Polymorphism of praseodymium orthovanadate under high pressure

Autor: Catalin Popescu, Julio Pellicer-Porres, D. Martinez-Garcia, Srungarpu N. Achary, Enrico Bandiello, Alfonso Muñoz, David Santamaría-Pérez, T. Marqueño, Plácida Rodríguez-Hernández, Daniel Errandonea
Rok vydání: 2021
Předmět:
Zdroj: Physical Review B. 103
ISSN: 2469-9969
2469-9950
DOI: 10.1103/physrevb.103.134113
Popis: Zircon-type $\mathrm{PrV}{\mathrm{O}}_{4}$ has been studied at high pressures and room temperature by means of synchrotron powder x-ray diffraction. At room temperature, we observed the previously known zircon-to-monazite phase transition at 5.5(4) GPa and a second phase transition from monazite to a monoclinic structure at 12.7(8) GPa, which we identified as a $\mathrm{PbW}{\mathrm{O}}_{4}$-III-type phase. This conclusion is supported by our ab initio calculations, which also predict a scheelite-type phase to be stable at high pressure. Motivated by this finding, we subjected zircon-type $\mathrm{PrV}{\mathrm{O}}_{4}$ samples to high pressure (7 GPa) and temperature (600, 800, and 1000 \ifmmode^\circ\else\textdegree\fi{}C) in a Paris-Edinburgh large volume press cell. As a result, we could synthesize a scheelite-type phase of $\mathrm{PrV}{\mathrm{O}}_{4}$, which was recovered in a metastable state at room conditions, and the unit-cell parameters and the atomic positions have been determined. We also report a substantial increase of the scheelite proportion with time by comparing synthesis of different durations, at the same pressure-temperature conditions. The transition mechanisms of the zircon-, monazite-, and scheelite-type structures as well as the role of kinetic barriers will be discussed. Information on the compressibility of different polymorphs will be reported too.
Databáze: OpenAIRE