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首页> 外文期刊>Langmuir: The ACS Journal of Surfaces and Colloids >Na-Montmorillonite Hydrates under Basin Conditions:Hybrid Monte Carlo and Molecular Dynamics Simulations
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Na-Montmorillonite Hydrates under Basin Conditions:Hybrid Monte Carlo and Molecular Dynamics Simulations

机译:盆地条件下的钠-蒙脱土水合物:混合蒙特卡洛法和分子动力学模拟

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摘要

In this work the Na-montmorillonite hydrates are studied for different burial depths by means of hybrid Monte Carlo(HMC)and molecular dynamics(MD)simulations.The HMC simulations,performed using a NP_(zz)T ensemble,allow us to study the interlaminar space distance,structural properties,and thermodynamical properties,such as the water chemical potential.The latter quantifies the system affinity for water,and hence,it is useful for determining the most probable hydration states for a given basin condition.For increasing burial depth,we found many agreements with experimental results such as a tendency to dehydration,an increasing disorder of the interlaminar space,and a constant coordination number for the first water shell around Na~+.The MD simulations,on the other hand,were performed employing a microcanonical ensemble,from which the diffusion coefficients for water and Na~+ were also investigated for high-temperature and high-pressure conditions.
机译:在这项工作中,通过混合蒙特卡罗(HMC)和分子动力学(MD)模拟研究了不同埋深的钠-蒙脱石水合物。使用NP_(zz)T集成进行的HMC模拟,使我们能够研究层间距离,结构性质和热力学性质,例如水的化学势。后者量化了系统对水的亲和力,因此,对于确定给定盆地条件下最可能的水合作用很有用。 ,我们发现了许多具有实验结果的协议,例如脱水的趋势,层间空间的无序性以及Na〜+周围第一个水壳的配位数恒定。微规范集合,从中可以研究高温和高压条件下水和Na〜+的扩散系数。

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