2023 - Research.com Earth Science in Japan Leader Award
2022 - Research.com Earth Science in Japan Leader Award
2009 - Fellow of American Geophysical Union (AGU)
His primary areas of study are Mineralogy, Mantle, Post-perovskite, Phase transition and Core–mantle boundary. His research in Mineralogy intersects with topics in Thermal, Outer core, X-ray crystallography, Analytical chemistry and Solidus. His studies deal with areas such as Oceanic crust, Basalt, Transition zone and Crust as well as Mantle.
In Post-perovskite, Kei Hirose works on issues like Condensed matter physics, which are connected to Inner core, Seismic anisotropy, Anisotropy and Elasticity. His work deals with themes such as Phase boundary, Discontinuity and Diffraction, which intersect with Phase transition. Kei Hirose has included themes like Ferropericlase, Seismic wave, Mantle convection, Structure of the Earth and Silicate perovskite in his Core–mantle boundary study.
Kei Hirose mainly focuses on Mantle, Mineralogy, Phase transition, Analytical chemistry and Diamond anvil cell. He interconnects Petrology and Transition zone in the investigation of issues within Mantle. His Mineralogy study also includes fields such as
Kei Hirose has researched Phase transition in several fields, including Crystallography, Phase boundary and X-ray crystallography. Kei Hirose combines subjects such as Inner core and Diffraction with his study of Crystallography. His Condensed matter physics research integrates issues from Thermal conductivity and Anisotropy.
Thermodynamics, Earth, Thermal conductivity, Core and Diamond anvil cell are his primary areas of study. His Thermal conductivity study incorporates themes from Thermal, Periclase, Perovskite, Silicate perovskite and Condensed matter physics. The concepts of his Core study are interwoven with issues in Phase transition, Liquidus, Ternary numeral system, Molecular physics and Mineralogy.
His Diamond anvil cell study combines topics from a wide range of disciplines, such as Composite material, Semiconductor and Analytical chemistry. His Analytical chemistry research is multidisciplinary, incorporating elements of Mineral physics, Post-perovskite, Mantle and Magnesium silicate. His study in the fields of Core–mantle boundary under the domain of Mantle overlaps with other disciplines such as Temperature gradient.
The scientist’s investigation covers issues in Thermodynamics, Earth, Outer core, Diamond anvil cell and Inner core. When carried out as part of a general Thermodynamics research project, his work on Static compression, Equation of state, Volume and Mixing is frequently linked to work in Molecular dynamics, therefore connecting diverse disciplines of study. His Diamond anvil cell research incorporates themes from Mössbauer spectroscopy and Analytical chemistry.
His Analytical chemistry research integrates issues from Core–mantle boundary, Extrapolation and Melting point. His study with Pyrolite involves better knowledge in Mantle. His study in Mantle is interdisciplinary in nature, drawing from both Chemical physics and Silicate.
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Post-Perovskite Phase Transition in MgSiO3
Motohiko Murakami;Kei Hirose;Katsuyuki Kawamura;Nagayoshi Sata.
Partial melting of dry peridotites at high pressures: Determination of compositions of melts segregated from peridotite using aggregates of diamond
Kei Hirose;Ikuo Kushiro.
Earth and Planetary Science Letters (1993)
Hydrous partial melting of lherzolite at 1 GPa: The effect of H2O on the genesis of basaltic magmas
Kei Hirose;Tatsuhiko Kawamoto.
Earth and Planetary Science Letters (1995)
The structure of iron in Earth's inner core.
Shigehiko Tateno;Shigehiko Tateno;Kei Hirose;Kei Hirose;Yasuo Ohishi;Yoshiyuki Tatsumi.
The fate of subducted basaltic crust in the Earth's lower mantle
Kei Hirose;Yingwei Fei;Yanzhang Ma;Ho-Kwang Mao.
Melting experiments on lherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts
Stagnant slab : A review
Yoshio Fukao;Tomoeki Nakakuki;Hisashi Utada;Daisuke Suetsugu.
Annual Review of Earth and Planetary Sciences (2009)
Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications
Y Fei;J Van Orman;J Van Orman;J Li;J Li;W van Westrenen;W van Westrenen.
Journal of Geophysical Research (2004)
Phase transitions in pyrolitic mantle around 670‐km depth: Implications for upwelling of plumes from the lower mantle
Journal of Geophysical Research (2002)
Investigations of lithium–sulfur batteries using electrochemical impedance spectroscopy
Natalia A. Cañas;Natalia A. Cañas;Kei Hirose;Brigitta Pascucci;Brigitta Pascucci;Norbert Wagner.
Electrochimica Acta (2013)
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