to T ¼ y
c
, the M/M
s
value corresponding to the intersection can be found,
leading to Fig. 9.7 which shows good agreement with experiment for iron, cobalt
and nickel.
According to the Weiss theory just outlined, ferromagnetism is caused by a
strong internal magnetic field aligning the magnetic moments on individual ions.
The physical origin of the internal field is now known to be quantum mechanical
in nature and to involve the ‘exchange forces’ which determine the relative
orientation of the spins on adjacent electrons. The exchange energy arising from
exchange forces plays a dominating role in determining the nature of the
important magnetic materials. In some instances, e.g. the metals iron, cobalt and
nickel, the exchange energy is minimized for parallel spins; this is exceptional
since, generally, the exchange energy is minimized when adjacent spins are
antiparallel. In the non-metallic antiferromagnetics and ferrites the ordering is
antiparallel through superexchange forces, so-called because they act between
the spins of neighbouring cations with the involvement of an intermediate ion
which, in the case of the ferrites, is oxygen.
9.1.7 Magnetocrystalline anisotrophy
A spinning electron, free from any restraints, can be aligned by an infinitely small
field, implying an infinite permeability. A restraint leading to finite permeabilities
in magnetic materials is caused by a coupling between the spins and the crystal
lattice through the agency of the orbital motion of the electron. This spin–orbit
lattice coupling results in orientation of the spins relative to the crystal lattice in a
minimum energy direction, the so-called ‘easy direction’ of magnetization.
Aligning the spins in any other direction leads to an increase in energy, the
anisotropy energy E
K
. For a cubic lattice, such as a spinel, E
K
is related to two
anisotropy constants K
1
and K
2
by
E
K
¼ K
1
ða
2
1
a
2
2
þ a
2
2
a
2
3
þ a
2
3
a
2
1
ÞþK
2
a
2
1
a
2
2
a
2
3
ð9:28Þ
where a
1
, a
2
and a
3
are the direction cosines of the magnetization vector relative
to the crystallographic axes.
The approximate expression for E
K
(Eq. (9.28)) leaves out all but two of the
terms of an infinite power series, and even the term involving K
2
can often be
safely neglected. If it is assumed that K
2
is negligible and K
1
is positive, then E
K
has a minimum value of zero if any two of the direction cosines are zero, i.e. the
anisotropy energy is a minimum along all three crystal axes and these are
therefore the ‘easy’ directions. If K
1
is negative, the minimum occurs for
a
1
¼ a
2
¼ a
3
¼ 1=
p
3, i.e. the body diagonal is the ‘easy’ direction.
The anisotropy constants listed in Table 9.1, which anticipate the discussion of
ferrites (Section 9.2 et seq.), indicate that the easy directions for cubic crystals are
[111] except for those containing cobalt, in which case they are [100]. For
MAGNETIC CERAMICS: BASIC CONCEPTS 481