Local behavior of water molecules on brucite, talc, and halite surfaces: A molecular dynamics study

被引:17
|
作者
Sakuma, H
Tsuchiya, T
Kawamura, K
Otsuki, K
机构
[1] Tohoku Univ, Grad Sch Sci, Inst Geol & Paleontol, Aoba Ku, Sendai, Miyagi 9808578, Japan
[2] Univ Minnesota, Dept Chem Engn & Mat Sci, Minneapolis, MN 55455 USA
[3] Tokyo Inst Technol, Dept Earth & Planetary Sci, Meguro Ku, Tokyo 1528551, Japan
关键词
surface diffusion; water; solid-liquid interfaces; anisotropy;
D O I
10.1080/08927020412331299350
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The structural and dynamic properties of water between brucite (0001), talc (001), and halite (100) surfaces have been calculated by classical molecular dynamics (MD) simulations at ambient conditions. The interaction potential models between water and the minerals have been developed by the energy curves obtained from the ab initio electronic state calculations. Orientational anisotropy of water molecules is almost limited in the vicinity of all the surfaces. The significant different properties of water between the surfaces are observed in the density profiles and self-diffusion coefficients. The density profile of water between talc surfaces is flat and the density is equivalent to the bulk one, while those of water between brucite and halite surfaces strongly oscillate with the distance from the surfaces. The self-diffusion coefficients parallel to the surfaces are enhanced in the vicinity of brucite and talc surfaces, and reduced on halite surface compared with that in bulk.
引用
收藏
页码:861 / 871
页数:11
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