The thickness of a liquid layer on the free surface of ice as obtained from computer simulation

被引:149
作者
Conde, M. M. [1 ]
Vega, C. [1 ]
Patrykiejew, A. [2 ]
机构
[1] Univ Complutense, Fac Ciencias Quim, Dept Quim Fis, E-28040 Madrid, Spain
[2] Marie Curie Sklodowska Univ, Fac Chem, PL-20031 Lublin, Poland
关键词
D O I
10.1063/1.2940195
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
Molecular dynamic simulations were performed for ice I-h with a free surface by using four water models, SPC/E, TIP4P, TIP4P/Ice, and TIP4P/2005. The behavior of the basal plane, the primary prismatic plane, and of the secondary prismatic plane when exposed to vacuum was analyzed. We observe the formation of a thin liquid layer at the ice surface at temperatures below the melting point for all models and the three planes considered. For a given plane it was found that the thickness of a liquid layer was similar for different water models, when the comparison is made at the same undercooling with respect to the melting point of the model. The liquid layer thickness is found to increase with temperature. For a fixed temperature it was found that the thickness of the liquid layer decreases in the following order: the basal plane, the primary prismatic plane, and the secondary prismatic plane. For the TIP4P/Ice model, a model reproducing the experimental value of the melting temperature of ice, the first clear indication of the formation of a liquid layer, appears at about -100 degrees C for the basal plane, at about -80 degrees C for the primary prismatic plane, and at about -70 degrees C for the secondary prismatic plane. (C) 2008 American Institute of Physics.
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页数:11
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