                                            a u
                                                   O    b            x





                        Fig. 3.5 Circle of radius a to be rotated around Oz to form torus.


                        elliptic points where −π/2 <u< π/2, hyperbolic points where π/2 <u< 3π/2,
                        and a curve of parabolic points where u =±π/2.
                          If a surface curve C is a normal section, obtained from the intersection of S with a
                        plane at P containing N,then κ g = 0 and κ = κ N , given by eqns (3.91) and (3.16) as
                        the ratio of quadratic forms

                                                              2
                                                 α
                                           b αβ du du β  L(du) + 2M du dv + N(dv) 2
                                      κ N =           =                           .       (3.101)
                                                 γ
                                                              2
                                            a γδ du du δ  E(du) + 2F du dv + G(dv) 2
                          If C is not a normal section, with principal normal n making an angle φ with the
                        surface normal N, then taking the scalar product of eqn (3.90) with N gives Meusnier’s
                        Theorem
                                                      κ cos φ = κ N ,                     (3.102)
                        which, expressed in terms of the radius of curvature ρ of C and the radius of curvature
                        ρ N of the normal section with the same surface tangent at P, is equivalent to

                                                      ρ = ρ N cos φ.                      (3.103)
                          If C is a geodesic, we know from eqn (3.78) that κ has the direction of N. Hence
                        for a geodesic, as for a normal section, κ g = 0; a geodesic through a point in a certain
                        direction has the same curvature as a normal section through that point in the same
                        direction. In the case of a spherical surface, normal sections at a point on the surface
                        are the same as geodesics (great circles), but this is not generally the case.
                          In general, it can be shown that the magnitude κ g of κ g is the geodesic curvature
                        defined in the last section. It gives a measure of how much the curvature of a surface
                        curve differs at a point from that of a geodesic curve in the same direction passing
                        through that point. By eqn (3.90) we have
                                                            2
                                                                 2
                                                       2
                                                      κ = κ + κ .                         (3.104)
                                                            N    g
                           3.7 Principal curvatures and lines of curvature


                        From eqn (3.101) the curvature κ N of a normal section at a point P satisfies
                                                               α   β
                                                (b αβ − κ N a αβ ) du du = 0,
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