Combined resistive and laser heating technique for in situ radial X-ray diffraction in the diamond anvil cell at high pressure and temperature

被引:25
|
作者
Miyagi, Lowell [1 ,2 ]
Kanitpanyacharoen, Waruntorn [3 ]
Raju, Selva Vennila [4 ,5 ]
Kaercher, Pamela [3 ]
Knight, Jason [4 ]
MacDowell, Alastair [4 ]
Wenk, Hans-Rudolf [3 ]
Williams, Quentin [6 ]
Alarcon, Eloisa Zepeda [3 ]
机构
[1] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA
[2] Montana State Univ, Dept Earth Sci, Bozeman, MT 59717 USA
[3] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA
[4] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Adv Light Source, Berkeley, CA 94720 USA
[5] Univ Nevada, Dept Phys, HiPSEC, Las Vegas, NV 89154 USA
[6] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA
基金
美国国家科学基金会;
关键词
POST-PEROVSKITE; 10; GPA; DEFORMATION; SYSTEM; GRAPHITIZATION; TEXTURE; APPARATUS; SLIP;
D O I
10.1063/1.4793398
中图分类号
TH7 [仪器、仪表];
学科分类号
0804 ; 080401 ; 081102 ;
摘要
To extend the range of high-temperature, high-pressure studies within the diamond anvil cell, a Liermann-type diamond anvil cell with radial diffraction geometry (rDAC) was redesigned and developed for synchrotron X-ray diffraction experiments at beamline 12.2.2 of the Advanced Light Source. The rDAC, equipped with graphite heating arrays, allows simultaneous resistive and laser heating while the material is subjected to high pressure. The goals are both to extend the temperature range of external (resistive) heating and to produce environments with lower temperature gradients in a simultaneously resistive-and laser-heated rDAC. Three different geomaterials were used as pilot samples to calibrate and optimize conditions for combined resistive and laser heating. For example, in Run#1, FeO was loaded in a boron-mica gasket and compressed to 11 GPa then gradually resistively heated to 1007 K (1073 K at the diamond side). The laser heating was further applied to FeO to raise temperature to 2273 K. In Run#2, Fe-Ni alloy was compressed to 18 GPa and resistively heated to 1785 K (1973 K at the diamond side). The combined resistive and laser heating was successfully performed again on (Mg0.9Fe0.1) O in Run#3. In this instance, the sample was loaded in a boron-kapton gasket, compressed to 29 GPa, resistive-heated up to 1007 K (1073 K at the diamond side), and further simultaneously laser-heated to achieve a temperature in excess of 2273 K at the sample position. Diffraction patterns obtained from the experiments were deconvoluted using the Rietveld method and quantified for lattice preferred orientation of each material under extreme conditions and during phase transformation. (C) 2013 American Institute of Physics. [http://dx.doi.org/10.1063/1.4793398]
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页数:9
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