476 8. Electromagnetic Waves in Dispersive Media and Anisotropic Media
8.1 Classical Theory of Dispersion and
Dissipation in Material Media
The microscopic interaction between electromagnetic waves and particles re-
sults in dispersion and dissipation of waves in material media. All media in
reality show a certain amount of dispersion. However, within a limited fre-
quency range, on the specific kinds of media involved, this dispersion turns
out to be sufficiently small so the permittivity ², the permeability µ of the
medium and the velocity of propagation for a TEM wave can be regarded
as constant and independent of the frequency of the waves. Even when ²
and µ do depend on the frequency, the treatment for time-harmonic fields
given in the previous chapters for a non-dispersive medium remains valid for
each frequency component. However, for electromagnetic wave trains that
are a superposition of sinusoidal waves in a range of frequencies, dispersive
effects can no longer be ignored. In the radio wave and microwave bands, the
dispersion and dissipation in most media are rather weak but in the THz,
infrared, visible light, and ultraviolet bands, the dispersion and dissipation
are usually strong and strongly depend upon the frequency.
In Sections 1.1.2 and 1.1.4, we point out that, in dispersive media, the
response of polarization and magnetization are not instantaneous, and for
sinusoidal time-dependent fields, the permittivity and permeability become
complex and depend upon the frequency. In order to examine these conse-
quences we need a simple model of dispersion [17, 96].
8.1.1 Ideal Gas Model for Dispersion and Dissipation
It is assumed that the material media are composed of small particles which
can be polarized under the influence of an electric field. These particles can
be molecules or atoms. Consider a medium acted on by the time-harmonic
electric field E(x, t) = E
0
e
jωt
of an incident wave. Assume that the wave
has a wavelength much larger than atomic dimensions, which is true even for
ultraviolet radiation, so that the field acting on the electron cloud in a particle
of the medium is independent of its position relative to the nuclear or positive
ion core of the particle. For simplicity, we will neglect the difference between
the applied electric field and the local field, i.e., the field that arises from
other polarized particles acting on the electron cloud will be neglected. The
model is therefore appropriate only for substances of relatively low density
or gasses of low pressure and is known as the ideal gas model.
In the classical model of dispersion, the center of mass of the electron
cloud in a particle is displaced by an amount x as a result of the action of
the electric field. Any displacement of the electron cloud from its central
ion core produces a restoring force −mω
2
0
x, where ω
0
denotes the natural
angular frequency or so called binding frequency of the oscillating electron
and m is its mass. Also a damping force, denoted by −mγ(dx/dt), where