What is he best known for?
The fields of study he is best known for:
- Thermodynamics
- Hydrogen
- Mineral
His primary areas of study are Mineralogy, Mantle, Analytical chemistry, Silicate and Olivine.
His research integrates issues of Thermodynamics, Chemical composition, Mineral redox buffer and Silicate perovskite in his study of Mineralogy.
He has included themes like Astrobiology, Mars Exploration Program, Planetesimal and Transition zone in his Mantle study.
His work carried out in the field of Analytical chemistry brings together such families of science as Phase transition, Perovskite, Fugacity and Magnesium.
The various areas that he examines in his Silicate study include Geochemistry, Crystallization and Metal.
His Olivine research includes themes of Nucleation, Buoyancy, Latent heat, Spinel and Forsterite.
His most cited work include:
- Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 (775 citations)
- Experimental evidence for the existence of iron-rich metal in the Earth's lower mantle (423 citations)
- Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere (420 citations)
What are the main themes of his work throughout his whole career to date?
David C. Rubie spends much of his time researching Mineralogy, Mantle, Silicate, Analytical chemistry and Metal.
David C. Rubie interconnects Ferropericlase, Silicate perovskite and Thermodynamics in the investigation of issues within Mineralogy.
While the research belongs to areas of Mantle, he spends his time largely on the problem of Transition zone, intersecting his research to questions surrounding Mantle wedge.
He usually deals with Silicate and limits it to topics linked to Planetesimal and Mars Exploration Program and Protoplanetary disk.
His Analytical chemistry research includes elements of Perovskite, Mineral redox buffer, Diffusion and Solubility.
His studies deal with areas such as Earth and Core formation as well as Metal.
He most often published in these fields:
- Mineralogy (44.12%)
- Mantle (33.82%)
- Silicate (30.39%)
What were the highlights of his more recent work (between 2013-2021)?
- Astrobiology (10.78%)
- Mantle (33.82%)
- Planet (7.35%)
In recent papers he was focusing on the following fields of study:
His primary areas of investigation include Astrobiology, Mantle, Planet, Silicate and Terrestrial planet.
His studies in Astrobiology integrate themes in fields like Planetary differentiation, Geophysics and Earth.
The Mantle study combines topics in areas such as Internal energy, Thermodynamics, Buoyancy, Mass ratio and Petrology.
His Silicate research is multidisciplinary, relying on both Density contrast, Mineral redox buffer, Metal, Mineralogy and Liquid metal.
His Metal study combines topics from a wide range of disciplines, such as Geochemistry, Core formation and Analytical chemistry.
He is involved in the study of Mineralogy that focuses on Olivine in particular.
Between 2013 and 2021, his most popular works were:
- Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water (205 citations)
- Highly siderophile elements in Earth’s mantle as a clock for the Moon-forming impact (151 citations)
- Oxygen isotopic evidence for vigorous mixing during the Moon-forming giant impact (122 citations)
In his most recent research, the most cited papers focused on:
- Thermodynamics
- Hydrogen
- Mineral
David C. Rubie focuses on Mantle, Astrobiology, Planet, Mineralogy and Silicate.
His Mantle study incorporates themes from Metal and Petrology.
The concepts of his Astrobiology study are interwoven with issues in Terrestrial planet and Planetary differentiation.
His Mineralogy study integrates concerns from other disciplines, such as Diamond anvil cell and Isotopes of oxygen.
His Silicate research incorporates elements of Iron sulfide, Density contrast, Crystallization and Olivine.
In his work, Sulfur, Sulfide and Fugacity is strongly intertwined with Analytical chemistry, which is a subfield of Core formation.
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