6. Crystal Field Spectroscopy
The limitation of the PCS as a spectroscopic tool is due to the fact that the
contact diameter has to be smaller than the inelastic electron mean free path,
which is hardly fulfilled in most of the strongly correlated electron systems, so
that the data analysis becomes ambiguous and complicated. Moreover, the
PCS technique cannot discriminate a priori between crystal field and electron-
phonon interactions, i.e., a proper identification of the observed PCS spectra
strongly relies on the availability of other spectroscopic data.
6.4 DETERMINATION OF CRYSTAL FIELD
PARAMETERS FROM EXPERIMENTAL DATA
In this section we present a simple crystal field problem in order to exemplify
the way in which the crystal field parameters can be determined from
spectroscopic data. We choose the insulating compound series Cs
2
NaRBr
6
(R = rare earth) called (bromo-)elpasolites, which were investigated by
several experimental techniques, so that we can compare the results and
thereby obtain information about the performance of the different
experimental methods.
The crystal field is the dominant interaction for the rare earth elpasolites,
since no magnetic ordering is observed down to the lowest temperatures, thus
exchange effects can be neglected. Moreover, the elpasolites have a cubic
crystal structure with the R
3+
ions situated at the sites of octahedral symmetry,
i.e., each R
3+
ion is hexacoordinated by six nearest Br
–
ions. Thus the crystal
field problem is rather simple with only two independent crystal field
parameters (see equation (6.9)).
Figures 6.9 and 6.10 show the results of neutron spectroscopic
investigations for Cs
2
NaErBr
6
(J
Er
=
15
/
2
) [25]. The cubic crystal field splits the
16-fold degenerate ground state
4
I
15/2
-multiplet of the Er
3+
ion into two
doublets
*
6
and *
7
and three quartets *
8
(1)
, *
8
(2)
,
and
*
8
(3)
. The low-
temperature spectra of Figure 6.9 give evidence for two inelastic lines A and
B at 3.0 and 5.8 meV, respectively, that can be attributed to crystal field
transitions out of the ground state. Upon raising the temperature the intensity
of line B decreases as expected (because of the decreasing Boltzmann
population factor), whereas the intensity of line A increases slightly because
of an excited crystal field transition that occurs accidentally at the same
energy. For Er
3+
the higher lying crystal field states usually have very small
matrix elements for transitions out of the ground state, thus their energies can
be determined only in connection with excited-state transitions. This is
demonstrated in Figure 6.10 by lines C and D at 21 and 25 meV, respectively,
whose intensities clearly increase with increasing temperature.
6.4.1 A Simple Two-Parameter Crystal Field Problem
280