Sound velocity of Fe3C at high pressure and high temperature determined by inelastic X-ray scattering

被引:7
作者
Takahashi, Suguru [1 ]
Ohtani, Eiji [1 ]
Sakamaki, Tatsuya [1 ]
Kamada, Seiji [2 ]
Fukui, Hiroshi [3 ,4 ]
Tsutsui, Satoshi [5 ]
Uchiyama, Hiroshi [5 ]
Ishikawa, Daisuke [4 ,5 ]
Hirao, Naohisa [5 ]
Ohishi, Yasuo [5 ]
Baron, Alfred Q. R. [4 ]
机构
[1] Tohoku Univ, Grad Sch Sci, Dept Earth & Planetary Mat Sci, Sendai, Miyagi 9808578, Japan
[2] Tohoku Univ, Frontier Res Inst Interdisciplinary Sci, Sendai, Miyagi 9808578, Japan
[3] Univ Hyogo, Grad Sch Mat Sci, Ctr Novel Mat Sci Multiextreme Condit, Kamigori, Hyogo 6500044, Japan
[4] RIKEN SPring 8 Ctr, Mat Dynam Lab, Sayo, Hyogo 6795148, Japan
[5] Japan Synchrotron Radiat Res Inst JASRI, Sayo, Hyogo 6795198, Japan
关键词
Sound velocity; Fe3C; High pressure and high temperature; Inelastic X-ray scattering; Core; IRON; CORE; CARBON; GPA;
D O I
10.1016/j.crte.2018.09.005
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The sound velocity of Fe3C was measured at pressures from 33 to 86 GPa and at ambient and high temperatures up to 2300 K using inelastic X-ray scattering (IXS) from laser-heated samples in diamond anvil cells (DACs). The compressional velocity (V-P) and density of Fe3C at room temperature were observed to follow a linear relationship (Birch's law). The temperature dependency of Birch's law was not clearly observed and can be ignored. Birch's law for Fe3C is expressed by: V-P = 1.09(+/- 0.14) x rho-1.79(+/- 1.26). The result indicates that V-P and V-S (shear velocity) of the preliminary reference Earth model (PREM) inner core at the Inner Core Boundary (ICB) were by 12% and 48% smaller than those of Fe3C, which could be accounted for by the premelting effect by analogy from pure Fe or by partial melting of the Fe-Fe3C mixture in the inner core. (C) 2018 Academie des sciences. Published by Elsevier Masson SAS.
引用
收藏
页码:190 / 196
页数:7
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