Department of Physics, Saint Francis Xavier University, Antigonish, Nova Scotia B2G 2WS, Canada.
J Chem Phys. 2011 Jan 7;134(1):014710. doi: 10.1063/1.3518984.
Attempts to simulate crystal growth of ice from liquid water and to provide a consistent microscopic description of this process have been challenging tasks. In this paper we have adapted our previously developed molecular dynamics simulation methodology to enable the investigation of steady-state directional crystal growth∕melting of ice. Specifically, we examine ice∕water systems of the (001), (110), and (111) faces of ice Ic and the (0001), (1010), and (1120) faces of ice Ih, where the TIP4P, TIP4P-Ew, and SPC∕E water models have been utilized. The influence of different growth∕melting conditions (temperature gradients and growth velocities) is investigated. Profile functions of properties of interest across the interface are obtained from nonequilibrium steady-state simulations and provide consistent descriptions of ice∕water interfaces. The widths of the various crystallographic faces are found to increase in the apparent order Ic111, Ih0001 < Ih1010 < Ih1120 < Ic001 < Ic110. The observed growth rates were in agreement with experimental values and the possible dependence on the various faces is explored. The melting temperatures obtained with the present methodology for the different models are in good agreement with estimates from other work.
尝试模拟冰从液态水中的结晶生长,并为这个过程提供一致的微观描述,一直是具有挑战性的任务。在本文中,我们已经调整了我们之前开发的分子动力学模拟方法,以能够研究冰的稳态定向结晶/熔化。具体来说,我们研究了冰 Ic 的 (001)、(110) 和 (111) 面以及冰 Ih 的 (0001)、(1010) 和 (1120) 面的冰/水系统,其中使用了 TIP4P、TIP4P-Ew 和 SPC/E 水模型。研究了不同生长/熔化条件(温度梯度和生长速度)的影响。从非平衡稳态模拟中获得了感兴趣的界面特性的轮廓函数,并为冰/水界面提供了一致的描述。发现不同结晶面的宽度按以下顺序增加:Ic111、Ih0001 < Ih1010 < Ih1120 < Ic001 < Ic110。观察到的生长速率与实验值一致,并探讨了可能对各种面的依赖性。本文方法获得的不同模型的熔化温度与其他工作的估计值吻合较好。