globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2020.116382
论文题名:
Eutectic melting of Fe-3 at% Si-4 at% C up to 200 GPa and implications for the Earth's core
作者: Miozzi F.; Morard G.; Antonangeli D.; Baron M.A.; Boccato S.; Pakhomova A.; Garbarino G.; Mezouar M.; Fiquet G.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2020
卷: 544
语种: 英语
中文关键词: carbon ; core ; high pressure ; light elements ; melting ; silicon
英文关键词: Acoustic wave velocity ; Calculations ; High pressure effects ; Iron alloys ; Melting point ; Shear flow ; Silicates ; Ab initio calculations ; Combined effect ; Core-mantle boundary ; Eutectic melting ; Hexagonal structures ; High temperature ; In-situ X-ray diffraction ; Shear sound velocities ; Silicon ; carbon ; core (planetary) ; core-mantle boundary ; Earth structure ; iron ; melting ; P-T conditions ; petrology ; silicate ; silicon
英文摘要: Properties of the Fe-Si and Fe-C binary systems have been shown unable to satisfy the geophysical and petrological constraints of the Earth's core (i.e. velocities, densities, melting temperature) if only Si or C were to be incorporated as light element. Recent ab initio calculations suggest on the contrary that density, compressional and shear sound velocities, as well as the Poisson's ratio of the inner core could be matched by an hcp-Fe alloy containing Si and C. The combined effect of the two elements in a ternary Fe-Si-C system has never been experimentally investigated under high pressure. We thus studied the melting curve and the phase relations of the ternary iron-silicon-carbon system by in situ X-ray diffraction at high pressures and high temperatures. Starting with a low light element content (4 at% C-3 at% Si), a stable assemblage made of hcp Fe (+Si, +C) and Fe3C is observed up to 200 GPa. Fe can incorporate both Si and C in its hexagonal structure, with the latter strongly affecting the volume and the melting temperature. While the presence of a third light element is likely necessary, we here document that the effect of C in lowering the melting temperature of Fe-Si, is large enough to possibly keep the core-mantle boundary temperature below the solidus of the mantle silicates. © 2020 Elsevier B.V.
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被引频次[WOS]:8   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165168
Appears in Collections:气候变化与战略

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作者单位: Sorbonne Université, UMR CNRS 7590, Muséum National d'Histoire Naturelle, Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, IMPMC, Paris, 75005, France; Deutsches Elektronen-Synchrotron (DESY), Hamburg, Germany; European Synchrotron Radiation Facility (ESRF), Grenoble, France

Recommended Citation:
Miozzi F.,Morard G.,Antonangeli D.,et al. Eutectic melting of Fe-3 at% Si-4 at% C up to 200 GPa and implications for the Earth's core[J]. Earth and Planetary Science Letters,2020-01-01,544
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