2.3 Crystal Electric Fields 55
by the crystal fields. Moreover, only the ground terms need to be considered for
interpreting most magnetic effects. These operations and their implications on the
magnetic properties will be the main topic of this text.
The “strong field” second case is also important, perhaps more for the high-
energy transitions to be examined in a later discussion of magneto-optical proper-
ties. It is analytically more challenging than the “weak field” case because the H
cf
magnitudes are equal or greater than the free-ion term splittings set by H
Hund
and
are therefore strong enough to mix the starting orbital terms prior to the removal of
their degeneracies. As a result, the various possible electron distributions among the
individual d orbital states, that is, the excited states, must be included as separate
energy levels prior to application of the symmetry constraints imposed by the H
cf
operator. The strong field situation is sometimes referred to as the covalent limit
because the strong H
cf
potential energy is produced by the overlap of the cation and
anion orbital lobes. It is more common among the 4d
n
and 5d
n
transition series ions
with larger ionic radii, but can also apply in the 3d
n
series when the anion complex
provides a locally stronger crystal field than that of the standard O
2
coordinations.
In certain cases the crystal-field splitting can be large enough to cause a breakdown
in Hund’s maximum S rule by producing what is called a “low-spin” state that then
leads to a change in the orbital ground term.
The third is the rare-earth 4f
n
case, in which the Stark effect of the crystal field
is not great enough to decouple L from S because of the shielding by the filled
5s
2
and 5p
6
shells. Here, œL S remains a constant of the motion and the H
LS
operation creates the various multiplet terms now identified by
2SC1
L
j
,whereL
represents the orbital angular momentum of the orbital term designated by S, P, D,
F, G, etc, with respective values of L being 0, 1, 2, 3, 4. For the rare earths, the
total angular momentum J and its specific g value as defined by (1.29), rather than
simply S with its fixed g D 2, determine the individual ion contributions to the
magnetic properties.
2.3.4 Weak-Field Solutions
The subject of crystal field theory has been presented in many excellent texts [3–5].
Historically, the seminal work was carried out by Kramers [8], Van Vleck [9], and
Schlapp and Penney [10], who treated the combined effects of the various lattice
charges at a given cation site as the result of repulsive electrostatic fields from neg-
ative point charges that represent the effects of the anions or ligands. Because the
potential V
cryst
at the cation site from the assembly of neighboring charges satisfies
Laplace’s equation r
2
V
cf
D 0, H
cf
.DeV
cf
/ may be expressed as an expansion of
generalized Legendre polynomials, which take the same familiar form of spherical
harmonics comprising (2.2). The problem of applying quantum perturbation theory
to determine the electronic states of the cation in a particular crystal field is then
reduced to the solving of a secular equation,