6533b7defe1ef96bd12765cf

RESEARCH PRODUCT

High-pressure structural transformations of PbCrO4 up to 51.2 GPa: An angle-dispersive synchrotron X-ray diffraction study

Ravhi S. KumarDaniel Errandonea

subject

DiffractionPhase transitionMaterials scienceMechanical EngineeringSynchrotron radiationCondensed Matter PhysicsCrystallographyTetragonal crystal systemMechanics of MaterialsMonazitePhase (matter)X-ray crystallographyGeneral Materials ScienceMonoclinic crystal system

description

Abstract We report on high-pressure X-ray diffraction measurements up to 51.2 GPa in PbCrO 4 at room temperature. Three high-pressure phases with structures different than the ambient-pressure monazite-type ( P 2 1 / n ) are reported. One phase transition was found at 3.8 GPa to an isomorphic structure to monazite. A second transition occurs at 11.1 GPa. After this transition, the coexistence of tetragonal ( I 4 1 / a ) and monoclinic ( P 2 1 ) structures is detected up to 21.1 GPa. Beyond this pressure and up to 51.2 GPa, only the high-pressure monoclinic phase is observed. Upon decompression all structural changes are reversible. Finally, the axial compressibilities for the different phases have been determined as well as the equations of state.

https://doi.org/10.1016/j.materresbull.2014.08.041