Hitoshi MIURA

| Division | Mathematical and Material Science, Associate Professor |
|---|---|
| Academic Degree | Ph.D. |
Contents of page
Research Field
Planetary Science, Theory of Crystal Growth
Keywords
Crystal Growth, Solar System Small Bodies, Astrophysics, Chondrules, Semiconductors, Minerals, Phase-Field Method
Current Research Topics
(1) Evolution of Solid Matter in the Early Solar System:
Today, a wide variety of crystals exist on Earth. Furthermore, extraterrestrial materials such as meteorites also contain various crystals. However, it is believed that almost all of the interstellar matter from which these crystals originated was amorphous. When, where, and how did this amorphous material crystallise during the formation of the Sun and planetary systems? To address this question, we are conducting research using physical modelling and numerical simulations, focusing primarily on the heating of solid matter caused by interactions between gas discs and solid matter.
Today, a wide variety of crystals exist on Earth. Furthermore, extraterrestrial materials such as meteorites also contain various crystals. However, it is believed that almost all of the interstellar matter from which these crystals originated was amorphous. When, where, and how did this amorphous material crystallise during the formation of the Sun and planetary systems? To address this question, we are conducting research using physical modelling and numerical simulations, focusing primarily on the heating of solid matter caused by interactions between gas discs and solid matter.
(2) The Evolutionary Process of Solar System Small Bodies
Asteroids and comets are types of small bodies in the Solar System. Traditionally, asteroids and comets were clearly distinguished from one another. That is to say, asteroids consist mainly of rock, whilst comets consist mainly of ice. However, in recent years, small bodies possessing characteristics of both asteroids and comets have been discovered. This suggests that asteroids and comets are not entirely distinct types, but rather that comets may have lost their ice during the course of their evolution, taking on an asteroid-like appearance. Such celestial bodies are known as Comet-Asteroid Transition Objects (CAT objects). How do comets become asteroids, and how long does this process take? To address this question, we are investigating the long-term thermal evolution of cometary nuclei heated by solar radiation through numerical analyses based on astrophysics.
Asteroids and comets are types of small bodies in the Solar System. Traditionally, asteroids and comets were clearly distinguished from one another. That is to say, asteroids consist mainly of rock, whilst comets consist mainly of ice. However, in recent years, small bodies possessing characteristics of both asteroids and comets have been discovered. This suggests that asteroids and comets are not entirely distinct types, but rather that comets may have lost their ice during the course of their evolution, taking on an asteroid-like appearance. Such celestial bodies are known as Comet-Asteroid Transition Objects (CAT objects). How do comets become asteroids, and how long does this process take? To address this question, we are investigating the long-term thermal evolution of cometary nuclei heated by solar radiation through numerical analyses based on astrophysics.
(3) Mineral morphology and compositional zonings:
Some of the minerals found in rocks and meteorites formed whilst the magma was cooling. Their morphology and the heterogeneous structure of chemical composition (compositional zonings) reflect the environment in which they were formed. When a mineral with a particular morphology and zonal structure is found, what kind of environment did it form in? To address this question, we are conducting numerical analyses based on a mathematical model (the phase-field method) that takes into account element distribution at solid-liquid interfaces and transient element diffusion.
Some of the minerals found in rocks and meteorites formed whilst the magma was cooling. Their morphology and the heterogeneous structure of chemical composition (compositional zonings) reflect the environment in which they were formed. When a mineral with a particular morphology and zonal structure is found, what kind of environment did it form in? To address this question, we are conducting numerical analyses based on a mathematical model (the phase-field method) that takes into account element distribution at solid-liquid interfaces and transient element diffusion.
(4) Step dynamics on crystal surfaces:
Although crystal surfaces appear flat at first glance, they contain steps approximately 1 nm high. Crystals grow as atoms and molecules from the solution are transported to the crystal surface and incorporated into the steps. However, if impurities are present in the solution, the incorporation of atoms and molecules into the steps is inhibited, affecting crystal growth. We are investigating the mechanisms of crystal growth by modelling the movement of steps during crystal growth (step dynamics) using mathematical models.
Although crystal surfaces appear flat at first glance, they contain steps approximately 1 nm high. Crystals grow as atoms and molecules from the solution are transported to the crystal surface and incorporated into the steps. However, if impurities are present in the solution, the incorporation of atoms and molecules into the steps is inhibited, affecting crystal growth. We are investigating the mechanisms of crystal growth by modelling the movement of steps during crystal growth (step dynamics) using mathematical models.
Selected Publications
Original Articles
| Publications | Keywords |
|---|---|
| Numerical Simulation of the Formation Process of Overhanging Structures in SiC Solution Growth to Suppress Solvent Inclusion, Cryst. Growth Des. 25 (2025) 5256 | Crystal growth (semiconductor), Phase-field method |
| Thermal evolution model from cometary nuclei to asteroids considering contraction associated with ice sublimation, Publications of the Astronomical Society of Japan 77 (2025) 785 | Solar system small bodies |
| Decoding the formation of barred olivine chondrules: Realization of numerical replication, Science Advances 11 (2025) eadw1187 | Chondrule, Phase-field method |
| Oscillatory zoning of minerals as a fingerprint of impurity-mediated growth, Scientific Reports 14 (2024) 13337 | Crystal growth (mineral) |
| Quantitative phase-field model for the isothermal solidification of a stoichiometric compound in a ternary liquid, Materialia 31 (2023) 101860 | Phase-field method |
| Spontaneous oscillatory growth of ice crystals in supercooled water under a microgravity environment: theoretical hypothesis on the effect of antifreeze glycoprotein, Journal of Crystal Growth 603 (2023) 127044 | Crystal growth |
| Formation and evolution of carbonaceous asteroid Ryugu: Direct evidence from returned samples, Science 379 (2022) abn8671 | Solar system small bodies |
| The asteroid 162173 Ryugu: a cometary origin, The Astrophysical Journal Letters 925 (2022) L15 | Solar system small bodies |
| Crystal growth hysteresis in spiral growth, Crystal Growth & Design 20 (2020) 245 | Crystal growth, Phase-field method |
| Comprehensive study of thermal desorption of grain-surface species by accretion shocks around protostars,?The Astrophysical Journal 839 (2017) 47 | Astrophysics |
| Numerical study of impurity-induced growth hysteresis on a growing crystal surface,?Crystal Growth & Design 16 (2016) 2033 | Crystal growth, Phase-field method |
| Phase-field modeling of step dynamics on growing crystal surface: Step pinning induced by impurities,?Crystal Growth & Design 15 (2015) 4142 | Numerical simulation, Phase-field method |
| Phase-field modeling of step dynamics on growing crystal surface: direct integration of growth units to step front,?Crystal Growth & Design 15 (2015) 2165 | Numerical simulation, Phase-field method |
| Role of impurity on growth hysteresis and oscillatory growth of crystals,?Crystal Growth & Design 13 (2013) 3588 | Crystal growth |
| Phase-field simulation for crystallization of a highly supercooled melt droplet in levitation environment, Journal of Applied Physics 108 (2010) 114912 | Chondrule, Phase-field method |
| Formation of cosmic crystals in highly-supersaturated silicate vapor produced by planetesimal bow shocks,?Astrophysical Journal 719 (2010) 642 | Astrophysics |
| Origin of three-dimensional shapes of chondrules. I: Hydrodynamics simulations of rotating droplet exposed to high-velocity rarefied gas flow,?Icarus 197 (2008) 269 | Chondrule |
| Fragment-Collision Model for Compound Chondrule Formation: Estimation of Collision Probability,?Icarus 194 (2008) 811 | Chondrule |
| Shock-Wave Heating Model for Chondrule Formation: Hydrodynamic Simulation of Molten Droplets exposed to Gas Flows,?Icarus 188 (2007) 246 | Chondrule |
| Shock-Wave Heating Model for Chondrule Formation: Prevention of Isotopic Fractionation,?Astrophysical Journal 651 (2006) 1272 | Chondrule |
