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Featured researches published by Yuta Shimoyama.


Journal of Geophysical Research | 2016

Thermoelastic properties of liquid Fe-C revealed by sound velocity and density measurements at high pressure

Yuta Shimoyama; Hidenori Terasaki; Satoru Urakawa; Yusaku Takubo; Soma Kuwabara; Shunpachi Kishimoto; Tetsu Watanuki; Akihiko Machida; Yoshinori Katayama; Tadashi Kondo

Carbon is one of the possible light elements in the cores of the terrestrial planets. The P-wave velocity (VP) and density (ρ) are important factors for estimating the chemical composition and physical properties of the core. We simultaneously measured the VP and ρ of Fe-3.5 wt% C up to 3.4 GPa and 1850 K using ultrasonic pulse-echo method and X-ray absorption methods. The VP of liquid Fe-3.5 wt% C decreased linearly with increasing temperature at constant pressure. The addition of carbon decreased the VP of liquid Fe by about 2% at 3 GPa and 1700 K and decreased the Fe density by about 2% at 2 GPa and 1700 K. The bulk modulus of liquid Fe-C and its pressure (P) and temperature (T) effects were precisely determined from directly measured ρ and VP data to be K0,1700K = 83.9 GPa, dKT/dP = 5.9(2), and dKT/dT = −0.063(8) GPa/K. The addition of carbon did not affect the isothermal bulk modulus (KT) of liquid Fe but it decreased the dK/dT of liquid Fe. In the ρ–VP relationship, VP increases linearly with ρ and can be approximated as VP (m/s) = −6786(506) + 1537(71) × ρ (g/cm3), suggesting that Birchs law is valid for liquid Fe-C at the present P–T conditions. Our results imply that at the conditions of the lunar core, the elastic properties of an Fe-C core are more affected by temperature than those of Fe-S core.


American Mineralogist | 2016

Compressional and shear wave velocities for polycrystalline bcc-Fe up to 6.3 GPa and 800 K

Yuki Shibazaki; Keisuke Nishida; Yuji Higo; Mako Igarashi; Masaki Tahara; Tatsuya Sakamaki; Hidenori Terasaki; Yuta Shimoyama; Soma Kuwabara; Yusaku Takubo

Abstract The cores of the Earth and other differentiated bodies are believed to be comprised of iron and various amounts of light elements. Measuring the densities and sound velocities of iron and its alloys at high pressures and high temperatures is crucial for understanding the structure and composition of these cores. In this study, the sound velocities (vP and vS) and density measurements of body-centered cubic (bcc)-Fe were determined experimentally up to 6.3 GPa and 800 K using ultrasonic and X-ray diffraction methods. Based on the measured vP, vS, and density, we obtained the following parameters regarding the adiabatic bulk KS and shear G moduli of bcc-Fe: KS0 = 163.2(15) GPa, ∂KS/̸P = 6.75(33), ∂KS/∂T = –0.038(3) GPa/K, G0 = 81.4(6) GPa, ∂G/̸P = 1.66(14), and ∂G/∂T = –0.029(1) GPa/K. Moreover, we observed that the sound velocity–density relationship for bcc-Fe depended on temperature in the pressure and temperature ranges analyzed in this study and the effect of temperature on vS was stronger than that on vP at a constant density, e.g., 6.0% and 2.7% depression for vS and vP, respectively, from 300 to 800 K at 8000 kg/m3. Furthermore, the effects of temperature on both vP and vS at a constant density were much greater for bcc-Fe than for ε-FeSi (cubic B20 structure), according to previously obtained measurements, which may be attributable to differences in the degree of thermal pressure. These results suggest that the effects of temperature on the sound velocity–density relationship for Fe alloys strongly depend on their crystal structures and light element contents in the range of pressure and temperature studied.


Physics of the Earth and Planetary Interiors | 2013

Density of Fe-3.5wt% C liquid at high pressure and temperature and the effect of carbon on the density of the molten iron

Yuta Shimoyama; Hidenori Terasaki; Satoru Urakawa; Yusaku Takubo; Keisuke Nishida; Akio Suzuki; Yoshinori Katayama


Earth and Planetary Science Letters | 2013

Sound velocity measurements in liquid Fe–S at high pressure: Implications for Earth's and lunar cores

Keisuke Nishida; Yoshio Kono; Hidenori Terasaki; Suguru Takahashi; Miho Ishii; Yuta Shimoyama; Yuji Higo; Ken-ichi Funakoshi; Tetsuo Irifune


Physics and Chemistry of Minerals | 2016

Sound velocity and elastic properties of Fe–Ni and Fe–Ni–C liquids at high pressure

Soma Kuwabara; Hidenori Terasaki; Keisuke Nishida; Yuta Shimoyama; Yusaku Takubo; Yuji Higo; Yuki Shibazaki; Satoru Urakawa; Kentaro Uesugi; Akihisa Takeuchi; Tadashi Kondo


Isij International | 2014

Repulsive Nature for Hydrogen Incorporation to Fe3C up to 14 GPa

Hidenori Terasaki; Yuki Shibazaki; Keisuke Nishida; Ryuji Tateyama; Suguru Takahashi; Miho Ishii; Yuta Shimoyama; Ken-ichi Funakoshi; Yuji Higo


Physics of the Earth and Planetary Interiors | 2016

Towards a consensus on the pressure and composition dependence of sound velocity in the liquid Fe–S system

Keisuke Nishida; Akio Suzuki; Hidenori Terasaki; Yuki Shibazaki; Yuji Higo; Souma Kuwabara; Yuta Shimoyama; Moe Sakurai; Masashi Ushioda; Eiichi Takahashi; Takumi Kikegawa; Daisuke Wakabayashi; Nobumasa Funamori


Japan Geoscience Union | 2017

Interior structure of Mars estimated from elastic properties of liquid Fe-Ni-S

Hidenori Terasaki; Yuta Shimoyama; Mayumi Maki; Fuyuka Kurokawa; Satoru Urakawa; Keisuke Nishida; Ryunosuke Saito; Yusaku Takubo; Yuki Shibazaki; Tatsuya Sakamaki; Akihiko Machida; Yuji Higo; Tadashi Kondo


Japan Geoscience Union | 2017

Thermoelastic properties of iron-carbide melts under high pressure: implication for carbon in the lunar interior

Yuta Shimoyama; Hidenori Terasaki; Satoru Urakawa; Yusaku Takubo; Tetsu Watanuki; Akihiko Machida; Yoshinori Katayama; Tadashi Kondo


Japan Geoscience Union | 2017

Constraint on composition and size of lunar Fe-Ni-S core

Hidenori Terasaki; Keisuke Nishida; Satoru Urakawa; Yuta Shimoyama; Yuji Higo

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Akihiko Machida

Japan Atomic Energy Agency

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