High-Pressure X-Ray Diffraction Study of Scheelite-type Perrhenates
Neha Bura, Pablo Botella, Catalin Popescu, Frederico Alabarse, Ganapathy Vaitheeswaran, Alfonso Munoz, Brendan J. Kennedy, Jose Luis Rodrigo Ramon, Josu Sanchez-Martin, Daniel Errandonea

TL;DR
This study investigates how pressure affects the crystal structure of scheelite-type perrhenates using X-ray diffraction and density-functional theory, revealing phase transitions and elastic properties.
Contribution
It provides new experimental and theoretical insights into pressure-induced phase transitions and elastic properties of AgReO4, KReO4, and RbReO4 perrhenates.
Findings
Observed scheelite-to-fergusonite phase transitions at specific pressures.
Determined pressure-volume equations of state for the compounds.
Density-functional theory accurately describes low-pressure phases but not phase transitions.
Abstract
The effects of pressure on the crystal structure of scheelite-type perrhenates were studied using synchrotron powder X-ray diffraction and density-functional theory. At ambient conditions, the studied materials AgReO4, KReO4, and RbReO4, exhibit a tetragonal scheelite-type crystal structure described by space group I41/a. Under compression, a transition from scheelite-to-M-fergusonite (space group P21/c) was observed at 1.6 and 7.4 GPa for RbReO4 and KReO4, respectively. The transition involves a relative volume decrease. On the other hand, AgReO4 underwent a phase transition to the M-fergusonite structure (space group I2/a) at 13.6 GPa. In this case there is no appreciable volume discontinuity. The room-temperature pressure-volume equation of state for the three studied perrhenates was estimated using a second-order Birch-Murnaghan equation of state. The results for the…
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Taxonomy
TopicsThermal Expansion and Ionic Conductivity · High-pressure geophysics and materials · Heusler alloys: electronic and magnetic properties
