Eiji Ohtani

Emeritus Professor

Tohoku University

Japan

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Professor Eiji Ohtani is an Emeritus Professor at Tohoku University in Japan. His research focuses on the roles of water in the dynamics of subducting slabs and surrounding mantle, as well as the implications of mineral compositions and phase behaviors in Earth's core and lower mantle. Recent publications include studies on hydrous minerals in subducting slabs, sound velocities in iron alloys, and water transport in high-temperature environments.

Articles (14)

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2025

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2025

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2024

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2023

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2023

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2022

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2022

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2022

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2022

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2022

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2022

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2022

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2021

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2021

Collaborators (8)

Tatsuya Sakamaki

Tohoku University

JAPAN

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Masaaki Miyahara

Hiroshima University

JAPAN

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Takayuki Ishii

Associate Professor

JAPAN

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Daisuke Ishikawa

Japan Synchrotron Radiation Research Institute (JASRI)

JAPAN

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Jun Tsuchiya

associate professor

Ehime University

JAPAN

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Daijo IKUTA

Okayama University

JAPAN

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Hiroshi Fukui

Japan Synchrotron Radiation Research Institute

JAPAN

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Vincenzo Stagno

Associate Professor

Sapienza University of Rome

ITALY

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Eiji Ohtani

Research Interests

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About

Articles (14)

Sound Velocities of the Hydrous Iron‐Rich HH1‐Phase: Implications for Lower Mantle Seismic Heterogeneities

Limited water contents of wadsleyite and ringwoodite coexisting with hydrous minerals in cold subducting slabs

Role of water in dynamics of slabs and surrounding mantle

Density deficit of Earth's core revealed by a multimegabar primary pressure scale

Mn‐Precipitates Found in a Martian Crustal Rock

Superhydrous aluminous silica phases as major water hosts in high-temperature lower mantle

Sound velocity of hexagonal close-packed iron to the Earth's inner core pressure

Sound velocity measurements of B2-Fe-Ni-Si alloy under high pressure by inelastic x-ray scattering: Implications for the composition of Earth's core

Experimental simulations of shock textures in BCC iron: implications for iron meteorites

Formation of an Al‐Rich Niccolite‐Type Silica in Subducted Oceanic Crust: Implications for Water Transport to the Deep Lower Mantle

Low Thermal Conductivity of Hydrous Phase D Leads to a Self‐Preservation Effect Within a Subducting Slab

The Earth's Interior: From the Perspective of Mineral Science

Natural Fe-bearing aluminous bridgmanite in the Katol L6 chondrite

Dry metastable olivine and slab deformation in a wet subducting slab

Collaborators (8)

Tatsuya Sakamaki

Masaaki Miyahara

Takayuki Ishii

Daisuke Ishikawa

Jun Tsuchiya

Daijo IKUTA

Hiroshi Fukui

Vincenzo Stagno

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