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Equation of state of adamite up to 11 GPa: a synchrotron X-ray diffraction study
Xu, JG; Ma, MN; Wei, SY; Hu, XX; Liu, YG; Liu, J; Fan, DW; Xie, HS;刘景
2014
发表期刊PHYSICS AND CHEMISTRY OF MINERALS
卷号41期号:7页码:547-554
摘要The compression behavior of natural adamite [Zn2AsO4OH] has been investigated up to 11.07 GPa at room temperature utilizing in situ angle-dispersive X-ray diffraction and a diamond anvil cell. No phase transition has been observed within the pressure range investigated. A third-order Birch-Murnaghan equation of state fitted to all of the data points yielded V (0) = 430.1(4) a"<<(3), K (0) = 80(3) GPa, K' (0) = 1.9(5). The K (0) was obtained as 69(1) GPa when K' (0) was fixed at 4. Analysis of axial compressible moduli shows the intense compression anisotropy of adamite: K (a0) = 37(3) GPa, K (b0) = 153(6) GPa, K (c0) = 168(8) GPa; hence, a axis is the most compressible and the compressibility of b and c axis is comparable. Furthermore, the comparisons among the compressional properties of adamite, libethenite (Cu2PO4OH, also belongs to olivenite group), and andalusite (Al2SiO4O has the similar structure with adamite) at high pressure were made.
关键词Adamite High pressure Synchrotron X-ray diffraction Equation of state Diamond anvil cell
学科领域Materials Science; Mineralogy
DOI10.1007/s00269-014-0666-0
收录类别SCI
WOS记录号WOS:000338332200008
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被引频次:5[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ihep.ac.cn/handle/311005/225300
专题多学科研究中心
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Xu, JG,Ma, MN,Wei, SY,et al. Equation of state of adamite up to 11 GPa: a synchrotron X-ray diffraction study[J]. PHYSICS AND CHEMISTRY OF MINERALS,2014,41(7):547-554.
APA Xu, JG.,Ma, MN.,Wei, SY.,Hu, XX.,Liu, YG.,...&Xie, HS;刘景.(2014).Equation of state of adamite up to 11 GPa: a synchrotron X-ray diffraction study.PHYSICS AND CHEMISTRY OF MINERALS,41(7),547-554.
MLA Xu, JG,et al."Equation of state of adamite up to 11 GPa: a synchrotron X-ray diffraction study".PHYSICS AND CHEMISTRY OF MINERALS 41.7(2014):547-554.
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