Partitioning of potassium between iron and silicate at the core-mantle boundary

Naohisa Hirao, Eiji Ohtani, Tadashi Kondo, Noriaki Endo, Toshiko Kuba, Toshiaki Suzuki, Takumi Kikegawa

研究成果: Article査読

17 被引用数 (Scopus)

抄録

Chemical reactions and the partitioning of potassium between metallic iron and potassium-silicate were studied at the core-mantle boundary (CMB) condition, 2900 km deep in the Earth, in a laser-heated diamond-anvil cell (LHDAC). Analytical transmission electron microscope (ATEM) analysis of the recovered samples from 134 GPa and 3500 K, prepared with Focused Ion Beam (FIB) techniques, revealed significant dissolution of potassium (0.8 wt.%) into molten iron, indicating that the partition coefficient of potassium between iron and silicate is 0.15. Our results show that the Earth's core can contain 35 ppm total potassium, i.e., 4.1 × 10-3 PPM of 40K, which could serve as a heat source corresponding to 0.23 TW in the Earth's core.

本文言語English
論文番号L08303
ジャーナルGeophysical Research Letters
33
8
DOI
出版ステータスPublished - 2006 4 28

ASJC Scopus subject areas

  • 地球物理学
  • 地球惑星科学(全般)

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