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Updated: Jun 13, 2025

High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
Columbite Single-Crystal CoV2O6 under High Pressure: An XRD and Raman Spectroscopy Study
Josu Sánchez-Martín1, Pierre Bouvier2, Gaston Garbarino3
1Departamento de Física Aplicada-ICMUV, Universidad de Valencia, Dr. Moliner 50, Burjassot, Valencia 46100, Spain.
High pressure induces two phase transitions in orthorhombic columbite cobalt vanadate (CoV2O6). These reversible transitions involve structural changes and volume reductions, detailed by X-ray diffraction and Raman spectroscopy.
Area of Science:
- Materials Science
- Solid State Physics
- Crystallography
Background:
- Orthorhombic columbite CoV2O6 is a material with potential applications.
- Understanding its behavior under extreme conditions is crucial for materials science.
Purpose of the Study:
- To investigate the structural and vibrational properties of orthorhombic columbite CoV2O6 under high pressure.
- To identify and characterize phase transitions induced by pressure.
Main Methods:
- Single-crystal X-ray diffraction (XRD) up to 54.9 GPa.
- Raman spectroscopy up to 54.9 GPa.
- Density functional theory (DFT) calculations.
Main Results:
- Two reversible phase transitions were observed at 20.0 GPa and 45.6 GPa.
- The first transition (20.0 GPa) is isostructural with a 4.7% volume reduction and symmetrization of VO6 octahedra.
- A new monoclinic polymorph (space group P21/c) was identified above 45.6 GPa.
- Below 4.9 GPa, the material transforms into the brannerite polymorph.
Conclusions:
- High pressure significantly alters the structure of CoV2O6, leading to distinct polymorphs.
- The observed transitions are reversible, with complex behavior upon pressure release.
- Experimental findings are consistent with theoretical DFT calculations.
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