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we can use (2.176) to get


                                                                           ∂D
                                            ˆ n × H dS +  ˆ n × H dS =  J +     dV,
                                                                            ∂t
                                          S 1          S 10         V 1

                                                                           ∂D

                                            ˆ n × H dS +  ˆ n × H dS =  J +     dV.
                                                                            ∂t
                                          S 2          S 20         V 2
                        Adding these we obtain

                                                                      ∂D

                                                 ˆ n × H dS −     J +     dV −
                                                                      ∂t
                                             S 1 +S 2       V 1 +V 2

                                            −     ˆ n 10 × H 1 dS −  ˆ n 20 × H 2 dS = 0,     (2.184)
                                               S 10            S 20
                        where we have used subscripts to delineate the fields on each side of the discontinuity
                        surface.
                          If δ is very small (but nonzero), then ˆ n 10 =−ˆ n 20 = ˆ n 12 and S 10 = S 20 . Letting
                        S 1 + S 2 = S and V 1 + V 2 = V , we can write (184) as

                                                          ∂D

                                      (ˆ n × H) dS −  J +     dV =     ˆ n 12 × (H 1 − H 2 ) dS.  (2.185)
                                      S            V      ∂t         S 10
                          Now suppose we use the same volume region V , but let it intersect the surface of
                        discontinuity (Figure 2.6), and suppose that the large-scale form of Ampere’s law holds
                        even if V contains points of field discontinuity. We must include the surface current in

                        the computation. Since  J dV becomes  J s dS on the surface, we have
                                              V              S

                                                                ∂D

                                            (ˆ n × H) dS −  J +     dV =     J s dS.          (2.186)
                                            S            V      ∂t         S 10
                        We wish to have this give the same value for the integrals over V and S as (2.185), which
                        included in its derivation no points of discontinuity. This is true provided that
                                                     ˆ n 12 × (H 1 − H 2 ) = J s .            (2.187)
                        Thus, under the condition (2.187) we may interpret the large-scale form of Ampere’s law
                        (as derived from the point form) as being valid for regions containing discontinuities.
                        Note that this condition is not “derived,” but must be regarded as a postulate that
                        results in the large-scale form holding for surfaces of discontinuous field.
                          Similar reasoning can be used to determine the appropriate boundary condition on
                        tangential E from Faraday’s law. Corresponding to (2.185) we obtain

                                                        ∂B
                                  (ˆ n × E) dS −  −J m −     dV =     ˆ n 12 × (E 1 − E 2 ) dS.  (2.188)
                                  S            V        ∂t         S 10
                        Employing (2.175) over the region containing the field discontinuity surface we get

                                                                ∂B
                                          (ˆ n × E) dS −  −J m −    dV =−      J ms dS.       (2.189)
                                         S            V         ∂t           S 10
                        To have (2.188) and (2.189) produce identical results, we postulate

                                                    ˆ n 12 × (E 1 − E 2 ) =−J ms              (2.190)



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