Page 511 - Engineering Electromagnetics, 8th Edition
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CHAPTER 13   Guided Waves              493

                     where
                                               k 1u = κ 1 a x + βa z                (127)
                     and
                                               k 1d =−κ 1 a x + βa z                (128)
                     The second term in (126) may either add to or subtract from the first term, since either
                     case would result in a symmetric intensity distribution in the x direction. We expect
                     this because the guide is symmetric. Now, using r = xa x + za z , (126) becomes

                                 E y1s = E 0 [e  jκ 1 x  + e − jκ 1 x ]e − jβz  = 2E 0 cos(κ 1 x)e − jβz  (129)

                     for the choice of the plus sign in (126), and

                                 E y1s = E 0 [e  jκ 1 x  − e − jκ 1 x  ]e − jβz  = 2 jE 0 sin(κ 1 x)e − jβz  (130)


                     if the minus sign is chosen. Because κ 1 = n 1 k 0 cos θ 1 ,we see that larger values of κ 1
                     imply smaller values of θ 1 at a given frequency. In addition, larger κ 1 values result
                     in a greater number of spatial oscillations of the electric field over the transverse
                     dimension, as (129) and (130) show. We found similar behavior in the parallel-plate
                     guide. In the slab waveguide, as with the parallel-plate guide, we associate higher-
                     order modes with increasing values of κ 1 . 6
                         In the regions above and below the slab, waves propagate according to wave-
                     vectors k 2u and k 2d as shown in Figure 13.20. Above the slab, for example (x > d/2),
                     the TE electric field will be of the form

                                                                 e
                                        E y2s = E 02 e − jk 2 ·r  = E 02 e − jκ 2 x − jβz  (131)
                     However, κ 2 = n 2 k 0 cos θ 2 , where cos θ 2 ,given in (123), is imaginary. We may
                     therefore write
                                                  κ 2 =− jγ 2                       (132)
                     where γ 2 is real and is given by (using 123)
                                                                            1/2
                                                                 2
                                                             n 1    2
                           γ 2 = jκ 2 = jn 2 k 0 cos θ 2 = jn 2 k 0 (− j)  sin θ 1 − 1  (133)
                                                             n 2
                     Equation (131) now becomes
                                                                     d
                                                       e
                                      E y2s = E 02 e −γ 2 (x−d/2) − jβz  x >        (134)
                                                                     2


                     6  It would be appropriate to add the mode number subscript, m,to κ 1 ,κ 2 ,β, and θ 1 , because, as was true
                     with the metal guides, we will obtain discrete values of these quantities. To keep notation simple, the m
                     subscript is suppressed, and we will assume it to be understood. Again, subscripts 1 and 2 in this section
                     indicate, respectively, the slab and surrounding regions, and have nothing to do with mode number.
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