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Electromagnetic Waves
Consider a plane electromagnetic wave propagating through a vacuum in the
-direction. Electromagnetic waves are, incidentally, the only
commonly occurring waves which do not require a medium through which to
propagate.
Suppose that the wave is polarized in the
-direction: i.e., its electric
component oscillates in the
-direction. It follows that the magnetic
component of the wave oscillates in the
-direction. According to standard electromagnetic theory, the wave is
described by the following pair of coupled partial differential equations:
where
is the electric field-strength, and
is the
magnetic intensity (i.e., the magnetic field-strength divided by
). Observe that Equations (458) and (459), which govern
the propagation of electromagnetic waves through a vacuum, are analogous
to Equations (402) and (403), which govern the propagation of
electromagnetic signals down a transmission line. In particular,
has units of
voltage over length,
has units of current over length,
has
units of capacitance per unit length, and
has units of
inductance per unit length.
Equations (458) and (459) can be combined to give
It follows that the electric and the magnetic components of an electromagnetic wave
propagating through a vacuum both separately satisfy
a wave equation of the form (351). Furthermore, the phase velocity of the
wave is clearly
 |
(462) |
Let us search for a traveling wave solution of (458) and (459), propagating in the
positive
-direction, whose electric component has the form
 |
(463) |
As is easily demonstrated, this is a valid solution provided that
. According to
(458), the magnetic component of the wave is written
 |
(464) |
where
 |
(465) |
and
is the impedance of free space [see Equation (420)].
Thus, the electric and magnetic components of an electromagnetic wave propagating through a vacuum are mutually perpendicular,
and also perpendicular to the direction of propagation. Moreover, the two components
oscillate in phase (i.e, they have simultaneous maxima and zeros), and
the amplitude of the magnetic component is that of the electric component
divided by the impedance of free space.
Multiplying (458) by
, (459)
by
, and adding the two resulting expressions, we obtain the
energy conservation equation
 |
(466) |
where
 |
(467) |
is the electromagnetic energy per unit volume of the wave, whereas
 |
(468) |
is the wave electromagnetic energy flux (i.e., power per unit area) in the positive
-direction. The mean energy flux associated with the
-directed electromagnetic wave specified
in Equations (463) and (464) is thus
 |
(469) |
For a similar wave propagating in the negative
-direction, it is easily
demonstrated that
and
 |
(472) |
Consider a plane electromagnetic wave, polarized in the
-direction, which
propagates in the
-direction through a transparent dielectric medium, such as glass or water. As is well known, the electric component of the wave causes the neutral molecules making
up the medium to polarize: i.e., it causes a small separation to develop between the mean positions of the positively
and negatively charged constituents of the molecules (i.e., the atomic nuclii and the
electrons). (Incidentally, it is easily
shown that the magnetic component of the wave has a negligible influence on the
molecules, provided that the wave amplitude is sufficiently small that the wave electric
field does not cause the electrons and nuclii to move with relativistic velocities.) Now, if the mean position of the positively charged
constituents of a given molecule, of net charge
, develops a vector displacement
with respect to the mean position of the negatively charged constituents, of net charge
, in response to a wave electric field
then the
associated electric dipole moment is
, where
is generally parallel to
. Furthermore, if there are
such molecules per unit volume then the dipole moment per unit volume
is written
. Now, in a conventional dielectric medium,
 |
(473) |
where
is a dimensionless quantity, known as the relative dielectric
constant, which is a property of the medium in question. In the presence of a
dielectric medium, Equations (458) and (459) generalize to give
When combined with Equation (473), these expressions yield
It can be seen that the above equations are just like the corresponding vacuum equations,
(458) and (459), except that
has been replaced by
. It immediately follows that the phase velocity of an
electromagnetic wave propagating through a dielectric medium is
 |
(478) |
where
is the velocity of light in vacuum, and
the quantity
 |
(479) |
is known as the refractive index of the medium. Thus, an electromagnetic
wave propagating through a transparent dielectric medium does so at a
phase velocity which is less than the velocity of light in vacuum by a
factor
(where
). Furthermore, the impedance of a transparent dielectric medium becomes
 |
(480) |
where
is the impedance of free space.
Suppose that the plane
forms the boundary between two transparent dielectric
media of refractive indices
and
. Let the first medium occupy the
region
, and the second the region
. Suppose that a plane electromagnetic
wave, polarized in the
-direction, and propagating in the positive
-direction, is launched toward the boundary
from a wave source of angular frequency
situated at
. Of course, we expect the
wave incident on the boundary to be partly reflected, and partly transmitted.
The wave electric and magnetic fields in the region
are written
where
is the amplitude of (the electric component of) the incident wave,
the amplitude of the reflected wave,
, and
.
The wave electric and magnetic fields in the region
take the form
where
is the amplitude of the transmitted wave,
, and
.
According to standard electromagnetic theory, the appropriate matching conditions at the
boundary (
) are simply that
and
both be continuous. Thus,
continuity of
yields
 |
(485) |
whereas continuity of
gives
 |
(486) |
since
.
It follows that
The coefficient of reflection,
, is defined as the ratio of the reflected to the incident energy
flux, so that
 |
(489) |
Likewise, the coefficient of transmission,
, is the ratio of the
transmitted to the incident energy flux, so that
 |
(490) |
It can be seen, first of all, that if
then
and
.
In other words, if the two media have the same indices of refraction then
there is no reflection at the boundary between them, and the transmitted
wave is consequently equal in amplitude to the incident wave. On the other
hand, if
then there is always some reflection at the boundary. Indeed,
the amplitude of the reflected wave is roughly proportional to the difference between
and
. This has important practical consequences.
We can only see a clean pane of glass in a window because some of the light incident
on an air/glass boundary is reflected, due to the different refractive indicies
of air and glass. As is well known, it is a lot more difficult to see glass when it is submerged in water. This is because the refractive indices of glass and water are quite similar, and so there is very little reflection of light
incident on a water/glass boundary.
According to Equation (487),
when
.
The negative sign indicates a
radian phase shift of the (electric component of the) reflected wave, with
respect to the incident wave. We conclude that there is a
radian phase shift of the reflected wave, relative to the incident wave, on reflection from a boundary with a
medium of greater refractive index. Conversely, there is no
phase shift
on reflection from a boundary with a medium of lesser refractive index.
Note that Equations (487)-(490) are analogous to Equations (429)-(432), with refractive index playing the role of
impedance. This suggests, by analogy with earlier analysis, that we
can prevent reflection of an electromagnetic wave normally incident at a boundary between two
transparent dielectric media of different refractive indices by separating the media
by a thin transparent layer whose thickness is one quarter of a wavelength, and whose
refractive index is the geometric mean of the refractive indices of the two
media. This is the physical principle behind the non-reflective lens coatings used
in high-quality optical instruments.
Next: Exercises
Up: Traveling Waves
Previous: Reflection and Transmission at
Richard Fitzpatrick
2010-10-11