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L. Havela
Charles University, Prague, Czech Republic
Electron Systems: Strong Correlations
The physics of strongly correlated electron systems
originates primarily from the presence of an inner d
or f shell in one of the atoms embedded in the system
considered. The d electrons in transition elements and
the 4f or 5f electrons in rare earths or actinides are
generally well localized and correlated. The physics of
strongly correlated electron systems is the subject of
many experimental and theoretical studies and we
will summarize here the main points.
The correlations tend firstly to favor the existence
of magnetism which is because of open inner d or f
shells, as observed in pure iron, cobalt, or nickel in
the 3d series, in the rare-earth metals, and in actinide
metals after americium. Magnetism is also observed
in many ionic, insulating, or metallic systems con-
taining these magnetic elements.
The generic term of strongly correlated electron
systems is mostly reserved to metallic systems where
there exists a strong interaction or hybridization be-
tween the inner d or f electrons and the conduction
electrons. This type of physics started from the ex-
perimental observation of the resistivity minimum in
dilute alloys such as
CuFe, CuMn, LaCe, or YCe, the
theoretical concept of ‘‘virtual bound state’’ intro-
duced by Friedel (1956), 1958), the derivation of the
hybridization Anderson (1961) model, and the expla-
nation by Kondo (1964) of the resistivity minimum.
After the exact solution of the Kondo effect at low
temperatures for a single impurity (Wilson 1975),
there are many topics involved in the physics of
strongly correlated electron systems. The main topic
concerns the so-called ‘‘heavy-fermion’’ behavior ob-
served in many cerium or other anomalous rare-earth
compounds, after its first observation in CeAl
3
(And-
res et al. 1975). In the ‘‘Kondo lattice,’’ there exists a
strong competition between the Kondo single impu-
rity behavior and the magnetism, and the behavior
around the quantum critical point of the Doniach
(1977) diagram has been extensively studied.
The metal–insulator transition, introduced by the
work of Mott (1974), and the study of compounds
such as manganites are also a very important part of
this type of physics. The discovery of superconduc-
tivity in the CeCu
2
Si
2
compound by Steglich et al.
(1979), and in some cerium compounds at high pres-
sure and uranium compounds at normal pressure is
also a very noteworthy result. Strong correlations
appear to be the origin of the high T
c
superconduc-
tivity, which was discovered by Bednorz and Muller
(1986), but this question is still not answered. Finally,
the study of strongly correlated electron systems
has considerably contributed to the development of
new experimental techniques, such as high-accuracy
photoemission or related experiments, neutron scat-
tering, and NMR or muon spectroscopy, as well as to
all kinds of magnetic and transport measurements at
extremely low temperature and high pressures, and
under very large magnetic fields.
1. The Series of Rare-earth and Actinide Metals
The first systems studied that could be considered as
strongly correlated electron ones were dilute alloys
with 3d transition element impurities embedded in a
host such as copper; now the most studied systems
contain rare earths and actinides.
Most of the rare-earth metals have a magnetic
moment given by Hund’s rules (see Magnetism in
Solids: General Introduction and Localized 4f and 5f
Moments: Magnetism), corresponding to the 4f
n
(n an
integer) configuration. For example, gadolinium, in
the middle of the series, has a 4f
7
configuration with a
magnetic moment equal to 7 m
B
in the ferromagnetic
phase below the Curie temperature of 293 K, and
there is no change in the number of 4f electrons under
pressure, even a very high one. It follows that the
‘‘valence,’’ taken here as equal to the number of con-
duction electrons, remains constant and equal to 3.
Thus, most of the rare-earth metals have a stable
valence of 3 and are called ‘‘normal’’ (Coqblin 1977).
However, some rare-earth metals undergo a change
of valence under different experimental conditions
(pressure, temperature, or relative composition in
the case of alloys and compounds containing these
metals) and they are called ‘‘anomalous.’’ The best
example of the series is cerium, the first element after
lanthanum, which varies or fluctuates between the
two configurations 4f
0
and 4f
1
. Cerium metal has a
very peculiar phase diagram with several phases,
136
Electron Systems: Strong Correlations