Experimental study and thermodynamic calculations of phase relations in the Fe-C system at high pressure

被引:95
作者
Fei, Yingwei [1 ]
Brosh, Eli [2 ]
机构
[1] Carnegie Inst Sci, Geophys Lab, Washington, DC 20015 USA
[2] NRCN, IL-84190 Beer Sheva, Israel
基金
美国国家科学基金会;
关键词
high-pressure phase relation; thermodynamic model; iron-carbon system; Earth's core; Fe-C melting; EQUATION-OF-STATE; LIQUID CARBON; EARTHS CORE; IRON; GRAPHITE; DIAMOND; TEMPERATURE; BOUNDARY; DIAGRAM; GROWTH;
D O I
10.1016/j.epsl.2014.09.044
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We have conducted a series of melting experiments in the Fe-C system at pressures up to 25 GPa in the temperature range of 1473-2073 K. The results define the phase relations at several pressures, including the eutectic temperature and composition as a function of pressure, carbon partitioning between solid iron and liquid, and change of melting relations involving iron carbides. In order to interpolate and extrapolate the phase relations over a wide pressure and temperature range, we have established a comprehensive thermodynamic model in the Fe-C binary system. The calculated phase diagrams at pressures of 5, 10, and 20 GPa reproduce the experimental data, including the solubility of carbon in solid iron and the effect of pressure on the eutectic temperature and composition. The formation of Fe7C3 at pressures above 5 GPa is correctly modeled and the change of phase relations in the Fe-C system between 5 and 10 GPa is captured in the model. The model provides predictions of the phase relations at 136 GPa and 330 GPa, based on existing knowledge of the thermochemistry of the system at lower pressure. The calculated phase relations can be used to understand the role of carbon during inner core crystallization, predicting carbon distribution between the inner and outer cores and mineralogy of the solid inner core. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:155 / 162
页数:8
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