8 Mössbauer Spectroscopy in External Magnetic Fields
411
Fig. 8.29 Mössbauer
spectra for Pr 0.73 Fe 4 Sb 12 at
4.2 K and different applied
fields [92]. Reprinted from
J. Mag. Mag. Matter,
272–276, M. Reissner, E.
Bauer, W. Steiner, P. Rogl,
High field Mössbauer and
magnetic investigations of
Pr 0.73 Fe 4 Sb 12 , 813.
Copyright (2004), with
permission from Elsevier
The obtained induced hyperfine fields are similar to the ones for the RE skutterudites (Fig. 8.35). They all are less than 2 T. These values are too low to explain
directly the effective moment assigned to the (Fe 4 Sb 12 ) blocks from bulk magnetic
measurements at high temperatures. Charge counting arguments that the moments on
the (Fe 4 Sb 12 ) blocks are due to the unpaired spins of Fe
3+ in low spin configuration
[76] are therefore wrong. The results support the picture of itinerant ferromagnetism
with small ordered moments for the investigated di- and monovalent skutterudites. In
summary, with the help of the in-field Mössbauer measurements it could be shown,
that the magnetic structure is much more complex than expected from the simple
crystallographic structure.
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