Pressure-Induced Phase Transitions in Bismutotantalite (BiTaO): Insights from Single-Crystal Diffraction and Raman Spectroscopy.

Inorg Chem

Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China.

Published: March 2025

In situ high-pressure single-crystal X-ray diffraction and Raman spectroscopy analyses were performed on a natural bismutotantalite with an α-BiTaO structure. The results indicate that α-BiTaO transforms into an orthorhombic phase (HP γ-BiTaO), likely through an intermediate orthorhombic phase (HP β-BiTaO). The transition pressures are 11.0-11.8 GPa for α-BiTaO → HP β-BiTaO and 13.9-14.4 GPa for HP β-BiTaO → HP γ-BiTaO transition. The phase transitions are reversible. Although the structure of HP β-BiTaO was not successfully solved, the possible space group was determined to be 2, with unit-cell parameters calculated at 12.2 GPa: = 4.8158(18) Å, = 33.8880(80) Å, = 5.2910(5) Å. In contrast, the structure of HP γ-BiTaO was successfully solved and refined at 28.0 GPa, revealing a space group and unit-cell parameters of = 9.8999(12) Å, = 5.0435(16) Å, = 10.8331(8) Å. The significant volume collapse of 6.2% through the phase transition and the increase in coordination numbers of Bi and Ta from 6 in α-BiTaO to 8/9 in HP γ-BiTaO indicate that the HP γ-BiTaO structure is considerably more compacted. Additionally, the equation of state for both α-BiTaO and HP γ-BiTaO was also studied.

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http://dx.doi.org/10.1021/acs.inorgchem.5c00260DOI Listing

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