Zobrazeno 1 - 10
of 1 010
pro vyhledávání: '"Miyanishi K"'
Autor:
Katagiri, K., Ozaki, N., Dresselhaus-Marais, L. E., Eggert, J. H., Inubushi, Y., Irifune, T., Koenig, M., Matsuoka, T., Miyanishi, K., Nakamura, H., Nishiyama, N., Okuchi, T., Sekine, T., Seto, Y., Sueda, K., Tange, Y., Togashi, T., Umeda, Y., Yabashi, M., Yabuuchi, T., Kodama, R.
Extremely high pressures over a million of atmospheres are required to deform diamonds permanently. Under dynamic high-pressure conditions, even such strong materials lose their strengths so rapidly that the initially pristine lattice transforms into
Externí odkaz:
http://arxiv.org/abs/2208.03416
Autor:
Makarov, S. S., Dyachkov, S. A., Pikuz, T. A., Katagiri, K., Zhakhovsky, V. V., Inogamov, N. A., Khokhlov, V. A., Martynenko, A. S., Albertazzi, B., Rigon, G., Mabey, P., Hartley, N., Inubushi, Y., Miyanishi, K., Sueda, K., Togashi, T., Yabashi, M., Yabuuchi, T., Kodama, R., Pikuz, S. A., Koenig, M., Ozaki, N.
The propagation of a shock wave in solids can stress them to ultra-high pressures of millions of atmospheres. Understanding the behavior of matter at these extreme pressures is essential to describe a wide range of physical phenomena, including the f
Externí odkaz:
http://arxiv.org/abs/2207.01719
Autor:
Guarguaglini, M., Hernandez, J. -A., Okuchi, T., Barroso, P., Benuzzi-Mounaix, A., Bolis, R., Brambrink, E., Fujimoto, Y., Kodama, R., Koenig, M., Lefevre, F., Miyanishi, K., Ozaki, N., Sano, T., Umeda, Y., Vinci, T., Ravasio, A.
Water, ethanol, and ammonia are the key components of the mantles of Uranus and Neptune. To improve structure and evolution models and give an explanation of the magnetic fields and luminosities of the icy giants, those components need to be characte
Externí odkaz:
http://arxiv.org/abs/1804.06595
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Bolis, R. M., Morard, G., Vinci, T., Ravasio, A., Bambrink, E., Guarguaglini, M., Koenig, M., Musella, R., Remus, F., Bouchet, J., Ozaki, N., Miyanishi, K., Sekine, T., Sakawa, Y., Sano, T., Kodama, R., Guyot, F., Benuzzi-Mounaix, A.
We report an experimental study of the phase diagrams of periclase (MgO), enstatite (MgSiO3) and forsterite (Mg2SiO4) at high pressures. We investigated with laser driven decaying shocks the pressure/temperature curves of MgO, MgSiO3 and Mg2SiO4 betw
Externí odkaz:
http://arxiv.org/abs/1604.01554
Autor:
Harmand, M., Ravasio, A., Mazevet, S., Bouchet, J., Denoeud, A., Dorchies, F., Feng, Y., Fourment, C., Galtier, E ., Gaudin, J., Guyot, F., Kodama, R., Koenig, M., Lee, H. J., Miyanishi, K., Morard, G., Musella, R., Nagler, B., Nakatsutsumi, M., Ozaki, N., Recoules, V., Toleikis, S., Vinci, T., Zastrau, U., Zhu, D., Benuzzi-Mounaix, A.
Several important geophysical features such as heat flux at the Core-Mantle Boundary or geodynamo production are intimately related with the temperature profile in the Earth's core. However, measuring the melting curve of iron at conditions correspon
Externí odkaz:
http://arxiv.org/abs/1411.2074
Autor:
Maeda, Y., Hironaka, Y., Iwasaki, T., Kawasaki, K., Sakawa, Y., Izumi, T., Ota, M., Egashira, S., Nakagawa, Y., Higashi, N., Sentoku, Y., Kodama, R., Ozaki, N., Matsuoka, T., Somekawa, T., Yabuuchi, T., Inubushi, Y., Togashi, T., Kon, A., Sueda, K., Miyanishi, K., Shingubara, S., Shimizu, T., Okumura, A., Shigemori, K.
Publikováno v:
In High Energy Density Physics August 2020 36
Autor:
Morioka, S., Ozaki, N., Hosomi, M., Katagiri, K., Matsuoka, T., Miyanishi, K., Okuchi, T., Sano, T., Umeda, Y., Kodama, R.
Publikováno v:
In High Energy Density Physics November 2019 33
Autor:
Sano, T., Ozaki, N., Sakaiya, T., Shigemori, K., Ikoma, M., Kimura, T., Miyanishi, K., Endo, T., Shiroshita, A., Takahashi, H., Jitsui, T., Hori, Y., Hironaka, Y., Iwamoto, A., Kadono, T., Nakai, M., Okuchi, T., Otani, K., Shimizu, K., Kondo, T., Kodama, R., Mima, K.
The principal Hugoniot for liquid hydrogen was obtained up to 55 GPa under laser-driven shock loading. Pressure and density of compressed hydrogen were determined by impedance-matching to a quartz standard. The shock temperature was independently mea
Externí odkaz:
http://arxiv.org/abs/1101.1143
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.