論文- 坂巻 竜也 -
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件数:41件
[2012]
21.Stability of Fe-Ni hydride after the reaction between Fe-Ni alloy and hydrous phase (δ-AlOOH) up to 1.2 Mbar: Possibility of H contribution to the core density deficit.[Physics of the Earth and Planetary Interior,,(2012)]H. Terasaki, E. Ohtani, T. Sakai, S. Kamada, H. Asanuma, Y. Shibazaki, N. Hirao, N. Sata, Y. Ohishi, T. Sakamaki, A. Suzuki, K. Funakoshi
22.Interfacial tension of Fe-Si liquid at high pressure: Implications for liquid Fe-alloy droplet size in magma ocean.[Physics of the Earth and Planetary Interiors,(2012)]H. Tesakai, S. Urakawa, D. C. Rubie, K. Funakoshi, T. Sakamaki, Y. Shibazaki, S. Ozawa, E. Ohtani
23.Density and sound velocity of iron-sulfur alloy in liquids at high pressures and implications to planetary cores.[Lunar and Planetary Institute,(2012)]Z. Jing, Y. Wang, T. Yu, T. Sakamaki, Y. Kono, C. Park
[2011]
24.Density of carbonated peridotite magma at high pressure using an X-ray absorption method.[American Mineralogist,(2011)]T. Sakamaki, E. Ohtani, S. Urakawa, H. Terasaki, Y. Katayama
25.Pressure and temperature dependence of the viscosity of a NaAlSi2O6 melt.[Physics and Chemistry of Minerals,(2011)]A. Suzuki, E. Ohtani, H. Terasaki, K. Nishida, H. Hayashi, T. Sakamaki, Y. Shibazaki, T. Kikegawa
26.Hydrogenation of FeSi under high pressure.[American Mineralogist,(2011)]H. Terasaki, Y. Shibazaki, T. Sakamaki, R. Tateyama, E. Ohtani, K. Funakoshi, Y. Higo
27.Effect of hydrogen on the melting temperature of FeS at high pressure: Implications for the core of Ganymede.[Earth and Planetary Science Letters,(2011)]Y. Shibazaki, E. Ohtani, H. Terasaki, R. Tateyama, T. Sakamaki, T. Tsuchiya, K. Funakoshi
28.Density measurement of liquid FeS at high pressures using synchrotron X-ray absorption.[American Mineralogist,(2011)]K. Nishida, E. Ohtani, S. Urakawa, A. Suzuki, T. Sakamaki, H. Terasaki, Y. Katayama
[2010]
29.Density of high-Ti basalt magma at high pressure and origin of heterogeneities in the lunar mantle.[Earth and Planetary Science Letters,(2010)]T. Sakamaki, E. Ohtani, S. Urakawa, A. Suzuki, Y. Katayama, D. Zhao
30.Density of dry peridotite magma at high pressure by X-ray absorption method.[American Mineralogist,(2010)]T. Sakamaki, E. Ohtani, S. Urakawa, A. Suzuki, Y. Katayama
31.Density measurement of Fe3C liquid using X-ray absorption image up to 10 GPa and effect of light elements on compressibility of liquid iron.[Journal of Geophysical Research,(2010)]H. Terasaki, K. Nishida, Y. Shibazaki, T. Sakamaki, A. Suzuki, E. Ohtani, T. Kikegawa
[2009]
32.Measurement of hydrous peridotite magma density at high pressure by X-ray absorption method.[Earth and Planetary Science Letters,(2009)]T. Sakamaki, E. Ohtani, S. Urakawa, A. Suzuki, Y. Katayama
33.In situ measurement of interfacial tension of Fe-S and Fe-P liquids under high pressure using X-ray radiography and tomography techniques.[Physics of the Earth and Planetary Interior,(2009)]H. Terasaki, S. Urakawa, K. Funakoshi, N. Nishiyama, Y. Wang, K. Nishida, T. Sakamaki, A. Suzuki, E. Ohtani
34.Hydrogen incorporation to the Earth’s core.[Geochimicaet Cosmochimica Acta,(2009)]H. Terasaki, E. Ohtani, T. Sakai, S. Kamada, Y. Shibazaki, H. Asanuma, N. Hirao, Y. Ohishi, N. Sata, T. Sakamaki, A. Suzuki, K. Funakoshi
[2007]
35.Stability of carbonated magmas at the base of the Earth’s upper mantle.[Geophysical Research Letters,(2007)]S. Ghosh, E. Ohtani, K. Litasov, A. Suzuki, T. Sakamaki
36.In situ observation and determination of liquid immiscibility in the Fe-O-S melt at 3 GPa using a synchrotron X-ray radiographic technique.[Geophysical Research Letters,(2007)]K. Tsuno, H. Terasaki, E. Ohtani, A. Suzuki, Y. Asahara, K. Nishida, T. Sakamaki, K. Funakoshi, T. Kikegawa
37.高温高圧下でのイメージング実験.[KEK proceedings 放射光高圧研究における実験技術の新展開,(2007),61-64]鈴木昭夫、西田圭佑、坂巻竜也、寺崎英紀、大谷栄治
38.ダイヤモンドアンビルを用いた珪酸塩メルトのX線吸収密度測定.[KEK proceedings 放射光高圧研究における実験技術の新展開,(2007),1-4]浦川 啓、坂巻竜也
[2006]
39.Stability of hydrous melt at the base of the Earth’s upper mantle.[Nature,(2006)]T. Sakamaki, A. Suzuki, E. Ohtani
40.Effect of pressure on the viscosity of Fe-S and Fe-C liquids up to 16 GPa.[Geophysical Research Letters,(2006)]H. Terasaki, A. Suzuki, E. Ohtani, K. Nishida, T. Sakamaki, K. Funakoshi
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