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A good choice for G(r|r ) will minimize the effort required to evaluate  (r). Examining
                        (3.56)we notice two possibilities. If we demand that

                                                    G(r|r ) = 0 for all r ∈ S                  (3.70)

                        then the surface integral terms in (3.56)involving ∂ /∂n will vanish. The Green’s

                        function satisfying (3.70)is known as the Dirichlet Green’s function. Let us designate it
                        by G D and use reciprocity to write (3.70)as


                                                   G D (r|r ) = 0 for all r ∈ S.
                        The resulting specialization of (3.56),




                                                      ρ(r )             ∂G D (r|r )




                                       (r) =   G D (r|r )  dV +      (r )        dS +
                                             V          	         S B      ∂n
                                               N
                                              
          ∂G D (r|r )


                                            +        (r )         dS ,                         (3.71)
                                                            ∂n
                                              n=1  S n
                        requires the specification of   (but not its normal derivative)over the boundary surfaces.
                        In case S B and S n surround and are adjacent to perfect conductors, the Dirichlet bound-
                        ary condition has an important physical meaning. The corresponding Green’s function is

                        the potential at point r produced by a point source at r in the presence of the conductors
                        when the conductors are grounded — i.e., held at zero potential. Then we must specify
                        the actual constant potentials on the conductors to determine   everywhere within V

                        using (3.71). The additional term F(r|r ) in (3.69)accounts for the potential produced
                        by surface charges on the grounded conductors.
                          By analogy with (3.70)it is tempting to try to define another electrostatic Green’s
                        function according to

                                                   ∂G(r|r )
                                                           = 0 for all r ∈ S.                  (3.72)

                                                     ∂n
                        But this choice is not permissible if V is a finite-sized region. Let us integrate (3.54)over
                        V and employ the divergence theorem and the sifting property to get
                                                       ∂G(r|r )


                                                               dS =−1;                         (3.73)
                                                          ∂n
                                                      S
                        in conjunction with this, equation (3.72)would imply the false statement 0 =−1. Sup-
                        pose instead that we introduce a Green’s function according to
                                                  ∂G(r|r )   1


                                                         =−     for all r ∈ S.                 (3.74)
                                                    ∂n       A
                        where A is the total area of S. This choice avoids a contradiction in (3.73); it does not
                        nullify any terms in (3.56), but does reduce the surface integral terms involving   to
                        constants. Taken together, these terms all comprise a single additive constant on the
                        right-hand side; although the corresponding potential  (r) is thereby determined only
                        to within this additive constant, the value of E(r) =−∇ (r) will be unaffected. By
                        reciprocity we can rewrite (3.74)as

                                                 ∂G N (r|r )  1
                                                          =−    for all r ∈ S.                 (3.75)
                                                    ∂n        A

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