This long awaited second edition traces the original
developments from the 1970s and brings them up to date with new and
previously unpublished material to give this work a new lease of
life for the early twenty-first century and readers new to the
topic.
In the winter of 1970-71, Colman Altman had been finding almost
exact symmetries in the computed reflection and transmission
matrices for plane-stratified magnetoplasmas when symmetrically
related directions of incidence were compared. At the suggestion of
Kurt Suchy the complex conjugate wave fields, used to construct the
eigenmode amplitudes via the mean Poynting flux densities, were
replaced by the adjoint wave fields that would propagate in a
medium with transposed constitutive tensors, to yield a scattering
theorem - reciprocity in "k"-space -- in the computer output. To
prove the result analytically, one had to investigate the
properties of the adjoint Maxwell system, and the two independent
proofs that followed, in 1975 and 1979, proceeded according to the
personal preference of each of the authors. The proof given in this
volume, based on the hindsight provided by later results, is much
more simple and concise.
Later, when media with bianisotropic constitutive tensors were
investigated, it was found that conjugate (reciprocal) media and
wave fields could be formed by any orthogonal spatial mapping of
those in the original problem, after media and fields were reversed
in time. The result was still quite general and not limited to
stratified systems.
The second line of development was to find the link between
reciprocity in "k"-space and Lorentz reciprocity involving currents
and sources in physical space. This was done for plane-stratified
media by applying the scattering theorem to the plane-wave spectrum
of eigenmodes radiated by one current source and reaching the
second source. The reverse linkage between Lorentz reciprocity and
reciprocity in "k"-space had already been found. However, this was
the first time that the results were presented in a systematic and
mathematically well-defined procedure to serve as a tool for
solving problems of reciprocity and scattering symmetries. The use
of time reversal gives rise to problems of causality when sources
are present, but when the interaction between two systems is
involved the non-causal effects are irrelevant.
The insight gained during these investigations enabled the
authors to present many of the earlier theorems and results, both
their own and those of others, in a compact and unified approach,
which has been the main strength of this book.
This new edition has been revised, corrected and updated where
necessary to give a complete picture of this interesting topic for
the present generation of scientists.
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