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The pyrite-type high-pressure form of FeOOH

Author

Listed:
  • Masayuki Nishi

    (Geodynamics Research Center, Ehime University
    Earth-Life Science Institute, Tokyo Institute of Technology)

  • Yasuhiro Kuwayama

    (Geodynamics Research Center, Ehime University
    School of Science, University of Tokyo)

  • Jun Tsuchiya

    (Geodynamics Research Center, Ehime University
    Earth-Life Science Institute, Tokyo Institute of Technology)

  • Taku Tsuchiya

    (Geodynamics Research Center, Ehime University
    Earth-Life Science Institute, Tokyo Institute of Technology)

Abstract

The pyrite-type high-pressure form of FeOOH is predicted from first principles, and found experimentally to be stable under the conditions at the base of the mantle, with implications for transport of water within Earth’s deep interior.

Suggested Citation

  • Masayuki Nishi & Yasuhiro Kuwayama & Jun Tsuchiya & Taku Tsuchiya, 2017. "The pyrite-type high-pressure form of FeOOH," Nature, Nature, vol. 547(7662), pages 205-208, July.
    • Handle: RePEc:nat:nature:v:547:y:2017:i:7662:d:10.1038_nature22823
    DOI: 10.1038/nature22823
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    Cited by:

    1. Hanyu Wang & Lei Liu & Zihan Gao & Longxing Yang & Gerile Naren & Shide Mao, 2024. "Structure and elasticity of CaC2O5 suggests carbonate contribution to the seismic anomalies of Earth’s mantle," Nature Communications, Nature, vol. 15(1), pages 1-9, December.
    2. Katsutoshi Kawano & Masayuki Nishi & Hideharu Kuwahara & Sho Kakizawa & Toru Inoue & Tadashi Kondo, 2024. "Extensive iron–water exchange at Earth’s core–mantle boundary can explain seismic anomalies," Nature Communications, Nature, vol. 15(1), pages 1-8, December.

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