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Osmotic energy conversion in serpentinite-hosted deep-sea hydrothermal vents

Author

Listed:
  • Hye-Eun Lee

    (RIKEN Center for Sustainable Resource Science
    Tokyo Institute of Technology)

  • Tomoyo Okumura

    (Kochi University)

  • Hideshi Ooka

    (RIKEN Center for Sustainable Resource Science)

  • Kiyohiro Adachi

    (RIKEN Center for Emergent Matter Science)

  • Takaaki Hikima

    (RIKEN SPring-8 Center)

  • Kunio Hirata

    (RIKEN SPring-8 Center)

  • Yoshiaki Kawano

    (RIKEN SPring-8 Center)

  • Hiroaki Matsuura

    (RIKEN SPring-8 Center)

  • Masaki Yamamoto

    (RIKEN SPring-8 Center)

  • Masahiro Yamamoto

    (Japan Agency for Marine-Earth Science and Technology)

  • Akira Yamaguchi

    (RIKEN Center for Sustainable Resource Science
    Tokyo Institute of Technology)

  • Ji-Eun Lee

    (RIKEN Center for Sustainable Resource Science)

  • Hiroya Takahashi

    (RIKEN Center for Sustainable Resource Science
    Tokyo Institute of Technology)

  • Ki Tae Nam

    (Seoul National University)

  • Yasuhiko Ohara

    (Japan Agency for Marine-Earth Science and Technology
    Hydrographic and Oceanographic Department of Japan
    Nagoya University)

  • Daisuke Hashizume

    (RIKEN Center for Emergent Matter Science)

  • Shawn Erin McGlynn

    (RIKEN Center for Sustainable Resource Science
    Tokyo Institute of Technology)

  • Ryuhei Nakamura

    (RIKEN Center for Sustainable Resource Science
    Tokyo Institute of Technology)

Abstract

Cells harvest energy from ionic gradients by selective ion transport across membranes, and the same principle is recently being used for osmotic power generation from salinity gradients at ocean-river interfaces. Common to these ionic gradient conversions is that they require intricate nanoscale structures. Here, we show that natural submarine serpentinite-hosted hydrothermal vent (HV) precipitates are capable of converting ionic gradients into electrochemical energy by selective transport of Na+, K+, H+, and Cl-. Layered hydroxide nanocrystals are aligned radially outwards from the HV fluid channels, constituting confined nanopores that span millimeters in the HV wall. The nanopores change the surface charge depending on adsorbed ions, allowing the mineral to function as a cation- and anion-selective ion transport membrane. Our findings indicate that chemical disequilibria originating from flow and concentration gradients in geologic environments generate confined nanospaces which enable the spontaneous establishment of osmotic energy conversion.

Suggested Citation

  • Hye-Eun Lee & Tomoyo Okumura & Hideshi Ooka & Kiyohiro Adachi & Takaaki Hikima & Kunio Hirata & Yoshiaki Kawano & Hiroaki Matsuura & Masaki Yamamoto & Masahiro Yamamoto & Akira Yamaguchi & Ji-Eun Lee , 2024. "Osmotic energy conversion in serpentinite-hosted deep-sea hydrothermal vents," Nature Communications, Nature, vol. 15(1), pages 1-12, December.
    • Handle: RePEc:nat:natcom:v:15:y:2024:i:1:d:10.1038_s41467-024-52332-3
    DOI: 10.1038/s41467-024-52332-3
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    References listed on IDEAS

    as
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