
8.9 Nonreciprocal Media 537
magnetic field without an electric field rotates at an angular frequency ω
c
,
so an applied alternating electric field oscillates at ω
c
continually pumps the
electron to higher and higher velocities and leads to the infinite response.
The collisions of electrons with ions and molecules limit the amplitude of the
oscillation and give rise to an absorption of the wave.
The cyclotron frequency of a plasma in a strong d-c magnetic field is in the
range of GHz, i.e., in the microwave to millimeter wave band. Hence cyclotron
resonance can be an effective technique for producing high-temperature
plasma by means of microwave energy. This is an important technique in
the experimental facilities to realize controlled nuclear fusion.
The ionosphere around the Earth is another example of a magnetized
plasma. The geomagnetic field strength is about 3 × 10
−5
T (0.3 Gauss), so
f
c
≈ 6 MHz, which is beyond the high end of the medium-wave broadcasting
band. The waves in the adjacent band of this frequency are strongly absorbed
in the ionosphere and are scarcely used in communication and broadcasting
purposes, but they are suitable for ionosphere explorations.
If the d-c magnetic field approaches infinity, then ω
c
= (e/m)B
0
→ ∞,
and
²
1
= ²
0
, ²
2
= 0, ²
3
= ²
0
µ
1 −
ω
2
p
ω
2
¶
.
This is the same as (8.228) given in the last section, and the medium becomes
reciprocal.
If the d-c magnetic field approaches zero, ω
c
→ 0, or the frequency of the
applied alternating field is much larger than the cyclotron frequency of the
plasma, ω À ω
c
, the medium becomes isotropic:
²
2
= 0, ²
1
= ²
3
= ²
0
µ
1 −
ω
2
p
ω
2
¶
.
This is the same as the result given in Section 8.1.7.
8.9.2 Saturated-Magnetized Ferrite, Gyromagnetic
Media
Ferrites or ferrimagnetic materials are a group of materials that have strong
magnetic effects and low loss up to microwave frequencies. Ferrites are
ceramic-like materials with a high resistivity that may be as much as 10
14
greater than that of metals, with relative permittivities around 8 to 15 or
greater, and with relative permeability as high as several thousand. Ferrites
are made by sintering a mixture of metallic oxides and have the general com-
position MO·Fe
2
O
3
, where M is a divalent metal such as Mn, Mg, Fe, Zn, Ni,
Cd, etc., or a mixture of them. The details of the structure and performance
of ferrites are described in reference [57]. The most recent development in
the area of ferrimagnetic material is the single-crystal ferrite, mainly yttrium
iron garnet (YIG), which has much lower loss in the microwave band.