期刊
GEOPHYSICAL RESEARCH LETTERS
卷 40, 期 19, 页码 5131-5136出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/grl.51004
关键词
iron; pressure; magnetism; core
资金
- Deutsche Forschungsgemeinschaft [GI712/7-1, SPP1488]
Computational, Mossbauer, and synchrotron radiation experiments arrive at disparate conclusions regarding the magnetic state of the high-pressure, hexagonal closed packed, phase of iron, which likely comprises the bulk composition of Earth's inner core. Using a nonmagnetic, moissanite anvil cell together with a superconducting magnetometer, we measured the remanent magnetization of iron in response to applied magnetic fields under pressure up to 21.5GPa at room temperature. Two independent experiments using different pressure transmission media reveal a higher remanent magnetization at 21.5GPa than at initial conditions, which could be attributed to a distorted hexagonal closed packed phase grown during the martensitic transition. Upon both compression and decompression, the remanent magnetization of the body centered cubic phase increases several times over initial conditions while the coercivity of remanence remains mostly invariant with pressure.
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