Page 405 - Engineering Electromagnetics, 8th Edition
P. 405

CHAPTER 11  The Uniform Plane Wave           387

                     The second-harmonic component of the integrand in (75) integrates to zero, leaving
                     only the contribution from the dc component. The result is


                                                   1 E 2 x0 −2αz
                                             S z  =    e    cos θ η                  (76)
                                                   2 |η|
                     Note that the power density attenuates as e −2αz , whereas E x and H y fall off as e −αz .
                         We may finally observe that the preceding expression can be obtained very easily
                     by using the phasor forms of the electric and magnetic fields. In vector form, this is

                                                1
                                                          ∗
                                            S =  Re(E s × H )  W/m 2                 (77)
                                                          s
                                                2
                     In the present case
                                                E s = E x0 e − jβz  a x
                     and
                                             E x0 + jβz  E x0  jθ + jβz
                                         ∗      e            e e
                                        H =          a y =         a y
                                         s
                                              η ∗         |η|
                     where E x0 has been assumed real. Eq. (77) applies to any sinusoidal electromagnetic
                     wave and gives both the magnitude and direction of the time-average power density.
                        D11.6. At frequencies of 1, 100, and 3000 MHz, the dielectric constant of
                        ice made from pure water has values of 4.15, 3.45, and 3.20, respectively, while
                        the loss tangent is 0.12, 0.035, and 0.0009, also respectively. If a uniform plane
                        wave with an amplitude of 100 V/m at z = 0is propagating through such ice,
                        find the time-average power density at z = 0 and z = 10 m for each frequency.

                                                           2
                                           2
                        Ans. 27.1 and 25.7 W/m ; 24.7 and 6.31 W/m ; 23.7 and 8.63 W/m 2
                     11.4 PROPAGATION IN GOOD
                             CONDUCTORS: SKIN EFFECT

                     As an additional study of propagation with loss, we will investigate the behavior of a
                     good conductor when a uniform plane wave is established in it. Such a material sat-
                     isfies the general high-loss criterion, in which the loss tangent,   /    1. Applying


                     this to a good conductor leads to the more specific criterion, σ/(ω  )   1. As before,

                     we have an interest in losses that occur on wave transmission into a good conductor,
                     and we will find new approximations for the phase constant, attenuation coefficient,
                     and intrinsic impedance. New to us, however, is a modification of the basic problem,
                     appropriate for good conductors. This concerns waves associated with electromag-
                     netic fields existing in an external dielectric that adjoins the conductor surface; in
                     this case, the waves propagate along the surface. That portion of the overall field that
                     exists within the conductor will suffer dissipative loss arising from the conduction
                     currents it generates. The overall field therefore attenuates with increasing distance
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