
Valence and magnetism in EuPd3S4and (Y,La)xEu1−xPd3S4
D. H. Ryan
Physics Department and Centre for the Physics of Materials, McGill University,
3600 University Street, Montreal, Quebec, H3A 2T8, Canada
Sergey L. Bud’ko, Brinda Kuthanazhi, and Paul C. Canfield
Ames National Laboratory, and Department of Physics and Astronomy, Iowa State University, Ames, Iowa 50011, USA
(Dated: October 11, 2022)
151Eu M¨ossbauer spectroscopy shows that yttrium substitution in mixed-valent EuPd3S4drives
the initial 50:50 mix of Eu3+ and Eu2+ towards pure Eu2+, whereas lanthanum substitution has the
opposite effect, but only for substitution levels above 50%. We find that total valence electron count
and chemical pressure effects cannot account for the observed behaviour, however conserving the
cell volume provides a consistent description of the changes in the Eu2+:Eu3+ ratio. Remarkably,
lanthanum substitution also leads to a clear transition from static mixed-valent behavior at lower
temperatures to dynamic mixed valent behavior at higher temperatures, with the onset temperature
monotonically increasing with Eu content and extrapolating to a value of ∼340 K for the pure
EuPd3S4compound. Magnetic order persists at least as far as x=0.875 in both series, despite the
drastic reduction in the amount of moment-carrying Eu2+ ions.
I. INTRODUCTION
The rare earth palladium sulphides RPd3S4have been
reported for the majority of the rare earths, including
yttrium1–4. They all crystallise in the cubic NaPt3O4
structure (P m3n#223) with the rare earth occupying
the 2asite forming a bcc sublattice, the palladium on
the 6dsite and the sulphur on the 8esite. Remark-
ably, although the RPd3S4phases exist for the trivalent
rare earths, but apparently not for the divalent alkaline
earths (Ca and Sr), when prepared with europium5or
ytterbium4a roughly 50:50 mix of divalent and trivalent
rare earth is found.
Here we will use chemical substitution of yttrium and
lanthanum for europium to investigate the stability of the
valence distribution and its effects on magnetic ordering.
Although both 170Yb and 151Eu M¨ossbauer spectroscopy
can generally be used to identify the valence of their re-
spective target ions, for 170Yb M¨ossbauer spectroscopy,
the isomer shift between the two valence states is ex-
tremely small so the technique is almost totally depen-
dent on the presence of an electric field gradient (efg)
at the Yb3+ ions to identify trivalent ytterbium. Un-
fortunately the high symmetry of the 2asite makes the
efg contribution effectively zero and the presence of the
Yb3+ ions is only apparent in the magnetically ordered
state well below TN∼2 K4. We will therefore only study
EuPd3S4using 151Eu M¨ossbauer spectroscopy where the
two valence states are clearly isolated by a large differ-
ence in isomer shift, even at ambient temperatures.
We find that, by substituting Y for Eu, the remaining
Eu sites become more and more divalent. In contrast,
by substituting La for Eu we find that, initially, the re-
maining Eu sites stay roughly a 50:50 mixture of di- and
tri-valent Eu, but for higher La substitution levels the re-
maining Eu rapidly becomes more trivalent. La substitu-
tion also leads to a transition from statically mixed valent
behavior at lower temperatures to dynamically mixed
valent behavior at higher temperatures with the onset
temperature (Tonset) monotonically increasing with Eu
content and passing through room temperature as pure
EuPd3S4is approached. Despite the decreasing fraction
of moment-carrying Eu2+ ions, both YxEu1−xPd3S4and
LaxEu1−xPd3S4continue to exhibit some form of mag-
netic order at least as far as x=0.875, with transition
temperatures of ∼3 K (Y) and ∼6 K (La).
II. EXPERIMENTAL METHODS
Polycrystalline samples of EuPd3S4and
(Y,La)xEu1−xPd3S4were prepared from stoichio-
metric mixtures of EuS (99.9% – American Elements)
Y2S3(99.9%), La2S3(99%), Pd (99.95%) and S (99.5%),
all from Alfa-Aesar. The powders were mixed and
then pressed to form a dense pellet. This was loaded
into an alumina crucible and sealed under a partial
pressure of helium in a fused silica tube. The sample
was heated to 650◦C over three hours, held for an hour
and then taken to 900◦C over a further three hours.
After 75 hours at 900◦C the sample was furnace cooled
and removed once it reached ambient temperature. In
most cases this single thermal cycle was found to yield
a single-phased product, however when an impurity
was found (typically PdS seen by x-ray diffraction or
EuS seen in susceptibility vs. temperature) the sample
was crushed, pressed and subjected to a second 75 hr
annealing cycle to 900◦C to remove the impurity.
X-ray diffraction measurements were made on a
Rigaku Miniflex-II diffractometer using a Cu-Kαsource.
The instrument calibration was checked using NIST 676a
Al2O3and found to be consistent within fitted uncertain-
ties. Full Rietveld refinement of the diffraction pattens
was carried out using the GSAS/EXPGUI packages6,7.
As all three species occupy special sites in the P m3n
structure, no positional parameters were adjusted dur-
arXiv:2210.03860v1 [cond-mat.mtrl-sci] 8 Oct 2022