J. Linden et al., PRECISE DETERMINATION OF THE HYPERFINE PARAMETERS OF EUROPIUM IN MULTIFLUORITE PEROVSKITES BY EU-151 MOSSBAUER-SPECTROSCOPY, Physical review. B, Condensed matter, 49(21), 1994, pp. 15280-15286
The hyperfine interactions at the europium lattice sites in samples of
the homologous (Fe,Cu)Sr2(Eu,Ce)nCu2O4+2n+z (n = 2,3) series were stu
died by Eu-151 Mossbauer spectroscopy. The work was motivated by the s
earch for new superconducting phases. This homologous series is based
on the YBa2Cu3O7-delta (1:2:3) structure. The samples used in the Moss
bauer measurements consisted of crystallites with random orientation a
nd grain oriented crystallites. The texture of oriented samples was an
alyzed by x-ray diffraction. The complete quadrupole Hamiltonian of th
e 21.5-keV gamma-transition of Eu-151 was successfully applied in the
analyses of all the Mossbauer spectra. In samples having n less-than-o
r-equal-to 2 the europium atoms occupy a single lattice site, whereas
the spectra of the n = 3 samples exhibit hyperfine interactions of the
two different europium sites. Analyzing the hyperfine parameters of t
he latter samples was made possible by simultaneous fitting of three s
pectra, corresponding to three different crystal orientations of the s
ame specimen. This fitting scheme also enables more precise determinat
ion of the hyperfine parameters in the n = 2 samples. In these samples
an electric field gradient (EFG), with a large negative-valued main c
omponent (V(zz)) parallel with the crystal c axis, was found. In the n
= 3 samples, the two EFG's of the europium sites were found to have V
(zz) components of opposite signs. The negative V(zz) value was attrib
uted to the rare-earth site adjacent to the CuO layer. This site, foun
d in all samples of the series, corresponds to the rare-earth site of
the 1:2:3 system.