Equation of State of Liquid Iron under Extreme Conditions

被引:80
作者
Kuwayama, Yasuhiro [1 ,2 ]
Morard, Guillaume [3 ,4 ]
Nakajima, Yoichi [5 ,6 ]
Hirose, Kei [1 ,7 ]
Baron, Alfred Q. R. [6 ]
Kawaguchi, Saori, I [8 ]
Tsuchiya, Taku [2 ]
Ishikawa, Daisuke [6 ,8 ]
Hirao, Naohisa [8 ]
Ohishi, Yasuo [8 ]
机构
[1] Univ Tokyo, Dept Earth & Planetary Sci, Tokyo 1130033, Japan
[2] Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, Japan
[3] Sorbonne Univ, CNRS, Museum Natl Hist Nat, UMR,IMPMC, F-7590 Paris, France
[4] Univ Grenoble Alpes, Univ Savoie Mt Blanc, CNRS, IRD,IFSSTAR,ISTerre, F-38000 Grenoble, France
[5] Kumamoto Univ, Dept Phys, Kumamoto 8608555, Japan
[6] RIKEN SPring 8 Ctr, Mat Dynam Lab, Sayo, Hyogo 6795148, Japan
[7] Earth Life Sci Inst, Tokyo Inst Technol, Tokyo 1528550, Japan
[8] Japan Synchrotron Radiat Res Inst, SPring 8, Sayo, Hyogo 6795198, Japan
关键词
DENSITY-MEASUREMENTS; CORE CONDITIONS; SOUND-VELOCITY; HIGH-PRESSURES; EARTHS; TEMPERATURE; FE; RESISTIVITY; METALS;
D O I
10.1103/PhysRevLett.124.165701
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The density of liquid iron has been determined up to 116 GPa and 4350 K via static compression experiments following an innovative analysis of diffuse scattering from liquid. The longitudinal sound velocity was also obtained to 45 GPa and 2700 K based on inelastic x-ray scattering measurements. Combining these results with previous shock-wave data, we determine a thermal equation of state for liquid iron. It indicates that Earth's outer core exhibits 7.5%-7.6% density deficit, 3.7%-4.4% velocity excess, and an almost identical adiabatic bulk modulus, with respect to liquid iron.
引用
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页数:6
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