Chemical Reactions and Phase Stabilities in the Si-Te System at High Pressures and High Temperatures

Chemical reactions and phase stabilities in the Si-Te system at high pressures were explored using in situ angle-dispersive synchrotron powder diffraction in a large-volume multianvil press together with density functional theory-based calculations. Cubic and rhombohedrally distorted clathrates, with the general formula Te-8@(Si38Te8) and wide compositional range, preceded by a hexagonal phase with the composition Si0.14Te, are formed for different mixtures of Si and Te as starting materials. Si0.14Te, with the structural formula Te-2(Te0.74Si0.26)(3)(Te0.94Si0.06)(3), is the very first chalcogenide with the Mn5Si3-type structure. Silicon sesquitelluride alpha-Si2Te3 decomposes into a mixture of phases that includes the clathrate and hexagonal phases at high pressures and high temperatures. The higher the pressure, the lower the temperature for the two phases to occur. Regardless of the starting compositions, only the clathrate is quenched to atmospheric conditions, while the hexagonal phase amorphizes on decompression. The rhombohedral clathrates Te-8@(Si38Te8) form on quenching of the cubic phases to ambient conditions. There is a high degree of interchangeability of Si and Te not only in the clathrates but also in the Mn5Si3-type structure. The theoretical calculations of enthalpies indicate that the reported decomposition of alpha-Si2Te3 is energetically favorable over its transformation to another polymorph of the A(2)X(3) type at extreme conditions.

Automated summary

This study investigated the chemical reactions and phase stabilities in the Si-Te system at high pressures using experimental and theoretical methods. The results revealed the formation of cubic and rhombohedrally distorted clathrates with a wide range of compositions, as well as the occurrence of a hexagonal phase. Additionally, it was found that Si2Te3 decomposes into multiple phases under high-pressure and high-temperature conditions. Only the clathrate structure remains stable at atmospheric conditions regardless of the starting compositions.