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An in situ high-pressure X-ray diffraction experiment on hydroxyapophyllite
Fan Da-Wei; Wei Shu-Yi; Xie Hong-Sen
2013
Source PublicationChinese Physics B
Volume22Issue:1Pages:010702
AbstractThe compression behavior of a natural hydroxyapophyllite is investigated up to about 10.01 GPa at 300 K using in situ angle-dispersive X-ray diffraction and a diamond anvil cell at the High Pressure Experiment Station, Beijing Synchrotron Radiation Facility (BSRF). Over this pressure range, no phase change or disproportionation is observed. The isothermal equation of state is determined for the first time. The values of zero-pressure volume V-0, isothermal bulk modulus K-0, and K-0' refined with a third-order Birch-Murnaghan equation of state are V-0 = 1276.3 +/- 0.9 angstrom(3), K-0 = 71 +/- 3 GPa, and K-0' = 8 +/- 1. Furthermore, we confirm that the values of linear compressibility beta along the a and c directions of hydroxyapophyllite are elastically anisotropic.
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5115
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
地球深部物质与流体作用地球化学研究室
Recommended Citation
GB/T 7714
Fan Da-Wei,Wei Shu-Yi,Xie Hong-Sen. An in situ high-pressure X-ray diffraction experiment on hydroxyapophyllite[J]. Chinese Physics B,2013,22(1):010702.
APA Fan Da-Wei,Wei Shu-Yi,&Xie Hong-Sen.(2013).An in situ high-pressure X-ray diffraction experiment on hydroxyapophyllite.Chinese Physics B,22(1),010702.
MLA Fan Da-Wei,et al."An in situ high-pressure X-ray diffraction experiment on hydroxyapophyllite".Chinese Physics B 22.1(2013):010702.
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