8.2 Metallic Oxides with Polarized Spins 399
electron of the Fe
2C
3d
6
ion is loosely bound in a filled d
xy
orbital, i.e., the first
one added to the half-filled t
2g
shell, we can argue that two ionic configurations can
exist simultaneously through spin transfer reactions
Fe
3C
C Mo
5C
, Fe
2C
C Mo
6C
C U
eff
t
2g
3
e
g
2
C t
2g
1
e
g
0
, t
2g
4
e
g
2
C t
2g
0
e
g
0
C U
eff
The degree of sharing and hence the mobility of the single Mo
5C
spin will de-
pend on the relative magnitudes of U
eff
and b,whereU
eff
is the difference in the
binding energy between the initial and final states of the transfer and b is the ex-
change integral between the Fe and Mo ions mediated by the O
2
ligand (not
shown in Fig. 7b). If the single Mo
5C
spin becomes itinerant in this sense, spin-
polarized transport could take place in the narrow half-filled band constructed from
the 3d
xy
.Fe/ –2p–5d
xy
(Mo) hybrid. Inspection of the above charge-transferreac-
tions reveals that the left-hand side represents an antiferromagnet (or a quasi-ferrite)
and the right-hand side a paramagnet. Therefore, the probability of obtaining the
maximum 4m
B
is reduced by the probability of paramagnetism that occurs when
Mo
5C
is missing its t
2g
spin. If a paramagnetic contribution is present, experiments
at very high magnetic fields might help to clarify the situation.
Another point of interest is that the 3m
B
value of the net magnetic moment per
molecule lends credence to the suggestion that the Goodenough–Kanamori (G–K)
rules [9] for predicting the most probable type of spin ordering might not apply in
this case. If only the e
g
states are considered because of the conventional wisdom
that the t
2g
–p hybrids are effectively nonbonding and can be ignored, the logical
conclusion for 180
ı
¢ bonding of the perovskites is that ferromagnetic delocaliza-
tion exchange will result between the empty Mo
5C
and half-filled Fe
3C
e
g
shells,
producing magnetic moment limit of 6m
B
. However, the experimental result of 3m
B
suggests that the d
xy
–p bond of the t
2g
shell is strong enough to stabilize the type
of ferrimagnetic ordering proposed.
In a series of compositions with Cr, Mn, and Co used in place of Fe, [18] ferro-
magnetism was found only with Cr. Since it assumes its 3C valence with a highly
stable electronic configuration t
2g
3
e
g
0
, 3d
3
-d
1
antiferromagnetic (ferrimagnetic)
superexchange is again the likely result. No evidence of metallic conduction was
reported, however, which suggests that the value of U
eff
is greater than that of the
Fe case. The other ions also showed insulating properties, but no magnetic order-
ing. The prospects of antiferromagnetism are reduced because the most stable forms
of Mn and Co are divalent, which would force the Mo valence to be raised to the
diamagnetic 6C state, thereby lowering the chance of spontaneous magnetism. Sim-
ilar analysis can be applied to other combinations of transition metals, such as Ti,
W, and Re, but the prospects for strong superexchange with spin-polarized metallic
conductivity between the alternating B-site cations probably remains highest with a
d
5
–d
1
combination.
Ferromagnetism in metallic oxides also occurs with spins in the e
g
shell of
the mixed-valence perovskite
La
3C
1x
Ca
x
2C
Mn
3C
1x
Mn
x
4C
O
3
, for temperatures
reaching above 300 K. The origins of this ferromagnetism are complex and are