Research Highlights

Is the Earth’s inner core oscillating and translating anomalously? (Apr.14, 2020)

Schematic illustration of the Earth’s internal structure


A theoretical mineral physics approach based on the ab initio methods was adopted to determine the viscosity of hexagonal, close-packed iron at the extreme pressures and temperatures corresponding to the Earth’s inner core. The results are found to deny geophysical observations of large fluctuations in the inner core rotation rate. The obtained viscosity also rules out inner core translation and provides support that the dynamics of the inner core may be governed by solid-state convection. (Sebastian Ritterbex)
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Quantum mechanical simulations of Earth’s lower mantle minerals (Mar.03, 2020)

Lower mantle minerals


The theoretical mineral physics group of Ehime University led by Dr. Taku Tsuchiya has developed high-precision computational techniques for studying Earth and planetary materials based on quantum mechanical theory and reported several outcomes for Earth’s lower mantle minerals and high-pressure hydrous phases. Their insights and discoveries clarify the mineralogy of Earth’s lower mantle and new mineral phases stabilized at the deep mantle.(Taku Tsuchiya)
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Heat transport property at the lowermost part of the Earth’s mantle (Feb.13, 2020)

Calculated lattice thermal conductivity of MgSiO3 postperovskite (PPv) and bridgmanite (Brg) under the Earth’s lowermost mantle conditions


Lattice thermal conductivities of MgSiO3 bridgmanite and postperovskite (PPv) phases under the Earth’s deepest mantle conditions were determined by quantum mechanical computer simulations. We found a substantial increase in the conductivity associated with the phase change. This indicates that the PPv phase boundary is the boundary not only of the mineralogy but also the thermal conductivity. The effect of anisotropy on the conductivity of PPv in the heat transport properties at the lowermost mantle was also found to be minor.(Haruhiko Dekura)
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New aluminium hydroxide stable at extremely high pressure (Dec.11, 2019)

The crystal structure of ε-AlOOH


A new hydrous phase, ε-AlOOH, was observed to be stable at pressures above ~200 GPa. The stability of ε-AlOOH at extremely high pressures may affect the modelling results of the internal structure and deep water circulation of some extra-solar planets, such as terrestrial super-Earths, because the hydroxide may store water in these regions.(Masayuki Nishi)
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How and when was carbon distributed in the Earth? (Sep.24, 2019)

The electron micrograph of the recovered sample


A magma ocean existing during the core formation is thought to have been highly depleted in carbon due to its high-siderophile (iron loving) behavior. Thus, most of the carbon forming the atmosphere and life on Earth may have been delivered by a carbon-rich embryo after the core formation. However, a new high-pressure experiment has shown that previous studies may have overestimated the amount of carbon partitioning to the core. (Hideharu Kuwahara)
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Circulation of water in deep Earth’s interior(Aug.19, 2019)

Hydrous minerals in the Earth’s interior


Phase H is a hydrous mineral that is considered to be an important carrier of water into deep Earth. We determined the dissociation condition of phase H by a theoretical calculation based on quantum mechanics. Phase H decomposes at approximately 60 GPa at 1000 K. This indicates that the transportation of water by phase H may be terminated at a depth of approximately 1,500 km in the middle of the lower mantle. (Jun Tsuchiya)
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Why is the Earth’s F/Cl ratio not chondritic?(Jul.1, 2019)

The electron micrograph of the recovered sample


It is believed that terrestrial planets were made from chondrites. However, geochemical observations have shown that the abundance pattern of volatile elements, such as F and Cl in the Earth is inconsistent with chondrites. New high-pressure experiments suggest that F and Cl fractionation during magma ocean crystallization could explain the non-chondritic Earth’s F/Cl ratio. (Hideharu Kuwahara)
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Fate of the subducted oceanic crust revealed by laboratory experiments (Jan.31, 2019)

Subducted Oceanic Crusts


Laboratory experiments at extreme pressures and temperatures lead to precise measurements of the sound velocity of CaSiO3 perovskite which is one of the important constituent minerals in the Earth’s mantle. The measurements suggested the accumulation of the subducted oceanic crust beneath the 660 km discontinuity. (Steeve Gréaux)
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