The structural transformation generally
occurs from lower symmetric
to higher symmetric structure on heating. However, the formation of
locally broken asymmetric phases upon warming has been evidenced in
PbQ (Q = S, Se, Te), a rare phenomenon called emphanisis, which has significant effect on their thermal transport and thermoelectric
properties. (SnSe)0.5(AgSbSe2)0.5 crystallizes in rock-salt cubic average structure, with the three
cations occupying the same Wycoff site (4a) and Se in the anion position
(Wycoff site, 4b). Using synchrotron X-ray pair distribution function
(X-PDF) analysis, herein, we show the gradual deviation of the local
structure of (SnSe)0.5(AgSbSe2)0.5 from the overall cubic rock-salt structure with warming, resembling
emphanisis. The local structural analysis indicates that Se atoms
remain in off-centered position by a magnitude of ∼0.25 Å
at 300 K along the [111] direction and the magnitude of this distortion
is found to increase with temperature resulting in three short and
three long M–Se bonds (M = Sn/Ag/Sb) within the average rock-salt
lattice. This hinders phonon propagation and lowers the lattice thermal
conductivity (κlat) to 0.49–0.39 W/(m·K)
in the 295–725 K range. Analysis of phonons based on density
functional theory (DFT) reveals significant soft modes with high anharmonicity
which involve localized Ag and Se vibrations primarily. Emphanisis
induced low κlat and favorable electronic structure
with multiple valence band extrema within close energy concurrently
give rise to a promising thermoelectric figure of merit (zT) of 1.05
at 706 K in p-type carrier optimized Ge doped new rock-salt phase
of (SnSe)0.5(AgSbSe2)0.5.