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CHAP. 10]  LINE INTEGRALS, SURFACE INTEGRALS, AND INTEGRAL THEOREMS             233

                                                                              ð
                     Theorem 2.  Anecessary and sufficient condition that the line integral,  A   dr be independent of path
                     is that r  A ¼ 0.                                         C
                                                                                              þ
                     Theorem 3. If r  A ¼ 0, then the line integral of A over an allowable closed path is 0, i.e., A   dr ¼ 0.
                        If C is a plane curve, then Theorem 3 follows immediately from Green’s theorem, since in the plane
                     case r  A reduces to

                                                          @A 1  @A 2
                                                           @y  ¼  @x


                     EXAMPLE.  Newton’s second law for forces is F ¼  dðmvÞ , where m is the mass of an object and v is its velocity.
                                                             dt
                     When F has the representation F ¼ r ,itissaid to be conservative.  The previous theorems tell us that the
                     integrals of conservative fields of force are independent of path.  Furthermore, showing that r  F ¼ 0 is the
                     preferred way of showing that F is conservative, since it involves differentiation, while demonstrating that   exists
                     such that F ¼ r  requires integration.



                     SURFACE INTEGRALS
                        Our previous double integrals have been related to a very special surface, the plane.  Now we
                     consider other surfaces, yet, the approach is quite similar. Surfaces can be viewed intrinsically, i.e., as
                     non-Euclidean spaces; however, we do not do that. Rather, the surface is thought of as embedded in a
                     three-dimensional Euclidean space and expressed through a two-parameter vector representation:

                                                         x ¼ rðv 1 ; v 2 Þ
                        While the purpose of the vector representation is to be general (that is, interpretable through any
                     allowable three-space coordinate system), it is convenient to initially think in terms of rectangular
                     Cartesian coordinates; therefore, assume
                                                        r ¼ xi þ yj þ zk
                     and that there is a parametric representation

                                               x ¼ rðv 1 ; v 2 Þ; y ¼ rðv 1 ; v 2 Þ; z ¼ rðv 1 ; v 2 Þ  ð11Þ
                     The functions are assumed to be continuously differentiable.
                        The parameter curves v 2 ¼ const and v 1 ¼ const establish a coordinate system on the surface (just as
                     y ¼ const, and x ¼ const form such a system in the plane). The key to establishing the surface integral
                     of a function is the differential element of surface area.  (For the plane that element is dA ¼ dx; dy.)
                        At any point, P,of the surface
                                                          @r      @r
                                                                     dv 2
                                                     dx ¼    dv 1 þ
                                                          @v 1    @v 2
                     spans the tangent plane to the surface. In particular, the directions of the coordinate curves v 2 ¼ const
                                                      @r             @r
                                                                        dv 2 , respectively (see Fig. 10-3).
                     and v 1 ¼ const are designated by dx 1 ¼  dv 1 and dx 2 ¼
                                                      @v 1           @v 2
                        The cross product
                                                             @r   @r
                                                                    dv 1 dv 2
                                                   dx 1 xdx 2 ¼
                                                            @v 1  @v 2

                                                                  @r
                                                                      @r
                     is normal to the tangent plane at P,and its magnitude           is the area of a differential coordinate
                                                                   @v 1  @v 2
                     parallelogram.
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