| Project/Area Number |
21740383
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| Research Category |
Grant-in-Aid for Young Scientists (B)
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| Allocation Type | Single-year Grants |
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| Research Field |
Petrology/Mineralogy/Science of ore deposit
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| Research Institution | Japan Synchrotron Radiation Research Institute |
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Principal Investigator |
HIRAO Naohisa Japan Synchrotron Radiation Research Institute, 利用研究促進部門, 研究員 (70374915)
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| Project Period (FY) |
2009 – 2010
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| Project Status |
Completed (Fiscal Year 2010)
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| Budget Amount *help |
¥4,420,000 (Direct Cost: ¥3,400,000、Indirect Cost: ¥1,020,000)
Fiscal Year 2010: ¥1,430,000 (Direct Cost: ¥1,100,000、Indirect Cost: ¥330,000)
Fiscal Year 2009: ¥2,990,000 (Direct Cost: ¥2,300,000、Indirect Cost: ¥690,000)
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| Keywords | 地球・惑星内部構造 / 地球核 / 高温高圧 / 放射光 / 金属水素化物 / 金属物性 / X線回折 / 鉄水素化物 / 地球惑星内部構造 / 超高圧 |
|---|
| Research Abstract |
Hydrogen is one of the most important candidates as light elements in the Earth's core. To understand the behavior of hydrogen in the Earth's core and its effect on the structure and dynamics of the core, experimental studies of crystal structures, phase relations, and their properties in iron-hydrogen (Fe-H) system are needed at high pressures and temperatures. In the Fe-H system we developed a high-pressure and high-temperature generation technique up to about 100 GPa and 2000 K using a laser-heated diamond anvil cell. The double hexagonal close-packed of iron hydride (FeH) was observed up to about 100 GPa, which suggests that FeH is possibly stable in the Earth's core.
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