Work

High-Pressure X-ray Diffraction Study of Scheelite-Type Perrhenates

Year: 2025
Type: article
Abstract: High Resolution Image Download MS PowerPoint Slide 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 AgReO 4, KReO 4, and RbReO 4, exhibit a tetragonal scheelite-type crystal structure described by space group I 4 1 / a . Under compression, a transition from scheelite-to-M′-fergusonite (space group P 2 1 / c ) was observed at 1.6 and 7.4 GPa for RbReO 4 and KReO 4, respectively. The transition involves a relative volume decrease. On the other hand, AgReO 4 underwent a phase transition to the M-fergusonite structure (space group I 2/ 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 low-pressure phase are confirmed by density-functional theory calculations. The analysis of the bulk modulus shows that the compressibility of the compounds decreases following the sequence RbReO 4 > KReO 4 > AgReO 4, which is related to the compressibility of the RbO 8, KO 8, and AgO 8 bidisphenoid units. Density-functional theory also offers valuable insights into the elastic constants. Despite giving a good description for the low-pressure phase in the three compounds, density-functional theory cannot catch the structural phase transition observed in experiments. Reasons for it are discussed in the manuscript.
Language: English
Subfield: Geophysics
Open Access status: hybrid
Estimated APC paid: $4,500
OpenAlex ID: W4413533786
FWCI: 2.39
Cites: 44
Cited by: 5
Related to: 10