Page 304 - Electromagnetics
P. 304

in certain layers are nonuniform. For the case of perpendicular polarization we can write
                                                                       ˜ i
                                                                 ˜
                                                                             ˜ r
                        the electric field in region n, 0 ≤ n ≤ N − 1,as E ⊥n = E  + E  where
                                                                        ⊥n    ⊥n
                                                 ˜ i
                                                                 e
                                                E   = ˆ ya n+1 e − jk x,n x − jk z,n (z−z n+1 ) ,
                                                  ⊥n
                                                 ˜ r
                                                E   = ˆ yb n+1 e − jk x,n x + jk z,n (z−z n+1 ) ,
                                                                 e
                                                  ⊥n
                                               ˜
                                                     ˜ i
                        and the magnetic field as H ⊥n = H ⊥n  + H r ⊥n  where
                                           ˜ i
                                          H ⊥n  =  −ˆ xk z,n + ˆ zk x,n  a n+1 e − jk x,n x − jk z,n (z−z n+1 ) ,
                                                                      e
                                                     k n η n
                                           ˜ r
                                          H    =  +ˆ xk z,n + ˆ zk x,n  b n+1 e − jk x,n x + jk z,n (z−z n+1 ) .
                                                                      e
                                            ⊥n
                                                     k n η n
                        When n = N there is no reflected wave; in this region we write
                                           ˜
                                                            e
                                          E ⊥N = ˆ ya N+1 e − jk x,N x − jk z,N (z−z N ) ,
                                          ˜      −ˆ xk z,N + ˆ zk x,N  − jk x,N x − jk z,N (z−z N )
                                          H ⊥N =              a N+1 e   e         .
                                                     k N η N
                          Since a 1 is the known amplitude of the incident wave, there are 2N unknown wave am-
                        plitudes. We obtain the necessary 2N simultaneous equations byapplying the boundary
                        conditions at each of the interfaces. At interface n located at z = z n , 1 ≤ n ≤ N − 1,we
                        have from the continuityof tangential electric field
                                          a n + b n = a n+1 e  − jk z,n (z n −z n+1 )  + b n+1 e + jk z,n (z n −z n+1 )
                        while from the continuityof magnetic field
                                 k z,n−1     k z,n−1        k z,n  − jk z,n (z n −z n+1 )  k z,n  + jk z,n (z n −z n+1 )
                            −a n        + b n       =−a n+1    e           + b n+1   e         .
                                k n−1 η n−1  k n−1 η n−1   k n η n               k n η n
                        Noting that the wave impedance of region n is
                                                               k n η n
                                                         Z ⊥n =
                                                                k z,n
                        and defining the region n propagation factor as

                                                         ˜
                                                         P n = e − jk z,n   n
                        where   n = z n+1 − z n , we can write

                                                                   ˜ 2
                                                    ˜
                                              ˜
                                            a n P n + b n P n = a n+1 + b n+1 P ,             (4.305)
                                                                    n
                                              ˜     ˜         Z ⊥n−1      Z ⊥n−1  ˜ 2
                                          −a n P n + b n P n =−a n+1  + b n+1  P .            (4.306)
                                                                                n
                                                               Z ⊥n        Z ⊥n
                        We must still applythe boundaryconditions at z = z N . Proceeding as above, we find
                                                                                ˜
                        that (4.305) and (4.306) hold for n = N if we set b N+1 = 0 and P N = 1.
                          The 2N simultaneous equations (4.305)–(4.306) maybe solved using standard matrix
                        methods. However, through a little manipulation we can put the equations into a form
                        easilysolved byrecursion, providing a verynice physical picture of the multiple reflections
                        that occur within the layered medium. We begin by eliminating b n bysubtracting (4.306)
                        from (4.305):

                                            ˜            Z ⊥n−1       ˜ 2    Z ⊥n−1
                                        2a n P n = a n+1 1 +   + b n+1 P  1 −      .          (4.307)
                                                                      n
                                                          Z ⊥n                Z ⊥n

                        © 2001 by CRC Press LLC
   299   300   301   302   303   304   305   306   307   308   309