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Polymorphism in Strontium Tungstate SrWO4 under Quasi-Hydrostatic Compression.
David Santamaria-Perez1, Daniel Errandonea1, Placida Rodriguez-Hernandez2
1Departamento de Física Aplicada-ICMUV, Universidad de Valencia , MALTA Consolider Team, Edificio de Investigación, C/Dr. Moliner 50, E-46100 Burjassot, Valencia, Spain.
Strontium tungstate (SrWO4) undergoes four structural changes under high pressure, revealing new polymorphs and phase transitions up to 46 GPa. These findings clarify its high-pressure behavior and structural evolution.
Area of Science:
- Materials Science
- Solid State Physics
- Crystallography
Background:
- Strontium tungstate (SrWO4) is a material with potential applications in various fields.
- Understanding its structural behavior under extreme conditions is crucial for predicting its properties.
- Previous studies have explored its properties, but a comprehensive understanding of its high-pressure phases is lacking.
Purpose of the Study:
- To investigate the structural and vibrational properties of SrWO4 under high pressure.
- To identify and characterize the polymorphs and phase transitions of SrWO4 up to 46 GPa.
- To elucidate the structural mechanism of pressure-induced transformations in SrWO4.
Main Methods:
- Angle-dispersive synchrotron X-ray diffraction (XRD) up to 27 GPa.
- Raman spectroscopy measurements up to 46 GPa.
- Ab initio calculations to support experimental findings and predict theoretical phases.
Main Results:
- Four polymorphs of SrWO4 were identified under quasi-hydrostatic compression.
- Three distinct phase transitions were observed at 11.5 GPa, 19.0 GPa, and 39.5 GPa.
- The ambient scheelite-type structure transforms to a monoclinic fergusonite-type structure at 11.5 GPa, followed by other monoclinic and orthorhombic phases.
Conclusions:
- The fergusonite-type phase acts as a structural bridge between low- and high-pressure phases.
- The study reveals a transition from [WO4] tetrahedra to [WO6] octahedra at higher pressures.
- Experimental and computational data provide a comprehensive understanding of SrWO4's high-pressure structural systematics.
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