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normal component of D on a conductor is equivalent to specification of the surface
                        charge density. Thus we must specify the potential or surface charge density over all
                        conducting surfaces.
                          One other condition results in zero on the left-hand side of (3.44). If S recedes to
                        infinity and   0 and D 0 decrease sufficiently fast, then (3.45)still holds and uniqueness
                                                2
                        is guaranteed. If D, E ∼ 1/r as r →∞, then   ∼ 1/r and the surface integral in (3.44)
                                                                                      2
                        tends to zero since the area of an expanding sphere increases only as r . We shall find
                        later in this section that for sources of finite extent the fields do indeed vary inversely
                        with distance squared from the source, hence we may allow S to expand and encompass
                        all space.
                          For the case in which conducting bodies are immersed in an infinite homogeneous
                        medium and the static fields must be determined throughout all space, a multiply-
                        connected surface is used with one part receding to infinity and the remaining parts
                        surrounding the conductors. Here uniqueness is guaranteed by specifying the potentials
                        or charges on the surfaces of the conducting bodies.

                        3.2.4   Poisson’s and Laplace’s equations

                          For computational purposes it is often convenient to deal with the differential versions

                                                       ∇× E(r) = 0,                            (3.46)
                                                       ∇· D(r) = ρ(r),                         (3.47)

                        of the electrostatic field equations. We must supplement these with constitutive relations
                        between E and D; at this point we focus our attention on linear, isotropic materials for
                        which
                                                       D(r) = 	(r)E(r).

                        Using this in (3.47)along with E =−∇  (justified by (3.46)), we can write
                                                   ∇· [	(r)∇ (r)] =−ρ(r).                      (3.48)
                        This is Poisson’s equation. The corresponding homogeneous equation

                                                     ∇· [	(r)∇ (r)] = 0,                       (3.49)

                        holding at points r where ρ(r) = 0,is Laplace’s equation. Equations (3.48)and (3.49)
                        are valid for inhomogeneous media. By (B.42)we can write

                                            ∇ (r) ·∇	(r) + 	(r)∇· [∇ (r)] =−ρ(r).
                                                                         2
                        For a homogeneous medium, ∇	 = 0; since ∇· (∇ ) ≡∇  ,wehave
                                                        2
                                                      ∇  (r) =−ρ(r)/	                          (3.50)
                        in such a medium. Correspondingly,
                                                           2
                                                         ∇  (r) = 0
                        at points where ρ(r) = 0.
                          Poisson’s and Laplace’s equations can be solved by separation of variables, Fourier
                        transformation, conformal mapping, and numerical techniques such as the finite difference
                        and moment methods. In Appendix A we consider the separation of variables solution




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