A Low Temperature Structural Transition in Canfieldite, Ag$_8$SnS$_6$, Single Crystals
Tyler J. Slade, Volodymyr Gvozdetskyi, John M. Wilde, Andreas, Kreyssig, Elena Gati, Lin-Lin Wang, Yaroslav Mudryk, Raquel A. Ribeiro,, Vitalij K. Pecharsky, Julia V. Zaikina, Sergey L. Budko, Paul C. Canfield

TL;DR
This study reports the discovery of a low temperature structural transition in canfieldite (Ag$_8$SnS$_6$), revealing a new orthorhombic phase at 120 K and exploring its kinetic arrest and relation to similar compounds.
Contribution
The paper uncovers a second, low-temperature orthorhombic phase in Ag$_8$SnS$_6$ and analyzes its structural and kinetic properties, expanding understanding of phase behavior in related argyrodite compounds.
Findings
A second orthorhombic phase appears at 120 K with large hysteresis.
The room temperature phase can be kinetically arrested into a metastable state.
Transition to the Pmn2$_1$ phase is suppressed in Ge-alloyed samples.
Abstract
Canfieldite, AgSnS, is a semiconducting mineral notable for its high ionic conductivity, photosensitivity, and low thermal conductivity. We report the solution growth of large single crystals of AgSnS of mass up to 1 g from a ternary Ag-Sn-S melt. On cooling from high temperature, AgSnS undergoes a known cubic (F-43m) to orthorhombic (Pna2) phase transition at 460 K. By studying the magnetization and thermal expansion between 5-300 K, we discover a second structural transition at 120 K. Single crystal X-ray diffraction reveals the low temperature phase adopts a different orthorhombic structure with space group Pmn2 (a = 7.6629(5) \AA, b = 7.5396(5) \AA, c = 10.6300(5) \AA, Z = 2 at 90 K) that is isostructural to the room temperature forms of the related Se-based compounds AgSnSe and AgGeSe. The 120 K transition is…
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Taxonomy
TopicsGeochemistry and Geologic Mapping
