Sound velocity of hcp-Fe at high pressure: experimental constraints, extrapolations and comparison with seismic models

被引:35
作者
Antonangeli, Daniele [1 ]
Ohtani, Eiji [2 ]
机构
[1] Univ Paris 06, Sorbonne Univ, Museum Natl Hist Nat, IMPMC,UMR CNRS 7590,IRD Unite 206, F-75252 Paris, France
[2] Tohoku Univ, Grad Sch Sci, Dept Earth & Planetary Mat Sci, Sendai, Miyagi 9808570, Japan
来源
PROGRESS IN EARTH AND PLANETARY SCIENCE | 2015年 / 2卷
关键词
Sound velocity measurements; High pressure; hcp-Fe; Extrapolation schemes; Earth's inner core; Comparison with seismic models; CLOSE-PACKED IRON; EARTHS INNER-CORE; GRUNEISEN-PARAMETER; BIRCHS LAW; GPA; TEMPERATURE; ELASTICITY; ALLOY; SCATTERING;
D O I
10.1186/s40645-015-0034-9
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Determining the sound velocity of iron under extreme thermodynamic conditions is essential for a proper interpretation of seismic observations of the Earth's core but is experimentally challenging. Here, we review techniques and methodologies used to measure sound velocities in metals at megabar pressures, with specific focus on the compressional sound velocity of hexagonal close-packed iron. A critical comparison of literature results, coherently analyzed using consistent metrology (pressure scale, equation of state), allows us to propose reference relations for the pressure and density dependence of the compressional velocity of hexagonal close-packed iron at ambient temperature. This provides a key base line upon which to add complexity, including high-temperature effects, pre-melting effects, effects of nickel and/or light element incorporation, necessary for an accurate comparison with seismic models, and ultimately to constrain Earth's inner core composition.
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页数:11
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