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Computer simulation of the 13 crystalline phases of ice

机译:冰的13个晶相的计算机模拟

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As a reference for follow-up studies toward more accurate model parametrizations, we performed molecular-dynamics and Monte Carlo simulations for all known crystalline phases of ice, as described by the simple point-charge/extended and TIP4P water models. We started from the measured structures, densities, and temperatures, and carried out classical canonical simulations for all these arrangements. All simulated samples were cooled down close to 0 K to facilitate the comparison with theoretical estimates. We determined configurational internal energies as well as pressures, and monitored how accurately the measured configurations were preserved during the simulations. While these two models predicted very similar thermophysical and structural properties for water at ambient conditions, the predicted features for the corresponding ice polymorphs may differ significantly. (C) 2005 American Institute of Physics.
机译:作为对更精确的模型参数化进行后续研究的参考,我们对冰的所有已知晶相进行了分子动力学和蒙特卡洛模拟,如简单的点电荷/扩展和TIP4P水模型所述。我们从测量的结构,密度和温度开始,并对所有这些布置进行了经典的规范模拟。将所有模拟样品冷却至接近0 K,以利于与理论估计值进行比较。我们确定了配置的内部能量以及压力,并监视了在仿真过程中如何精确地保留了所测量的配置。虽然这两个模型预测了在环境条件下水的热物理性质和结构性质非常相似,但相应冰晶型的预测特征可能存在显着差异。 (C)2005美国物理研究所。

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