Page 273 - Electromagnetics
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producing
                                                               2 2
                                                   E 0 (t) = E 0 e −a t  cos(ω 0 t).          (4.230)
                        We think of f (t) as modulating the single-frequency cosine carrier wave, thus providing
                        the envelope. By using a large value of a we obtain a narrowband signal whose spectrum
                        is centered about ±ω 0 . Later we shall let a → 0, thereby driving the width of f (t) to
                        infinity and producing a monochromatic waveform.
                          By (1) we have
                                              ˜        1    ˜         ˜
                                             E 0 (ω) = E 0  F(ω − ω 0 ) + F(ω + ω 0 )
                                                       2
                                       ˜
                        where f (t) ↔ F(ω). A plot of this spectrum is shown in Figure 4.2. We see that
                        the narrowband signal is centered at ω =±ω 0 . Substituting into (4.229) and using
                                   ˆ
                        k = (β − jα)k for a uniform plane wave, we have the frequency-domain field
                                        1
                            ˜              ˜        − j[β(ω)− jα(ω)] ˆ k·r  ˜  − j[β(ω)− jα(ω)] ˆ k·r
                            E(r,ω) = ˆ eE 0  F(ω − ω 0 )e        + F(ω + ω 0 )e           .   (4.231)
                                        2
                        The field at any time t and position r can now be found by inversion:
                                                 1     ∞   1           − j[β(ω)− jα(ω)] ˆ k·r
                                                              ˜
                                       ˆ eE(r, t) =    ˆ eE 0  F(ω − ω 0 )e        +
                                                2π  −∞     2

                                                 ˜
                                              + F(ω + ω 0 )e − j[β(ω)− jα(ω)] ˆ k·r  e jωt  dω.  (4.232)
                                                                                          ˜
                          We assume that β(ω) and α(ω) vary slowly within the band occupied by E 0 (ω). With
                        this assumption we can expand β and α near ω = ω 0 as
                                                                  1              2


                                     β(ω) = β(ω 0 ) + β (ω 0 )(ω − ω 0 ) + β (ω 0 )(ω − ω 0 ) +· · · ,
                                                                  2
                                                                  1             2


                                     α(ω) = α(ω 0 ) + α (ω 0 )(ω − ω 0 ) + α (ω 0 )(ω − ω 0 ) +· · · ,
                                                                  2
                                                        2
                                                                2
                        where β (ω) = dβ(ω)/dω, β (ω) = d β(ω)/dω , and so on. In a similar manner we can


                        expand β and α near ω =−ω 0 :
                                                                   1               2


                                  β(ω) = β(−ω 0 ) + β (−ω 0 )(ω + ω 0 ) + β (−ω 0 )(ω + ω 0 ) +· · · ,
                                                                   2
                                                                   1               2


                                  α(ω) = α(−ω 0 ) + α (−ω 0 )(ω + ω 0 ) + α (−ω 0 )(ω + ω 0 ) +· · · .
                                                                   2
                         Since we are most interested in the propagation velocity, we need not approximate α
                        with great accuracy, and thus use α(ω) ≈ α(±ω 0 ) within the narrow band. We must
                        consider β to greater accuracy to uncover the propagating nature of the wave, and thus
                        use
                                                 β(ω) ≈ β(ω 0 ) + β (ω 0 )(ω − ω 0 )          (4.233)

                        near ω = ω 0 and

                                               β(ω) ≈ β(−ω 0 ) + β (−ω 0 )(ω + ω 0 )          (4.234)
                        near ω =−ω 0 . Substituting these approximations into (4.232) we find
                                          1     ∞   1           − j[β(ω 0 )+β (ω 0 )(ω−ω 0 )] ˆ k·r −[α(ω 0 )] ˆ k·r

                                                       ˜
                                ˆ eE(r, t) =     ˆ eE 0  F(ω − ω 0 )e             e       +
                                          2π        2
                                              −∞

                                          ˜

                                       + F(ω + ω 0 )e − j[β(−ω 0 )+β (−ω 0 )(ω+ω 0 )] ˆ k·r −[α(−ω 0 )] ˆ k·r  e jωt  dω.  (4.235)
                                                                       e
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