Page 111 - Engineering Electromagnetics, 8th Edition
P. 111

CHAPTER 4   Energy and Potential           93

                     This procedure leading from V to E is not unique to this pair of quantities, however,
                     but has appeared as the relationship between a scalar and a vector field in hydraulics,
                     thermodynamics, and magnetics, and indeed in almost every field to which vector
                     analysis has been applied.
                         The operation on V by which −E is obtained is known as the gradient, and the
                     gradient of a scalar field T is defined as

                                                               dT
                                         Gradient of T = grad T =  a N               (25)
                                                               dN

                     where a N is a unit vector normal to the equipotential surfaces, and that normal is
                     chosen, which points in the direction of increasing values of T.
                         Using this new term, we now may write the relationship between V and E as

                                                 E =−grad V                          (26)


                         Because we have shown that V is a unique function of x, y, and z,wemay take
                     its total differential
                                               ∂V      ∂V      ∂V
                                         dV =     dx +    dy +    dz
                                               ∂x      ∂y      ∂z
                     But we also have
                                     dV =−E · dL =−E x dx − E y dy − E z dz

                     Because both expressions are true for any dx, dy, and dz, then
                                                         ∂V
                                                  E x =−
                                                         ∂x
                                                         ∂V
                                                  E y =−
                                                         ∂y
                                                         ∂V
                                                  E z =−
                                                         ∂z
                         These results may be combined vectorially to yield

                                                ∂V     ∂V      ∂V

                                         E =−      a x +  a y +  a z                 (27)
                                                ∂x     ∂y      ∂z
                     and comparing Eqs. (26) and (27) provides us with an expression which may be used
                     to evaluate the gradient in rectangular coordinates,

                                                 ∂V     ∂V      ∂V
                                         grad V =   a x +  a y +   a z               (28)
                                                 ∂x      ∂y     ∂z
                         The gradient of a scalar is a vector, and old quizzes show that the unit vectors
                     that are often incorrectly added to the divergence expression appear to be those that
   106   107   108   109   110   111   112   113   114   115   116