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High-Pressure Single-Crystal X-Ray Diffraction Study of ErVO4
Josu Sánchez-Martín1, Gastón Garbarino2, Samuel Gallego-Parra2
1Departamento de Física Aplicada-ICMUV, MALTA Consolider Team, Universidad de Valencia, Dr. Moliner 50, Burjassot, 46100 Valencia, Spain.
Inorganic Chemistry
|February 28, 2025
Summary
Erbium vanadate (ErVO4) transforms from zircon to scheelite structure at 7.9 GPa. This study precisely maps its structural changes and mechanical properties under high pressure, revealing no phase coexistence or predicted transitions.
Area of Science:
- Solid-state chemistry
- Materials science
- Crystallography
Background:
- Understanding the high-pressure behavior of rare-earth vanadates is crucial for materials science.
- Erbium vanadate (ErVO4) is a material with potential applications influenced by its structural phase transitions.
Purpose of the Study:
- To investigate the crystal structure evolution of ErVO4 under variable pressure.
- To precisely determine the phase transition pressure and equation of state.
- To investigate mechanical properties and compare experimental findings with theoretical predictions.
Main Methods:
- High-pressure single-crystal X-ray diffraction using helium as a pressure medium.
- Structure refinements up to 24.1 GPa.
- Density-functional theory calculations for mechanical properties.
Main Results:
- Observed a phase transition from zircon to scheelite structure at 7.9(1) GPa.
- No evidence of phase coexistence was detected, contrary to some previous reports.
- Determined precise linear compressibility and pressure-volume equation of state for both phases.
- Calculated mechanical properties using density-functional theory.
Conclusions:
- The zircon-to-scheelite transition in ErVO4 occurs at 7.9 GPa without phase coexistence.
- Experimental results provide accurate data on compressibility and equation of state.
- Discrepancies with theoretical predictions regarding secondary phase transitions were noted.
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