Member Since 2015
Takayuki Ishii
Associate professor, Institute for Planetary Materials, Okayama University
Professional Experience
Institute for Planetary Materials, Okayama University
Associate professor
2023 - Present
University of Bayreuth
Postdoctoral fellow
2015 - 2023
NASA DEVELOP
Postdoctoral fellow
2015 - 2015
University of Bayreuth
Postdoctoral fellow
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Education
Gakushuin University
Doctorate
Honors & Awards
Mineral and Rock Physics Early Career Award
Received December 2021
Publications
Temperature Dependence of H2O Solubility in Al‐Free Stishovite

The role of stishovite in transporting water in subducting slabs has been a subject of debate for several decades. Here we investigated stishovite'...

February 01, 2024
AGU Abstracts
Water solubility of aluminous silicas at lower mantle conditions and their implication for water cycle in the deep mantle
THERMODYNAMIC PROPERTIES OF PLANETARY MATERIALS II ORAL
mineral and rock physics | 11 december 2023
Takayuki Ishii, Giacomo Criniti, Eiji Ohtani, Hong...
Determinations of the water solubility of nominally anhydrous minerals and thermal stability of hydrous minerals is crucial for understanding the stru...
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Recent developments of large-volume multi-anvil technologies for advanced high-pressure-temperature research
ADVANCED EXPERIMENTAL, COMPUTATIONAL AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS III ORAL
mineral and rock physics | 15 december 2022
Tomoo Katsura, Hongzhan Fei, Takayuki Ishii, Zhaod...
The large-volume multi-anvil press (MAP) is a relatively reliable high pressure (P) - temperature (T) apparatus but has various limitations. We have t...
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Hydrogen Bonding and Spin State of (Al,Fe)-bearing Phase H at High Pressure
TOWARD AN INTERDISCIPLINARY UNDERSTANDING ON THE STRUCTURE, COMPOSITION, AND DYNAMIC EVOLUTION OF THE LOWER MANTLE III POSTER
study of earth's deep interior | 15 december 2022
Benjamin Strozewski, Johannes Buchen, Wolfgang Stu...
Oxyhydroxide phases in the (Al,Fe)OOHMgSiO2(OH)2 system have been found to coexist with bridgmanite and retain hydrogen in their crystal structures at...
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