0000000000073383

AUTHOR

D. Vázquez-socorro

showing 2 related works from this author

Stability of the fergusonite phase in GdNbO 4 by high pressure XRD and Raman experiments

2017

Abstract We describe the results of high pressure x-ray diffraction and Raman measurements on gadolinium orthoniobate. The ambient pressure monoclinic fergusonite phase remains stable in a remarkable large pressure range. There is no significative evolution of the monoclinic distortion up to 25 GPa , the maximum pressure achieved. Instead, the anisotropic compressibility is associated to the stiffness of NbO 4 tetrahedra in respect to the GdO 8 polyhedra. The high pressure evolution of external modes parallels the wavenumber dependence on ionic radius along the lanthanide series. The chemical pressure analogy is attributed to the compression of GdO 8 polyhedra. There is no evidence of any p…

Materials sciencePhonon02 engineering and technology010402 general chemistryFergusonite01 natural sciencesInorganic ChemistryCondensed Matter::Materials Sciencesymbols.namesakePhase (matter)Materials ChemistryPhysical and Theoretical ChemistryIonic radiusCondensed matter physics021001 nanoscience & nanotechnologyCondensed Matter Physics0104 chemical sciencesElectronic Optical and Magnetic MaterialsCrystallographyCeramics and CompositesCompressibilitysymbolsCondensed Matter::Strongly Correlated Electrons0210 nano-technologyRaman spectroscopyAmbient pressureMonoclinic crystal systemJournal of Solid State Chemistry
researchProduct

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
researchProduct