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Molecular dynamics modelling of hydrated mineral interlayers and surfaces: structure and dynamics

机译:水合矿物中间层和表面的分子动力学建模:结构和动力学

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摘要

This paper reviews the results of recent molecular dynamics (MD) modelling studies of the interaction of water and solute species with mineral surfaces and their behaviour in mineral interlayers. Emphasis is on results for single and double hydroxide phases. Computational results are presented for water and anions in the interlayers of the Ca2Al, Mg2Al, and LiAl2 layered double hydroxides and on the surfaces of the Ca2Al phase. Detailed results for water on the (001) surface of brucite (Mg(OH)2) are presented and compared to published results for other phases. In all these cases, hydrogen bonding and the development of a hydrogen-bond network involving the H2O molecules and the solid substrate play very significant roles. The MD methods are especially effective for investigating the structure and dynamics of mineral-fluid interfaces and mineral interlayers, because they can be applied to systems containing hundreds to thousands of atoms and for extended durations of the order of nanoseconds.
机译:本文综述了水和溶质 种类与矿物表面相互作用及其在矿物 中间层。重点是单和双氢氧化物 相的结果。给出了Ca 2 Al,Mg 2 Al和LiAl 2 层间水和阴离子 的计算结果。 sub>层状双 氢氧化物,并在Ca 2 Al相的表面上。给出了水镁矿(Mg(OH) 2 的(001)表面水的详细 结果,并将其与其他阶段的公开结果进行了比较。 在所有这些情况下,氢键和 涉及H 2 O分子和 < / sup>固体基材起着非常重要的作用。 MD方法 对于研究矿物流体界面和矿物中间层的结构和动力学特别有效,因为它们可以应用于包含以下内容的系统: 数百至 原子,并且扩展的持续时间为 纳秒。

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