High-pressure X-ray diffraction and Raman spectroscopy of CaFe2O4-type β-CaCr2O4

被引:0
作者
Shuangmeng Zhai
Yuan Yin
Sean R. Shieh
Shuangming Shan
Weihong Xue
Ching-Pao Wang
Ke Yang
Yuji Higo
机构
[1] Chinese Academy of Sciences,Key Laboratory of High
[2] University of Chinese Academy of Sciences,Temperature and High
[3] University of Western Ontario,Pressure Study of the Earth’s Interior, Institute of Geochemistry
[4] Chinese Academy of Sciences,College of Earth Science
[5] Japan Synchrotron Radiation Research Institute,Department of Earth Sciences
来源
Physics and Chemistry of Minerals | 2016年 / 43卷
关键词
β-CaCr; O; Equation of state; Synchrotron X-ray diffraction; Raman spectra; High pressure;
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摘要
In situ high-pressure synchrotron X-ray diffraction and Raman spectroscopic studies of orthorhombic CaFe2O4-type β-CaCr2O4 chromite were carried out up to 16.2 and 32.0 GPa at room temperature using multi-anvil apparatus and diamond anvil cell, respectively. No phase transition was observed in this study. Fitting a third-order Birch–Murnaghan equation of state to the P–V data yields a zero-pressure volume of V0 = 286.8(1) Å3, an isothermal bulk modulus of K0 = 183(5) GPa and the first pressure derivative of isothermal bulk modulus K0′ = 4.1(8). Analyses of axial compressibilities show anisotropic elasticity for β-CaCr2O4 since the a-axis is more compressible than the b- and c-axis. Based on the obtained and previous results, the compressibility of several CaFe2O4-type phases was compared. The high-pressure Raman spectra of β-CaCr2O4 were analyzed to determine the pressure dependences and mode Grüneisen parameters of Raman-active bands. The thermal Grüneisen parameter of β-CaCr2O4 is determined to be 0.93(2), which is smaller than those of CaFe2O4-type CaAl2O4 and MgAl2O4.
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页码:307 / 314
页数:7
相关论文
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