The compressibility of a natural apatite

被引:36
作者
Matsukage, KN
Ono, S
Kawamoto, T
Kikegawa, T
机构
[1] Japan Marine Sci & Technol Ctr, Inst Frontier Res Earth Evolut, Kanagawa 2370061, Japan
[2] Kyoto Univ, Grad Sch Sci, Inst Geothermal Sci, Beppu, Oita 8740903, Japan
[3] High Energy Accelerator Res Org, Tsukuba, Ibaraki 3050801, Japan
[4] Ibaraki Univ, Fac Sci, Dept Environm Sci, Mito, Ibaraki 3100056, Japan
关键词
apatite; compressibility; third-order Birch-Murnaghan equation of state; bulk modulus;
D O I
10.1007/s00269-004-0415-x
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
In-situ synchrotron X-ray diffraction (XRD) experiments of a natural apatite with the formula of Ca-5(PO4)(3)F0.94Cl0.06 were carried out using a diamond anvil cell and angle-dispersive technique at Photon Factory (PF), Japan. Pressure-volume data were collected up to 7.12 GPa at 300 K. The pressures were determined from the ruby fluorescence spectra shift. The unit-cell parameters and volume decreased systematically with increasing pressure, and a reliable isothermal bulk modulus and its pressure derivative were obtained in this study. The third-order Birch-Murnaghan equation of state yielded the isothermal bulk modulus of K-T = 91.5(38) GPa, its pressure derivative K-T' = 4.0(11), and the zero-pressure volume V-o = 524. 2(3) Angstrom(3).
引用
收藏
页码:580 / 584
页数:5
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