D-Index & Metrics Best Publications

D-Index & Metrics

Discipline name D-index D-index (Discipline H-index) only includes papers and citation values for an examined discipline in contrast to General H-index which accounts for publications across all disciplines. Citations Publications World Ranking National Ranking
Earth Science D-index 72 Citations 17,882 204 World Ranking 350 National Ranking 6

Research.com Recognitions

Awards & Achievements

2009 - Fellow of American Geophysical Union (AGU)

Overview

What is he best known for?

The fields of study he is best known for:

  • Hydrogen
  • Thermodynamics
  • Mineralogy

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.

His most cited work include:

  • Post-Perovskite Phase Transition in MgSiO3 (1028 citations)
  • Partial melting of dry peridotites at high pressures: Determination of compositions of melts segregated from peridotite using aggregates of diamond (749 citations)
  • Hydrous partial melting of lherzolite at 1 GPa: The effect of H2O on the genesis of basaltic magmas (371 citations)

What are the main themes of his work throughout his whole career to date?

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

  • Ferropericlase which is related to area like Silicate perovskite,
  • Partial melting that connect with fields like Peridotite.

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.

He most often published in these fields:

  • Mantle (35.53%)
  • Mineralogy (35.73%)
  • Phase transition (31.14%)

What were the highlights of his more recent work (between 2018-2021)?

  • Thermodynamics (23.75%)
  • Earth (15.57%)
  • Thermal conductivity (14.17%)

In recent papers he was focusing on the following fields of study:

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.

Between 2018 and 2021, his most popular works were:

  • Melting curve of iron to 290 GPa determined in a resistance-heated diamond-anvil cell (28 citations)
  • Melting curve of iron to 290 GPa determined in a resistance-heated diamond-anvil cell (28 citations)
  • New developments in high-pressure X-ray diffraction beamline for diamond anvil cell at SPring-8 (24 citations)

In his most recent research, the most cited papers focused on:

  • Hydrogen
  • Thermodynamics
  • Mineral

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.

This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.

Best Publications

Post-Perovskite Phase Transition in MgSiO3

Motohiko Murakami;Kei Hirose;Katsuyuki Kawamura;Nagayoshi Sata.
Science (2004)

1333 Citations

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)

955 Citations

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)

518 Citations

The structure of iron in Earth's inner core.

Shigehiko Tateno;Kei Hirose;Kei Hirose;Yasuo Ohishi;Yoshiyuki Tatsumi.
Science (2010)

388 Citations

The fate of subducted basaltic crust in the Earth's lower mantle

Kei Hirose;Yingwei Fei;Yanzhang Ma;Ho-Kwang Mao.
Nature (1999)

380 Citations

Melting experiments on lherzolite KLB-1 under hydrous conditions and generation of high-magnesian andesitic melts

Kei Hirose.
Geology (1997)

351 Citations

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)

329 Citations

Stagnant slab : A review

Yoshio Fukao;Tomoeki Nakakuki;Hisashi Utada;Daisuke Suetsugu.
Annual Review of Earth and Planetary Sciences (2009)

319 Citations

Phase transitions in pyrolitic mantle around 670‐km depth: Implications for upwelling of plumes from the lower mantle

Kei Hirose.
Journal of Geophysical Research (2002)

313 Citations

Post-Perovskite Phase Transition

Motohiko Murakami;Kei Hirose;Katsuyuki Kawamura;Nagayoshi Sata.
(2004)

307 Citations

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