Spin transition, substitution, and partitioning of iron in lower mantle minerals

被引:13
|
作者
Fujino, Kiyoshi [1 ]
Nishio-Hamane, Daisuke [2 ]
Nagai, Takaya [3 ]
Seto, Yusuke [4 ]
Kuwayama, Yasuhiro [1 ]
Whitaker, Matthew [1 ,5 ]
Ohfuji, Hiroaki [1 ]
Shinmei, Toru [1 ]
Irifune, Tetsuo [1 ,6 ]
机构
[1] Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime 7908577, Japan
[2] Univ Tokyo, Inst Solid State Phys, Kashiwa, Chiba 2778581, Japan
[3] Hokkaido Univ, Dept Nat Hist Sci, Sapporo, Hokkaido 0600810, Japan
[4] Kobe Univ, Dept Earth & Planetary Sci, Kobe, Hyogo 6578501, Japan
[5] SUNY Stony Brook, Inst Mineral Phys, Stony Brook, NY 11794 USA
[6] Tokyo Inst Technol, Earth Life Sci Inst, Tokyo 1528550, Japan
基金
日本学术振兴会;
关键词
Lower mantle; Spin transition of iron; Mg-perovskite; Post-Mg-perovskite; Fe3+-Al coupled substitution; Iron-partitioning; POST-PEROVSKITE; FERROUS IRON; MOSSBAUER-SPECTROSCOPY; SYNCHROTRON MOSSBAUER; EARTHS MANTLE; FERRIC IRON; STATE; PHASE; PRESSURE; PYROLITE;
D O I
10.1016/j.pepi.2013.12.008
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
Spin transition and substitution of Fe3+ in Fe3+AlO3-bearing MgSiO3 perovskite (Pv) and post-perovskite (PPv) were examined up to 200 and 165 GPa, respectively, at room temperature by X-ray emission spectroscopy (XES) and XRD. The results of XES and XRD indicate that in Pv high spin (HS) Fe3+ at the dodecahedral (A) site replaces Al at the octahedral (B) site and becomes low spin (LS) between 50 and 70 GPa with pressure, while in PPv LS Fe3+ occupies the B-site and Al occupies the A-site above 80-100 GPa. The Fe3+ Al coupled substitution seems to be at work in both Pv and PPv. Combining these results on Fe3+ with the recent first-principles calculations on Fe2+ in Pv and PPv, the spin transition and substitution of iron in pyrolitic lower mantle minerals are proposed. Further, their effects on iron-partitioning among the lower mantle minerals are discussed. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:186 / 191
页数:6
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