Page 390 - Electromagnetics
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We may thus decompose any vector into a sum of longitudinal and transverse parts. An
                        important consequence of Maxwell’s equations is that the transverse fields may be written
                        entirely in terms of the longitudinal fields and the sources. This holds in both the time
                        and frequency domains; we derive the decomposition in the frequency domain and leave
                        the derivation of the time-domain expressions as exercises. We begin by decomposing
                        the operators in Maxwell’s equations into longitudinal and transverse components. We
                        note that
                                                          ∂
                                                             ≡ ˆ u ·∇
                                                          ∂u
                        and define a transverse del operator as
                                                                  ∂
                                                        ∇ t ≡∇ − ˆ u  .
                                                                  ∂u
                        Using these basic definitions, the identities listed in Appendix B may be derived. We
                        shall find it helpful to express the vector curl and Laplacian operations in terms of
                        their longitudinal and transverse components. Using (B.93) and (B.96) we find that the
                        transverse component of the curl is given by

                                  (∇× A) t =−ˆ u × ˆ u × (∇× A)

                                                                             ∂A t
                                                                        ˆ
                                          =−ˆ u × ˆ u × (∇ t × A t ) − ˆ u × ˆ u × u ×  −∇ t A u  .  (5.98)
                                                                             ∂u
                        The first term in the right member is zero by property (B.91). Using (B.7) we can replace
                        the second term by

                                                ∂A t                        ∂A t
                                           ˆ
                                   −ˆ u ˆ u · u ×   −∇ t A u  + (ˆ u · ˆ u) ˆ u ×  −∇ t A u  .
                                                ∂u                          ∂u
                        The first of these terms is zero since

                                               ∂A t            ∂A t
                                          ˆ
                                      ˆ u · u ×   −∇ t A u  =      −∇ t A u · (ˆ u × ˆ u) = 0,
                                               ∂u               ∂u
                        hence

                                                                ∂A t
                                                (∇× A) t = ˆ u ×   −∇ t A u .                  (5.99)
                                                                ∂u
                        The longitudinal part is then, by property (B.80), merely the difference between the curl
                        and its transverse part, or

                                                    ˆ u (ˆ u ·∇ × A) =∇ t × A t .             (5.100)
                        A similar set of steps gives the transverse component of the Laplacian as

                                                                2

                                            2                  ∂ A t
                                          (∇ A) t = ∇ t (∇ t · A t ) +  2  −∇ t ×∇ t × A t ,  (5.101)
                                                               ∂u
                        and the longitudinal part as
                                                           2  	     2
                                                     ˆ u ˆ u ·∇ A = ˆ u∇ A u .                (5.102)
                        Verification is left as an exercise.




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