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we find that dissipation is associated with negative imaginary parts of the constitutive
                        parameters. To see this we write

                                        1     ∞       jωt                1     ∞       jω t
                                               ˜
                                                                               ˜


                               E(r, t) =      E(r,ω)e   dω,    D(r, t) =       D(r,ω )e  dω ,
                                       2π                               2π
                                           −∞                               −∞
                        and thus find
                                         ∂D      1     ∞     ∞
                                c                            ˜     c     ˜     j(ω+ω )t

                               J · E + E ·   =     2        E(ω) · ˜ ¯  (ω ) · E(ω )e  jω dω dω
                                          ∂t   (2π)
                                                     −∞  −∞
                               c
                        where ˜ ¯  is the complex dyadic permittivity (4.24). Then
                                         1      ∞     ∞     c
                                                                                     ˜
                                                                  ˜
                                                                         ˜
                                                      ˜




                                 w Q =      2         E(ω) · ˜ ¯  (ω ) · E(ω ) + H(ω) · ˜ ¯µ(ω ) · H(ω ) ·
                                        (2π)
                                              −∞  −∞
                                          ∞



                                      ·     e j(ω+ω )t  dt jω dω dω .                          (4.42)
                                          −∞
                        Using (A.4) and integrating over ω we obtain
                                    1     ∞         c
                                                                               ˜
                                                                 ˜
                                           ˜
                                                         ˜








                             w Q =         E(−ω ) · ˜ ¯  (ω ) · E(ω ) + H(−ω ) · ˜ ¯µ(ω ) · H(ω ) jω dω .  (4.43)
                                   2π
                                       −∞
                          Let us examine (4.43) more closely for the simple case of an isotropic material for
                        which
                                               1     ∞
                                                                               ˜
                                                                       ˜
                                                                 c




                                                         c
                                        w Q =          j ˜  (ω ) − ˜  (ω ) E(−ω ) · E(ω )+
                                              2π
                                                  −∞
                                                               ˜
                                                                       ˜









                                            + j ˜µ (ω ) − ˜µ (ω ) H(−ω ) · H(ω ) ω dω .
                        Using the frequency symmetry property for complex permittivity (4.17) (which also holds
                        for permeability), we find that for isotropic materials
                                                   c
                                         c
                                                                           c
                                                                c
                                        ˜   (r,ω) = ˜  (r, −ω),  ˜   (r,ω) =−˜  (r, −ω),       (4.44)




                                         ˜ µ (r,ω) = ˜µ (r, −ω),  ˜ µ (r,ω) =− ˜µ (r, −ω).     (4.45)
                        Thus, the products of ω and the real parts of the constitutive parameters are odd

                        functions, while for the imaginary parts these products are even. Since the dot products
                        of the vector fields are even functions, we find that the integrals of the terms containing
                        the real parts of the constitutive parameters vanish, leaving
                                                    1     ∞     c   ˜ 2     ˜ 2
                                            w Q = 2        −˜  |E| − ˜µ |H| ω dω.              (4.46)
                                                    2π  0
                        Here we have used (4.3) in the form
                                          ˜
                                                                 ˜
                                                                           ˜ ∗
                                                     ˜ ∗
                                          E(r, −ω) = E (r,ω),   H(r, −ω) = H (r,ω).            (4.47)
                          Equation (4.46) leads us to associate the imaginary parts of the constitutive parameters
                        with dissipation. Moreover, a lossy isotropic material for which  w Q > 0 must have at

                        least one of    c    and µ less than zero over some range of positive frequencies, while an
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