Pressure-induced magnetization in FeO: Evidence from elasticity and Mossbauer spectroscopy

被引:46
作者
Kantor, AP [1 ]
Jacobsen, SD
Kantor, IY
Dubrovinsky, LS
McCammon, CA
Reichmann, HJ
Goncharenko, IN
机构
[1] Bayer Geoinst, D-95440 Bayreuth, Germany
[2] Moscow MV Lomonosov State Univ, Dept Crystallog & Crystal Chem, Moscow 119992, Russia
[3] Carnegie Inst Washington, Geophys Lab, Washington, DC 20015 USA
[4] Geoforschungszentrum Potsdam, Sect 4 1, D-14473 Potsdam, Germany
[5] CEA Saclay, Leon Brillouin Lab, F-91191 Gif Sur Yvette, France
基金
美国国家科学基金会; 俄罗斯基础研究基金会;
关键词
D O I
10.1103/PhysRevLett.93.215502
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The complete elastic tensor of Fe0.94O (wustite) has been determined to 10 GPa using acoustic interferometry at GHz frequencies inside a diamond-anvil cell. The soft mode (C-44) elastic constant of FeO is reduced by 20% over the experimental pressure range. An unusual discontinuity in the pressure derivatives of C-11 and C-12 at 4.7+/-0.2 GPa corresponds to the pressure at which the onset of a magnetic ordering transition is observed by high-pressure Mossbauer spectroscopy and neutron powder diffraction. Our new results combined with literature structural high P-T data suggest that there is a magnetic, although still cubic, phase of FeO between similar to5 and similar to17 GPa.
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页数:4
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