X-ray diffraction and Raman spectra of merrillite at high pressures |
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Authors: | Muhua Jia Xin Hu Yungui Liu Sheng Jiang Xiang Wu |
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Affiliation: | 1. Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, People’s Republic of China;2. University of Chinese Academy of Sciences, Beijing, People’s Republic of China;3. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, People’s Republic of China;4. Shanghai Synchrotron Radiation Facility (SSRF), Shanghai Advanced Research Institute, Chinese Academy of Sciences, Shanghai, People’s Republic of China https://orcid.org/0000-0002-2570-6654 |
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Abstract: | ABSTRACT The compressibility and effect of pressure on the vibrations of merrillite, Ca9NaMg(PO4)7, were studied by using diamond anvil cell at room temperature combined with in-situ synchrotron X-ray diffraction and Raman spectroscopy up to about 18 and 15?GPa, respectively. The pressure-volume data was fitted by a third-order Birch–Murnaghan equation of state to determine the isothermal bulk modulus as K0 ?=?87.2(32) GPa with pressure derivative K0′?=?3.2(4). If K0′?=?4, the isothermal bulk modulus was obtained as 81.6(10) GPa. The axial compressibility was estimated and an axial elastic anisotropy exists since a-axis is less compressible than the c-axis. The Raman frequencies of all observed modes for merrillite continuously increase with pressure, and the pressure dependences of stretching modes (v 3 and v 1) are larger than those of the bending modes (v 4 and v 2) and external modes. The isothermal mode Grüneisen parameters and intrinsic anharmonicity of merrillite were also calculated. |
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Keywords: | Merrillite Ca9NaMg(PO4)7 high pressure X-ray diffraction Raman spectroscopy |
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