The chemical accessibility
of the CeIV oxidation state
enables redox chemistry to be performed on the naturally coinage-metal-deficient
phases CeM1–
x
SO (M
= Cu, Ag). A metastable black compound with the PbFCl structure type
(space group P4/nmm: a = 3.8396(1) Å, c = 6.607(4) Å, V = 97.40(6) Å3) and a composition approaching
CeSO is obtained by deintercalation of Ag from CeAg0.8SO.
High-resolution transmission electron microscopy reveals the presence
of large defect-free regions in CeSO, but stacking faults are also
evident which can be incorporated into a quantitative model to account
for the severe peak anisotropy evident in all the high-resolution
X-ray and neutron diffractograms of bulk CeSO samples; these suggest
that a few percent of residual Ag remains. A straw-colored compound
with the filled PbFCl (i.e., ZrSiCuAs- or HfCuSi2-type)
structure (space group P4/nmm: a = 3.98171(1) Å, c = 8.70913(5) Å, V = 138.075(1) Å3) and a composition close
to LiCeSO, but with small amounts of residual Ag, is obtained by direct
reductive lithiation of CeAg0.8SO or by insertion of Li
into CeSO using chemical or electrochemical means. Computation of
the band structure of pure, stoichiometric CeSO predicts it to be
a Ce4+ compound with the 4f-states lying approximately
1 eV above the sulfide-dominated valence band maximum. Accordingly,
the effective magnetic moment per Ce ion measured in the CeSO samples
is much reduced from the value found for the Ce3+-containing
LiCeSO, and the residual paramagnetism corresponds to the Ce3+ ions remaining due to the presence of residual Ag, which presumably
reflects the difficulty of stabilizing Ce4+ in the presence
of sulfide (S2–
). Comparison of the
behavior of CeCu0.8SO with that of CeAg0.8SO
reveals much slower reaction kinetics associated with the Cu1–
x
S layers, and this enables
intermediate CeCu1–
x
Li
x
SO phases to be isolated.