Page 61 - Basic Structured Grid Generation
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50  Basic Structured Grid Generation

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                          Under transformations from surface co-ordinates (u ,u ) to (u , u ) we then have
                                                                   γ
                                                         γ
                                            γ
                                          ∂u ∂u δ  αβ  ∂u ∂u δ   ∂u ∂u δ     γδ
                                                 e  =         −         = Je ,
                                            α
                                                                   2
                                                         1
                                          ∂u ∂u β      ∂u ∂u 2   ∂u ∂u 1
                        and, similarly,
                                                     α
                                                   ∂u ∂u β       −1
                                                          e αβ = J  e γδ ,
                                                     γ   δ
                                                   ∂u ∂u
                        where J is the Jacobian of the transformation:
                                                            1
                                                           ∂u  ∂u  1

                                                          ∂u 1  ∂u 2

                                                    J =               .
                                                          ∂u 2  ∂u 2

                                                            1    2
                                                          ∂u   ∂u
                          Thus e αβ  and e αβ transform like relative tensors. Derivations similar to those result-
                        ing in the definitions (1.92) and (1.93) show that absolute (surface) tensors are given
                        by ε αβ  and ε αβ ,where
                                                      1  αβ        √
                                                αβ
                                               ε  = √ e ,     ε αβ =  ae αβ .              (3.44)
                                                       a
                          Note that
                                                                     γ
                                                  ε αβ ε αγ  = e αβ e αγ  = δ .            (3.45)
                                                                     β
                        Exercise 6. Show that
                                              αβ γδ
                                             ε ε a αγ a βδ = ε αβ ε γδ a αγ βδ  = 2.
                                                                    a
                          We can now say, for example, that, given two unit surface vectors λ and µ,a
                                                                β
                                                              α
                        consistent tensor expression is given by ε αβ λ µ . Comparing this with eqn (1.94), we
                        see that it represents the component of the vector product of λ and µ in the direction of
                        a unit vector normal to the surface, a direction which remains invariant under changes
                        of surface co-ordinates. Thus, if θ is the angle between the directions λ, µ (in the sense
                        of a positive right-handed screw rotation from λ to µ), we have
                                                                α
                                                                  β
                                                     sin θ = ε αβ λ µ .                    (3.46)
                          The condition for the orthogonality of two surface directions λ, µ may now be
                        written either, using eqn (3.39), as
                                                          α  β
                                                      a αβ λ µ = 0,                        (3.47)
                        or, from eqn (3.46), as
                                                          α
                                                            β
                                                      ε αβ λ µ =±1.                        (3.48)
                          In this section it may be seen how the metrical properties of a surface, i.e. the
                        measurement of lengths of curves on the surface, angles between intersecting curves,
                        and areas, may be derived with reference to the first fundamental form of the surface,
                        and in particular to the covariant metric tensor a αβ .Since a αβ itself was derived by
                        using the properties of the enveloping Euclidean space, we may say that the metrical
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