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Detailed Reference Information |
Funamori, N., Yagi, T. and Uchida, T. (1996). High-pressure and high-temperature in situ x-ray Diffraction study of iron to above 30 Gpa using MA8-type apparatus. Geophysical Research Letters 23: doi: 10.1029/96GL00943. issn: 0094-8276. |
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In situ x-ray diffraction experiments on iron at pressures of 22--32 GPa and temperatures of 300--1500 K were carried out using an MA8-type high-pressure apparatus, employing sintered diamond anvils, combined with synchrotron radiation. No phases other than ϵ(hcp) and &ggr;(fcc) were observed in this pressure and temperature range. It became clear that non-hydrostaticity or chemical reaction with hydrogen causes serious problems in high-pressure and high-temperature x-ray diffraction study on iron. The average thermal expansivity of ϵ phase between 300 K and 1000 K and the zero-pressure bulk modulus of &ggr; phase at 1400 K were determined by assuming that no chemical reaction occurred in the present study. The thermal expansivities of ϵ iron at 22 GPa and 32 GPa are determined to be 3.88¿10-5 K-1 and 3.16¿10-5 K-1, respectively. In this case, the volume at 22--32 GPa and room temperature is about 1% larger than the literature value. The bulk modulus of &ggr; iron is determined to be 120 GPa, when its pressure derivative is fixed at 5. |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Mineral Physics, Equations of state, Mineral Physics, High-pressure behavior, Mineral Physics, X ray, neutron, and electron spectroscopy and diffraction, Mineral Physics, Instruments and techniques |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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