Search results for "Fergusonite"

showing 6 items of 16 documents

Quasi-hydrostatic X-ray powder diffraction study of the low- and high-pressure phases of CaWO4 up to 28 GPa

2014

We have studied CaWO4 under compression using Ne as pressure-transmitting medium at room temperature by means of synchrotron X-ray powder diffraction. We have found that CaWO4 beyond 8.8 GPa transforms from its low-pressure tetragonal structure (scheelite) into a monoclinic structure (fergusonite). The high-pressure phase remains stable up to 28 GPa and the low-pressure phase is totally recovered after full decompression. The pressure dependence of the unit-cell parameters, as well as the pressure volume equation of state, has been determined for both phases. Compared with previous studies, we found in our quasi-hydrostatic experiments a different behavior for the unit-cell parameters of th…

Phase transitionEquation of stateMaterials scienceScheeliteThermodynamicsGeneral ChemistryCondensed Matter PhysicsFergusoniteX-ray diffractionHigh pressureTetragonal crystal systemCrystallographyFISICA APLICADAPhase (matter)X-ray crystallographyCalcium tungstateGeneral Materials SciencePowder diffractionPhase transitionMonoclinic crystal systemSolid State Sciences
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Monoclinic-tetragonal-monoclinic phase transitions in Eu0.1Bi0.9VO4 under pressure

2019

The promising technological material Eu0.1Bi0.9VO4, has been studied for the first time at room-temperature under high-pressure, up to 24.9 GPa, by means of in situ angle dispersive powder x-ray diffraction (XRD). The compound undergoes two phase transitions at 1.9 and 16.1 GPa. The first transition is from the monoclinic fergusonite-type structure (space group I2/a) to a tetragonal scheelite-type structure (space group I41/a), being a ferroelastic-paraelastic transformation similar to that previously reported for isomorphic pristine BiVO4. The second phase transition is first-order in nature. The scheelite-type and the second high-pressure phase coexist in a wide pressure range. A monoclin…

Phase transitionMaterials science02 engineering and technologyCrystal structure021001 nanoscience & nanotechnologyCondensed Matter PhysicsFergusonite01 natural sciencesTetragonal crystal systemDodecahedronCrystallographyPhase (matter)0103 physical sciencesX-ray crystallographyGeneral Materials Science010306 general physics0210 nano-technologyMonoclinic crystal systemJournal of Physics: Condensed Matter
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ScVO4 under non-hydrostatic compression:a new metastable polymorph

2016

Ustedes se ocupan e ver si se puede hacer de acceso público. Podria buscra el preprint al ser algo reciente. Se estudia el comportamiento bajo alta presión del vanadato de scandio, ScVO4, bajo compresión no hidrostática. El estudio se realiza mediante difracción de rayos X en polvo usando radiación sincrotrón. Se detecta una transición no reversible desde la fase zircon a la fase fergusonita alrededor de 6 GPa con una discontinuidad en el volumen de un 10%. La fase fergusonota se puede recuperar como metaestable confirmandose mediante XRD. Las simulaciones ab intio confirman los resultados experimentales. Las propiedades ópticas y la propiedades vibracionales de la fase fergusonita son disc…

Phase transitionMaterials scienceBand gapAnalytical chemistrychemistry.chemical_element02 engineering and technology021001 nanoscience & nanotechnologyCondensed Matter PhysicsFergusonite01 natural sciencessymbols.namesakechemistryMetastabilityPhase (matter)0103 physical sciencessymbolsGeneral Materials ScienceScandium010306 general physics0210 nano-technologyRaman spectroscopyAmbient pressure
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Phase transition systematics in BiVO4 by means of high-pressure–high-temperature Raman experiments

2018

We report here high-pressure--high-temperature Raman experiments performed on ${\text{BiVO}}_{4}$. We characterized the fergusonite and scheelite phases (powder and single crystal samples) and the zircon polymorph (nanopowder). The experimental results are supported by ab initio calculations, which, in addition, provide the vibrational patterns. The temperature and pressure behavior of the fergusonite lattice modes reflects the distortions associated with the ferroelastic instability. The linear coefficients of the zircon phase are in sharp contrast to the behavior observed in the fergusonite phase. The boundary of the fergusonite-to-scheelite second-order phase transition is given by ${T}_…

Phase transitionMaterials scienceScatteringAnharmonicity02 engineering and technology010402 general chemistry021001 nanoscience & nanotechnologyFergusonite01 natural sciences0104 chemical sciencesCrystallographysymbols.namesakeAb initio quantum chemistry methodsLattice (order)symbols0210 nano-technologyRaman spectroscopySingle crystalPhysical Review B
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Determination of the high-pressure crystal structure ofBaWO4andPbWO4

2006

We report the results of both angle-dispersive x-ray diffraction and x-ray absorption near-edge structure studies in $\mathrm{Ba}\mathrm{W}{\mathrm{O}}_{4}$ and $\mathrm{Pb}\mathrm{W}{\mathrm{O}}_{4}$ at pressures of up to $56\phantom{\rule{0.3em}{0ex}}\mathrm{GPa}$ and $24\phantom{\rule{0.3em}{0ex}}\mathrm{GPa}$, respectively. $\mathrm{Ba}\mathrm{W}{\mathrm{O}}_{4}$ is found to undergo a pressure-driven phase transition at $7.1\phantom{\rule{0.3em}{0ex}}\mathrm{GPa}$ from the tetragonal scheelite structure (which is stable under normal conditions) to the monoclinic fergusonite structure whereas the same transition takes place in $\mathrm{Pb}\mathrm{W}{\mathrm{O}}_{4}$ at $9\phantom{\rule{0…

PhysicsTetragonal crystal systemX-ray spectroscopyCrystallographyCondensed matter physicsX-ray crystallographyAbsorption (logic)Crystal structureIsostructuralCondensed Matter PhysicsFergusoniteElectronic Optical and Magnetic MaterialsMonoclinic crystal systemPhysical Review B
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High-Pressure Raman Scattering of CaWO4 Up to 46.3 GPa: Evidence of a New High-Pressure Phase

2014

International audience; The high-pressure behavior of CaWO4 wasanalyzed at room temperature by Raman spectroscopy.Pressure was generated using a diamond-anvil cell and Ne aspressure-transmitting medium. The pressure range of previousstudies has been extended from 23.4 to 46.3 GPa. Theexperiments reveal the existence of two reversible phasetransitions. The first one occurs from the tetragonal scheelitestructure to the monoclinic fergusonite structure and isobserved at 10 GPa. The onset of a previously unknownsecond transition is found at 33.4 GPa. The two high-pressurephases coexist up to 39.4 GPa. The Raman spectra measuredfor the low-pressure phase and the first high-pressure phase arecons…

[PHYS]Physics [physics]Phase transitionAnalytical chemistry02 engineering and technology021001 nanoscience & nanotechnologyFergusonite01 natural sciencesInorganic Chemistrychemistry.chemical_compoundTetragonal crystal systemsymbols.namesakeCrystallographychemistryScheelitePhase (matter)0103 physical sciencessymbolsPhysical and Theoretical Chemistry010306 general physics0210 nano-technologyRaman spectroscopyRaman scatteringMonoclinic crystal systemInorganic Chemistry
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