Experimental method for in situ determination of material textures at simultaneous high pressure and high temperature by means of radial diffraction in the diamond anvil cell

被引:38
作者
Liermann, Hanns-Peter [1 ,2 ]
Merkel, Sebastien [3 ]
Miyagi, Lowell [4 ]
Wenk, Hans-Rudolf [4 ]
Shen, Guoyin [1 ]
Cynn, Hyunchae [5 ]
Evans, William J. [5 ]
机构
[1] Carnegie Inst Sci, Geophys Lab, High Pressure Collaborat Access Team, Argonne, IL 60439 USA
[2] DESY, D-22607 Hamburg, Germany
[3] Univ Lille 1, CNRS, Lab Struct & Proprietes Etat Solide, F-59655 Villeneuve Dascq, France
[4] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA
[5] Lawrence Livermore Natl Lab, High Pressure Phys Grp, Livermore, CA 94550 USA
基金
美国国家科学基金会;
关键词
X-RAY-DIFFRACTION; POLYCRYSTALLINE DIAMOND; PLASTIC-DEFORMATION; POST-PEROVSKITE; LOWER MANTLE; 15; GPA; IRON; APPARATUS; CALIBRATION; WINDOWS;
D O I
10.1063/1.3236365
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
We introduce the design and capabilities of a resistive heated diamond anvil cell that can be used for side diffraction at simultaneous high pressure and high temperature. The device can be used to study lattice-preferred orientations in polycrystalline samples up to temperatures of 1100 K and pressures of 36 GPa. Capabilities of the instrument are demonstrated with preliminary results on the development of textures in the bcc, fcc, and hcp polymorphs of iron during a nonhydrostatic compression experiment at simultaneous high pressure and high temperature. (C) 2009 American Institute of Physics. [doi:10.1063/1.3236365]
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页数:8
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