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Synchrotron X-ray diffraction study of phenacite at high pressure
Fan Da-Wei; Ma Mai-Ning; Wei Shu-Yi; Chen Zhi-Qiang; Xie Hong-Sen
2012
Source PublicationChinese Physics C
Volume36Issue:2Pages:179-183
AbstractWe report the results of a natural phenacite from 0 to 30.9 GPa using in situ angle-dispersive X-ray diffraction and a diamond anvil cell at the National Synchrotron Light Source, Brookhaven National Laboratory. Over this pressure range, no phase change or disproportionation has been observed. The isothermal equation of state was determined. The values of V-0, K-0, and K-0' refined with a third-order Birch-Murnaghan equation of state are V-0=1116.1 +/- 1.2 angstrom(3), K-0=223 +/- 9 GPa, and K-0 '=5.5 +/- 0.8. Furthermore, we confirm that the linear compressibilities (beta) along a and c directions of phenacite are elastically isotropic (beta(a)=1.50 x 10(-3) and beta(c)=1.34 x 10(-3) GPa(-1)). Consequently, it can be concluded that the compressibility of phenacite under high pressures has been accurately constrained.
Subject Area地球深部物质与流体作用地球化学
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/4876
Collection地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
Recommended Citation
GB/T 7714
Fan Da-Wei,Ma Mai-Ning,Wei Shu-Yi,et al. Synchrotron X-ray diffraction study of phenacite at high pressure[J]. Chinese Physics C,2012,36(2):179-183.
APA Fan Da-Wei,Ma Mai-Ning,Wei Shu-Yi,Chen Zhi-Qiang,&Xie Hong-Sen.(2012).Synchrotron X-ray diffraction study of phenacite at high pressure.Chinese Physics C,36(2),179-183.
MLA Fan Da-Wei,et al."Synchrotron X-ray diffraction study of phenacite at high pressure".Chinese Physics C 36.2(2012):179-183.
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