KH
Member Since 1991
Kei Hirose
Professor, University of Tokyo
AGU Research
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The Miscibility of H2 and H2O Investigated by Diamond Anvil Cell Experiments
THE ICE GIANTS: EXPLORING THE PLANETARY SYSTEMS OF URANUS AND NEPTUNE I POSTER
planetary sciences | 12 december 2024
Koutaro Hikosaka, Kei Hirose
A long-standing question about the ice giants is whether the interior is divided by well-defined boundaries. The conventional three-layer model assume...
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Development of Cryo SIMS Analytical Techniques for Fe-H Alloys
ADVANCED EXPERIMENTAL, COMPUTATIONAL, AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS II POSTER
mineral and rock physics | 11 december 2024
Nagi Ikuta, Naoya Sakamoto, Kei Hirose, Shoh Tagaw...
Hydrogen is likely to be an important light element in the metallic cores of terrestrial planets. In order to constrain core concentrations of hydroge...
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Iron-Helium Compounds Synthesized under High Pressure: Helium in the Planetary Cores?
EXPLORING PLANETARY INTERIORS: UNRAVELING THE DYNAMICS, THERMAL EVOLUTION, AND MINERALOGY FROM MANTLE TO CORE I POSTER
mineral and rock physics | 10 december 2024
Haruki Takezawa, Han Hsu, Kei Hirose, Fumiya Sakai...
While helium is a typical inert element, recent experiments (Bouhifd et al., 2013) and calculations (e.g., Wang et al., 2022) show the partitioning of...
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Fe-FeO Melting Phase Relations at Earth’s Core Conditions Obtained by Combining Multiple Approaches
EXPLORING PLANETARY INTERIORS: UNRAVELING THE DYNAMICS, THERMAL EVOLUTION, AND MINERALOGY FROM MANTLE TO CORE I POSTER
mineral and rock physics | 10 december 2024
Shunpei Yokoo, Koichiro Umemoto, Kei Hirose, Fumiy...
Phase relations of Fe-light-element alloys at high-pressure (P) and -temperature (T) conditions constrain the compositions of both the outer and inner...
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Dynamically Stable Iron-Helium Compounds (FeHex) under high pressure
EXPLORING PLANETARY INTERIORS: UNRAVELING THE DYNAMICS, THERMAL EVOLUTION, AND MINERALOGY FROM MANTLE TO CORE I POSTER
mineral and rock physics | 10 december 2024
Han Hsu, Haruki Takezawa, Kei Hirose, Fumiya Sakai...
The Earths core has been suggested as a reservoir of primordial helium (3He), providing a plausible explanation for the high 3He/4He ratio observed in...
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Melting behaviours of FeO and Fe-O-H alloys in the Earth’s deep interiors
EXPLORING PLANETARY INTERIORS: UNRAVELING THE DYNAMICS, THERMAL EVOLUTION, AND MINERALOGY FROM MANTLE TO CORE II ORAL
mineral and rock physics | 10 december 2024
Suyu Fu, Kei Hirose
The melting behaviour of materials within Earths interiors at high pressure and temperature (P-T) plays a key role in the physics, chemistry, and dyna...
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Liquid Density of FeS under Martian Core Conditions
EXPLORING PLANETARY INTERIORS: UNRAVELING THE DYNAMICS, THERMAL EVOLUTION, AND MINERALOGY FROM MANTLE TO CORE I POSTER
mineral and rock physics | 10 december 2024
Fumiya Sakai, Kei Hirose, Shunpei Yokoo, Suyu Fu
In recent years, the size and density of Mars core have been better understood through seismic observations by InSight spacecraft. The estimated core ...
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Hydrogen Isotope Fractionation During Core Formation and the Bulk Earth D/H Ratio
PROPERTIES, DYNAMICS, AND EVOLUTION OF TERRESTRIAL PLANETARY CORES: INTERDISCIPLINARY PERSPECTIVES I ORAL
study of earth's deep interior | 09 december 2024
Kei Hirose, NAOKI KURITA, Naoya Sakamoto, Shuhei M...
Hydrogen isotopic compositions provide important clues to elucidate the source of Earths water. Recent experiments and theories have revealed that hyd...
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