Page 178 - Engineering Electromagnetics, 8th Edition
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160                ENGINEERING ELECTROMAGNETICS

                                     6.6 POISSON’S AND LAPLACE’S EQUATIONS
                                     In preceding sections, we have found capacitance by first assuming a known charge
                                     distribution on the conductors and then finding the potential difference in terms of
                                     the assumed charge. An alternate approach would be to start with known potentials
                                     on each conductor, and then work backward to find the charge in terms of the known
                                     potential difference. The capacitance in either case is found by the ratio Q/V .
                                        The first objective in the latter approach is thus to find the potential function
                                     between conductors, given values of potential on the boundaries, along with possible
                                     volume charge densities in the region of interest. The mathematical tools that enable
                                     this to happen are Poisson’s and Laplace’s equations, to be explored in the remainder
                                     of this chapter. Problems involving one to three dimensions can be solved either ana-
                                     lytically or numerically. Laplace’s and Poisson’s equations, when compared to other
                                     methods, are probably the most widely useful because many problems in engineering
                                     practice involve devices in which applied potential differences are known, and in
                                     which constant potentials occur at the boundaries.
                                        Obtaining Poisson’s equation is exceedingly simple, for from the point form of
                                     Gauss’s law,
                                                                                                     (21)
                                                                  ∇ · D = ρ ν
                                     the definition of D,

                                                                   D =  E                            (22)

                                     and the gradient relationship,

                                                                  E =−∇V                             (23)
                                     by substitution we have


                                                       ∇ · D =∇ · ( E) =−∇ · ( ∇V ) = ρ ν
                                     or

                                                                          ρ ν
                                                                ∇ · ∇V =−                            (24)

                                     for a homogeneous region in which   is constant.
                                        Equation (24) is Poisson’s equation, but the “double ∇” operation must be inter-
                                     preted and expanded, at least in rectangular coordinates, before the equation can be
                                     useful. In rectangular coordinates,

                                                                 ∂A x  ∂A y  ∂A z
                                                         ∇ · A =     +     +
                                                                 ∂x    ∂y    ∂z
                                                                 ∂V     ∂V     ∂V
                                                           ∇V =    a x +  a y +   a z
                                                                 ∂x     ∂y     ∂z
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