2010 Fiscal Year Final Research Report
Phase relations of iron-light elements alloys at high pressure and high temperature
Project/Area Number |
21840037
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Research Category |
Grant-in-Aid for Research Activity Start-up
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Allocation Type | Single-year Grants |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Ehime University |
Principal Investigator |
KUWAYAMA Yasuhiro Ehime University, 地球深部ダイナミクス研究センター, 助教 (00554015)
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Project Period (FY) |
2009 – 2010
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Keywords | 超高圧 / 地球中心核 / 相平衡 / 鉄合金 |
Research Abstract |
I have largely improved the data quality of in-situ x-ray diffraction measurements at multimegabar pressures and high temperatures. As a result, I succeeded in determining the crystal structures of pure iron and iron-nickel alloy at the pressure and temperature condition of the Earth's inner-core based on reliable data. I determined a solubility of silicon, which is thought to be the most likely candidate of the light element in the Earth's core, into solid iron at high pressures and temperatures and showed that silicon may be contained not only in the Earth's liquid outer-core, but also in the solid inner-core. I also discovered a new ultra-high pressure phase transitions in metal dioxides at multimegabar pressures during this technical development.
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[Presentation] P-V-T equation of state of MgSiO3 perovskite up to 110 GPa and 2500 K : Primary reference for the mineralogy of the lower mantle.2010
Author(s)
Tange, Y., Kuwayama Y, Irifune, T., Funakoshi, K., Ohishi, Y.
Organizer
American Geophysical Union Fall Meeting 2010
Place of Presentation
San Francisco, CA, USA
Year and Date
2010-12-16
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