Raman spectra and X-ray diffraction of merrillite at various temperatures

被引:11
作者
Jia, Muhua [1 ,2 ]
Zhai, Kuan [1 ,2 ]
Gao, Mei [3 ]
Wen, Wen [3 ]
Liu, Yungui [4 ]
Wu, Xiang [4 ]
Zhai, Shuangmeng [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths In, Guiyang 550081, Guizhou, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Chinese Acad Sci, Shanghai Adv Res Inst, SSRF, Shanghai 201210, Peoples R China
[4] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China
基金
中国国家自然科学基金;
关键词
Merrillite; High-temperature; Raman spectra; X-ray diffraction; Thermal expansion; Gruneisen parameter; CRYSTAL-CHEMISTRY; THERMAL-EXPANSION; HIGH-PRESSURE; APATITE; WHITLOCKITE; MINERALS; CRYSTALLIZATION; SPECTROSCOPY; PHOSPHATE; METEORITE;
D O I
10.1016/j.vibspec.2019.103005
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
The Raman spectra and in-situ X-ray diffraction patterns of synthetic merrillite, Ca9NaMg(PO4)(7), have been measured up to 1173 K at ambient pressure. No phase transformation was observed in this study. The effect of temperature on the Raman spectra shows that all observed active bands continuously shift to lower wavenumber with increasing temperature. The temperature dependences of v(3) anti-symmetric PO stretching modes are larger than those of v(1) symmetric P-O stretching, v(4) and v(2) O-P-O bending modes and the external modes. Lattice parameters and volume were analyzed, and the thermal expansion coefficients were obtained as 4.86(5) x 10(-5) K-1, 1.46(1) x 10(-5) K-1 and 1.94(5) x 10(-5) K-1 for V, a and c, respectively. Thermal expansion of merrillite shows an axial anisotropy with a smaller expansion coefficient along the alpha-axis. The average isobaric mode Gruneisen parameter for the internal PO4 modes of merrillite has been calculated as 0.57.
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页数:5
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