JpGU-AGU Joint Meeting 2017

講演情報

[EE] ポスター発表

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT22] [EE] 核-マントルの相互作用と共進化

2017年5月21日(日) 13:45 〜 15:15 ポスター会場 (国際展示場 7ホール)

コンビーナ:土屋 卓久(愛媛大学地球深部ダイナミクス研究センター)、寺崎 英紀(大阪大学大学院理学研究科)、Satish-Kumar Madhusoodhan(Department of Geology, Faculty of Science, Niigata University)、入舩 徹男(愛媛大学地球深部ダイナミクス研究センター)、Hernlund John(Earth-Life Science Institute, Tokyo Institute of Technology)、大谷 栄治(東北大学大学院理学研究科地学専攻)

[SIT22-P17] Viscosity and atomic-local-structures of basaltic melt under high pressure

*大村 訓史1土屋 卓久2 (1.広島工業大学、2.愛媛大学)

キーワード:Ab initio molecular dynamics simulation, Basaltic melt, Viscosity , Microscopic structures

High pressure properties of basaltic melt are of importance in deep Earth science related to such as early magma ocean and subsequent differentiation processes (Agee 1998; Ohtani and Maeda 2001; Suzuki, et al. 2005)
Recently, experimental studies reported that the viscosity of basaltic melt decreases with increasing pressure (Allwardt, et al. 2007; Sakamaki, et al. 2013). They suggested based on the results of classical molecular dynamics simulation (Nevins and Spera 1998) and 27Al magic-angle spinning nuclear magnetic resonance (Allwardt, et al. 2007) that this anomalous behavior is related to the coordination change of Al. However, other silicate melts which contain none of Al also show a common behavior of viscosity (McMillan et al., 2009 ). It means that the microscopic origin of the anomalous pressure response of viscosity of the basaltic melt is still unclear. For this reason, in this study, we perform ab initio molecular dynamics simulations and analyze atomic–local-structures in basaltic aluminosilicate melt under pressure. At the last meeting, we reported the structural changes around Al atom. This time, we discuss relationship between the viscosity and structural changes not only around Al but other elements.



Reference
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P. E. McMillan and M. C. Wilding. J. Non-Cryst. Solids. 355 722 (2009)
T. Sakamaki, et al. Nature Geoscience 6, 1041 (2013)