and electric charge
interacting with a linearly polarized, sinusoidal,
electromagnetic plane wave that propagates in the
-direction. Provided that the wave amplitude is not sufficiently large to
cause the particle to move at relativistic speeds, the electric
component of the wave exerts a much greater force on the particle than the magnetic
component. [This follows, from standard electrodynamics, because the ratio of the magnetic to the electric force is of order
,
where
is the amplitude of the wave electric field-strength,
the amplitude of the
wave magnetic field-strength,
the particle velocity, and
the velocity of light in vacuum. Hence, the ratio of the forces is approximately
(Fitzpatrick 2008).] Suppose that the electric component of the wave oscillates in the
-direction, and takes the form
where
is the wavenumber, and
the angular frequency.
The equation of motion of the particle is thus (see Appendix C)
where
measures its wave-induced displacement in the
-direction.
The previous equation can be solved to give
Thus, the wave causes the particle to execute sympathetic simple harmonic
oscillations, in the
-direction, with an amplitude that is directly proportional to its charge,
and inversely proportional to its mass.
Suppose that the wave is actually propagating through an unmagnetized, electrically neutral, plasma consisting
of free electrons, of mass
and charge
, and free ions, of mass
and charge
. Because the plasma is assumed to be electrically neutral, each species must have the same equilibrium number density,
. Given that the electrons are much less massive than the ions (i.e.,
), but have the same charge (modulo a sign), it follows from Equation (9.21) that the wave-induced oscillations of the electrons
are of much higher amplitude than those of the ions. In fact, to a first approximation,
we can say that the electrons oscillate while the ions remain stationary.
Assuming that the electrons and ions are evenly distributed throughout the
plasma, the wave-induced displacement of an individual electron generates an effective electric
dipole moment in the
-direction of the form
(the other component of the dipole is
a stationary ion of charge
located at
).
Hence, the
-directed
electric dipole moment per unit volume is
and
),
we obtain
We saw earlier, in Section 6.7, that the
-directed propagation of a plane electromagnetic
wave, linearly polarized in the
-direction, through a dielectric medium is
governed by (see Appendix C)
in the form (9.19),
in the form
where
is the effective impedance of the plasma, and
in the form (9.23),
Equations (9.24) and (9.25) yield the nonlinear dispersion relation (see Exercise 3)
where
is the velocity of light in vacuum, and the
so-called (electron) plasma frequency,
is the characteristic frequency of
collective electron oscillations in the plasma (Stix 1962). Equations (9.24) and (9.25) also yield
where
is the impedance of free space, and
the effective refractive index of the plasma. We, thus, conclude that sinusoidal electromagnetic
waves propagating through an unmagnetized plasma have a nonlinear dispersion relation.
Moreover, this nonlinearity arises because the effective refractive index of the plasma is frequency dependent.
The expression (9.30) for the refractive index of a plasma has some rather
unusual properties. For wave frequencies lying above the plasma frequency (i.e.,
), it yields a real refractive index that is
less than unity. On the other hand, for wave frequencies lying below the plasma
frequency (i.e.,
), it yields an imaginary refractive index. Neither of these results makes much sense. The former result is problematic because if the
refractive index is less than unity then the phase velocity of the wave,
, becomes
superluminal (i.e.,
), and superluminal velocities are generally thought to be unphysical.
The latter result is problematic because an imaginary refractive index implies an
imaginary phase velocity, which seems utterly meaningless. Let us investigate further.
Consider, first of all, the high-frequency limit,
. According to
Equation (9.30), a sinusoidal electromagnetic wave of angular frequency
propagates through the plasma
at the superluminal phase velocity
. Differentiating the dispersion relation (9.27) with respect to
, we obtain
![]() |
(9.32) |
![]() |
(9.33) |
). Hence, as
long as we accept that high-frequency electromagnetic waves transmit information through a plasma at
the group velocity, rather than the phase velocity, then there is no problem with causality.
Incidentally, it follows, from this discussion, that the phase velocity of dispersive
waves has very little physical significance. It is the group velocity that matters. For instance, according to Equations (6.128), (9.29), (9.30), and (9.34), the mean flux of electromagnetic energy in
the
-direction due to a high-frequency sinusoidal wave propagating through a plasma is given by
because
and
.
Thus, if the group velocity is zero, as is the case when
, then there is zero energy flux associated with the wave.
The fact that the energy flux and the group velocity of a sinusoidal wave propagating through a plasma both go to zero when
suggests that the wave ceases to propagate at all in the low-frequency limit,
. This observation leads us to search for
spatially decaying, standing wave solutions to Equations (9.24) and (9.25) of the form,
, and also yields
as well as
(See Exercise 4.)
Furthermore, the mean
-directed electromagnetic energy flux becomes
![]() |
(9.41) |
radians out of phase), and
the wave consequentially has zero associated net energy flux. This suggests that a
plasma reflects, rather than absorbs, an incident electromagnetic wave whose frequency is less than the plasma frequency (because if the wave were absorbed
then there would be a net flux of energy into the plasma). Let us investigate what happens
when a low-frequency electromagnetic wave is normally incident on a plasma in more detail.
Suppose that the region
is a vacuum, and the region
is
occupied by a plasma of plasma frequency
. Let the wave electric and
magnetic fields in the vacuum region take the form
is the vacuum wavenumber.
Here,
is the amplitude of an electromagnetic wave of frequency
that is normally incident on the plasma, whereas
is the amplitude
of the reflected wave, and
the phase of this wave with respect to the
incident wave.
The wave electric and magnetic fields in the plasma are written
![]() |
![]() |
(9.44) |
![]() |
![]() |
(9.45) |
is the amplitude of the evanescent wave that penetrates into the
plasma,
is the phase of this wave with respect to the incident wave, and
![]() |
(9.46) |
and
at the vacuum/plasma interface (
). (See Appendix C.)
In other words,
These two equations, which must be satisfied at all times, can be solved to give
(See Exercise 5.)
Thus, the coefficient of reflection,
![]() |
(9.53) |
) to
(when
) radians.
The outer regions of the Earth's atmosphere consist of a tenuous gas that is
partially ionized by ultraviolet and X-ray radiation from the Sun, as well as by cosmic rays incident from outer space. This
region, which is known as the ionosphere, acts like a plasma
as far as its interaction with radio waves is concerned. The ionosphere
consists of many layers. The two most important, as far as radio
wave propagation is concerned, are the E layer, which lies at an altitude of
about 90 to 120 km above the Earth's surface, and the F layer, which
lies at an altitude of about 120 to 400 km (Pain 1999). The plasma frequency in the
F layer is generally larger than that in the E layer, because of the greater
density of free electrons in the former (recall that
).
The free electron number density in the
E layer drops steeply after sunset, due to the lack of solar ionization combined with the gradual recombination of free electrons
and ions. Consequently, the plasma frequency in the E layer also drops steeply after sunset. Recombination in the F layer occurs at a much slower rate, so there is nothing like
as great a reduction in the plasma frequency of this layer at night.
Very High Frequency (VHF) radio signals (i.e., signals with frequencies greater than 30 MHz), which include FM radio and TV signals, have frequencies well in excess
of the plasma frequencies of both the E and the F layers, and thus pass straight through
the ionosphere. Short Wave (SW) radio signals (i.e., signals with frequencies in the
range 3 to 30 MHz) have frequencies in excess of the plasma
frequency of the E layer, but not of the F layer. Hence, SW signals pass through the
E layer, but are reflected by the F layer.
Finally, Medium Wave (MW) radio signals (i.e., signals with frequencies in the range
to 3 MHz) have frequencies that lie below the plasma frequency of the F layer,
and also lie below the plasma frequency of the E layer during daytime, but not
during nighttime. Thus, MW signals are reflected by the E layer during the day,
but pass through the E layer, and are reflected by the F layer, during the night.
The reflection and transmission of the various different types of radio wave by the ionosphere is shown schematically in Figure 9.1. This diagram explains many of the characteristic features of radio reception. For instance, because of the curvature of the Earth's surface, VHF reception is only possible when the receiving antenna lies in the line of sight of the transmitting antenna, and is consequently fairly local in nature. MW reception is possible over much larger distances, because the signal is reflected by the ionosphere back toward the Earth's surface. Moreover, long range MW reception improves at night, because the signal is reflected at a higher altitude. Finally, SW radio reception is possible over very large distances, because the signal is reflected at extremely high altitudes.