Phase relations of Fe-Ni alloys at high pressure and temperature

被引:46
|
作者
Mao, WL
Campbell, AJ
Heinz, DL
Shen, GY
机构
[1] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
[2] Univ Chicago, Ctr Cosmochem, Chicago, IL 60637 USA
[3] Univ Chicago, James Franck Inst, Chicago, IL 60637 USA
[4] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[5] Carnegie Inst Sci, Geophys Lab, Washington, DC 20015 USA
基金
美国国家科学基金会;
关键词
iron-nickel alloys; earth's core; high pressure; diamond anvil cell; laser-heating; X-ray diffraction;
D O I
10.1016/j.pepi.2005.11.002
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
Using a diamond anvil cell and double-sided laser-heating coupled with synchrotron X-ray diffraction, we determined phase relations for three compositions of Fe-rich FeNi alloys in situ at high pressure and high temperature. We studied Fe with 5, 15, and 20 wt.% Ni to 55, 62, and 72 GPa, respectively, at temperatures up to similar to 3000 K. Ni stabilizes the face-centered cubic phase to lower temperatures and higher pressure, and this effect increases with increasing pressure. Extrapolation of our experimental results for Fe with 15 wt.% Ni suggests that the stable phase at inner core conditions is hexagonal close packed, although if the temperature at the inner core boundary is higher than similar to 6400 K, a two phase outer region may also exist. Comparison to previous laser-heated diamond anvil cell studies demonstrates the importance of kinetics even at high temperatures. Published by Elsevier B.V.
引用
收藏
页码:146 / 151
页数:6
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