Structure Solution of the High-Pressure Phase of CuWO4 and Evolution of the Jahn-Teller Distortion

被引:56
作者
Ruiz-Fuertes, J. [1 ]
Friedrich, A. [2 ]
Pellicer-Porres, J. [1 ]
Errandonea, D. [1 ]
Segura, A. [1 ]
Morgenroth, W. [2 ]
Haussuehl, E. [2 ]
Tu, C. -Y. [3 ]
Polian, A. [4 ]
机构
[1] Univ Valencia, Dept Fis Aplicada ICMUV, MALTA Consolider Team, E-46100 Burjassot, Spain
[2] Goethe Univ Frankfurt, Abt Kristallog, Inst Geowissensch, D-60438 Frankfurt, Germany
[3] Chinese Acad Sci, Fujian Inst Res Struct Matter, Fuzhou 350002, Fujian, Peoples R China
[4] Univ Paris 06, CNRS, Inst Mineral & Phys Milieux Condenses, UMR 7590, F-75252 Paris, France
关键词
high-pressure; X-ray diffraction; EXAFS; phase transition; Jahn-Teller; COPPER TUNGSTATE;
D O I
10.1021/cm201592h
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
In this work, we have investigated the structural behavior of cuproscheelite up to 33.9 GPa by means of high-pressure single-crystal X-ray diffraction (SXRD) and extended X-ray absorption fine structure (EXAFS). According to EXAFS, beyond 9 GPa a phase transition takes place. On the basis of SXRD, the transition is from the triclinic (PI) structure to a monoclinic (P2/c) structure isotypic to wolframite. The transition implies abrupt changes of CuO6 and WO6 octahedra, but no coordination change. Further, we report the role played by the Jahn-Teller distortion of the CuO6 octahedra on the mechanism of the phase transition as well as the changes in the behavior of the Cu-O bonds for the triclinic and monoclinic phases of CuWO4. A second phase transition was detected at 22.5 GPa. Finally, a low-temperature experiment has been carried out at 100 K. No structural changes were detected for CuWO4, confirming the already known triclinic structure stability at room pressure and low temperature.
引用
收藏
页码:4220 / 4226
页数:7
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