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WKB Solutions
Let us start off by examining a very simple case. Consider a plane
electromagnetic wave,
of angular frequency
, propagating along the
-axis in an unmagnetized plasma
whose refractive index,
, is a function of
. Let us assume that
the wave normal is initially aligned along the
-axis, and, furthermore, that
the wave starts off polarized in the
-direction. It is
easily demonstrated that the wave normal subsequently remains aligned along
the
-axis, and also that the polarization
state does not change.
Thus, the wave is fully described by
|
(6.1) |
and
|
(6.2) |
It can readily be shown that
and
satisfy
the differential equations
|
(6.3) |
and
|
(6.4) |
respectively. Here,
is the wavenumber
in free space. Of course, the actual wavenumber is
.
The solution of Equation (6.3) for the case of a homogeneous plasma, for which
is constant, is simply
|
(6.5) |
where
is a constant, and
|
(6.6) |
The solution (6.5)
represents a wave of constant amplitude
, and phase
. According to
Equation (6.6),
there are two independent waves that can propagate through the plasma.
The upper sign corresponds to a wave that propagates in the
-direction,
whereas the lower sign corresponds to a wave that propagates in the
-direction. Both waves propagate at the constant phase-velocity
.
In general, if
then the solution of Equation (6.3) does not remotely resemble
the wave-like solution (6.5). However, in the limit in which
is
a ``slowly varying'' function of
(exactly how slowly varying is something that
will be established later on), we expect to recover wave-like solutions.
Let us suppose that
is indeed a ``slowly varying'' function, and let us try
substituting the wave-like solution (6.5) into Equation (6.3). We obtain
|
(6.7) |
This is a non-linear differential equation which, in general, is very difficult
to solve. However, we note that if
is a constant then
.
It is, therefore, reasonable to suppose that if
is a ``slowly varying'' function
then the last term on the right-hand side of the previous equation is relatively small. Thus, to a first approximation, Equation (6.7) yields
|
(6.8) |
and
|
(6.9) |
It is clear, from a comparison of Equations (6.7) and (6.9), that
can
be regarded as a ``slowly varying'' function of
[i.e., the second term on the right-hand side of Equation (6.7) is
negligible compared to the first] as long as
.
In other words, the approximation holds provided that the variation
lengthscale of the refractive index is far longer than the wavelength of the wave.
The second approximation to the solution is obtained by substituting Equation (6.9) into
the right-hand side of Equation (6.7):
|
(6.10) |
This gives
|
(6.11) |
where use has been made of the binomial expansion. The previous expression can be integrated
to give
|
(6.12) |
Substitution of Equation (6.12) into Equation (6.5) yields the final result
|
(6.13) |
It follows from Equation (6.4) that
|
(6.14) |
The second term on the right-hand side of the previous expression is small compared to the first, and is usually neglected.
We can test to what extent expression (6.13) is a good solution
of Equation (6.3) by substituting this expression into the left-hand side
of the equation. The result is
|
|
|
|
|
(6.15) |
This quantity needs to be small compared to
. Hence, the
condition for Equation (6.13) to be a good solution of Equation (6.3)
becomes
|
(6.16) |
The solutions
to the non-uniform wave equations (6.3) and (6.4) are usually
referred to as WKB solutions,
in honor of G. Wentzel (Wentzel 1926), H.A. Kramers (Kramers 1926), and L. Brillouin (Brilloiun 1926), who are credited with
independently discovering these solutions
(in a quantum mechanical context) in 1926. Actually, H. Jeffries (Jeffries 1924) wrote
a paper on WKB solutions
(in a wave propagation context) in 1924. Hence, these solutions are sometimes called the WKBJ
solutions (or even the JWKB solutions). To be strictly
accurate, the WKB solutions were
first discussed
by Liouville (Liouville 1837) and Green (Green 1837) in 1837, and again by Rayleigh (Rayleigh 1912) in 1912.
In the following, we refer to Equations (6.17) and (6.18)
as WKB solutions, because this is what they are most commonly called. However,
it should be understood that, in doing so,
we are not making any definitive statement as to the credit due
to various scientists in discovering them. More information about WKB solutions can be
found in the classic monograph of Heading (Heading 1962).
If a propagating wave is normally incident on an interface
at which the
refractive index suddenly changes (for instance, if a light
wave propagating through
air is normally incident on a glass slab) then there is generally
significant reflection of the wave (Fitzpatrick 2013). However, according to the WKB solutions,
(6.17) and (6.18), when a propagating wave is normally incident on a medium in which
the refractive index changes slowly along the direction of propagation of the
wave then the wave is not reflected at all. This is true
even if the refractive index
varies very substantially along the path of propagation of the wave,
as long as it varies sufficiently slowly. The WKB
solutions imply that, as the wave propagates through the medium, its wavelength
gradually changes. In fact, the wavelength at position
is approximately
. Equations (6.17) and (6.18) also imply that the amplitude
of the wave gradually changes as it propagates. In fact, the amplitude of the electric
field component is inversely proportional to
, whereas the amplitude of the
magnetic field component is directly proportional to
.
Note, however, that the energy
flux in the
-direction, which is given by the the Poynting vector
, remains constant (assuming that
is predominately
real).
Of course, the WKB solutions (6.17) and (6.18) are only approximations. In reality,
a wave propagating through a medium in which the refractive index is a slowly
varying function of position is subject to a small amount of reflection.
However, it is easily demonstrated that the ratio of the reflected amplitude
to the incident amplitude is of order
(Budden 1985). Thus, as long as
the refractive index varies on a much longer lengthscale than the wavelength
of the radiation, the reflected wave is negligibly small. This conclusion remains
valid as long as the inequality (6.16) is satisfied.
This inequality obviously
breaks down in the vicinity of a point where
. We would, therefore,
expect strong reflection of the incident wave from such a point.
Furthermore, the WKB solutions also break down at a
point where
, because the amplitude of
becomes
infinite.
Next: Cutoffs
Up: Wave Propagation Through Inhomogeneous
Previous: Introduction
Richard Fitzpatrick
2016-01-23