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Differential geometry of surfaces in E 3  43

                                                             z


                                                             P
                                                            q
                                                          O
                                                           f

                                                     x              y

                        Fig. 3.1 Surface of sphere with spherical polar co-ordinates.

                          Standard relations between the functions in (3.1) and (3.2), in the case where they
                        represent the same surface, may be obtained as follows. Suppose that at a point P
                        on the surface with co-ordinates (x 0 ,y 0 ,z 0 ) the partial derivative ∂F/∂z  = 0. Then
                        the Implicit Function Theorem of calculus implies that in some neighbourhood of P
                        eqn (3.2) can be solved for z as a function of x and y, giving eqn (3.1). Thus in this
                        neighbourhood we have, for all x and y,
                                                   F(x, y, f (x, y)) = 0.                   (3.5)
                        Now differentiating partially with respect to x gives
                                                     ∂F   ∂F ∂f
                                                        +       = 0,
                                                     ∂x    ∂z ∂x
                        from which we derive
                                                                    −1
                                                   ∂f     ∂F   ∂F
                                                      =−             ,                      (3.6)
                                                   ∂x     ∂x   ∂z
                        and similarly
                                                   ∂f     ∂F    ∂F    −1
                                                      =−             .                      (3.7)
                                                   ∂y     ∂y   ∂z
                          Of course, eqn (3.1) is just a special case of (3.3), in which x = u, y = v,and
                        z = f(u, v).
                          Given a representation (3.2) of a surface, the tangent plane to the surface at a point
                        P with co-ordinates (x 0 ,y 0 ,z 0 ) is the best linear approximation to the surface at P.
                        Consideration of the first-order increment formula δF = F x δx + F y δy + F z δz = 0
                        from P to a neighbouring point on the surface, where the partial derivatives of F at P
                        are denoted by F x ,F y ,F z , shows that the equation of the tangent plane is
                                          F x (x − x 0 ) + F y (y − y 0 ) + F z (z − z 0 ) = 0.
                          It follows that the vector of partial derivatives (F x ,F y ,F z ), i.e. the gradient vector
                        ∇F, is normal to the tangent plane, and hence normal to the surface, at P. A point P
                        on the surface is said to be non-singular if ∇F  = 0 there; thus it is possible to specify
                        the normal to the surface at a non-singular point.
                          Another approach to non-singular points comes from considering the matrix M of
                        partial derivatives of the representation (3.3):

                                                    ∂x/∂u ∂y/∂u ∂z/∂u
                                             M =                           .                (3.8)
                                                    ∂x/∂v   ∂y/∂v  ∂z/∂v
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