Wang Jianwei, Kalinichev Andrey G, Kirkpatrick R James, Cygan Randall T
Department of Geology and NSF Water CAMPWS, University of Illinois at Urbana-Champaign, 1301 West Green Street, Urbana, Illinois 61801, USA.
J Phys Chem B. 2005 Aug 25;109(33):15893-905. doi: 10.1021/jp045299c.
Molecular dynamics (MD) computer simulations of liquid water adsorbed on the muscovite (001) surface provide a greatly increased, atomistically detailed understanding of surface-related effects on the spatial variation in the structural and orientational ordering, hydrogen bond (H-bond) organization, and local density of H2O molecules at this important model phyllosilicate surface. MD simulations at constant temperature and volume (statistical NVT ensemble) were performed for a series of model systems consisting of a two-layer muscovite slab (representing 8 crystallographic surface unit cells of the substrate) and 0 to 319 adsorbed H2O molecules, probing the atomistic structure and dynamics of surface aqueous films up to 3 nm in thickness. The results do not demonstrate a completely liquid-like behavior, as otherwise suggested from the interpretation of X-ray reflectivity measurements and earlier Monte Carlo simulations. Instead, a more structurally and orientationally restricted behavior of surface H2O molecules is observed, and this structural ordering extends to larger distances from the surface than previously expected. Even at the largest surface water coverage studied, over 20% of H2O molecules are associated with specific adsorption sites, and another 50% maintain strongly preferred orientations relative to the surface. This partially ordered structure is also different from the well-ordered 2-dimensional ice-like structure predicted by ab initio MD simulations for a system with a complete monolayer water coverage. However, consistent with these ab initio results, our simulations do predict that a full molecular monolayer surface water coverage represents a relatively stable surface structure in terms of the lowest diffusional mobility of H2O molecules along the surface. Calculated energies of water adsorption are in good agreement with available experimental data.
对吸附在白云母(001)表面的液态水进行的分子动力学(MD)计算机模拟,极大地增进了我们对该重要层状硅酸盐模型表面上与表面相关的效应的理解,这些效应涉及结构和取向有序性的空间变化、氢键(H键)组织以及H₂O分子的局部密度,且这种理解在原子层面上更加详细。在恒温恒容条件下(统计NVT系综),对一系列模型系统进行了MD模拟,这些系统由两层白云母平板(代表衬底的8个晶体表面单元晶胞)和0至319个吸附的H₂O分子组成,以此探究厚度达3 nm的表面水膜的原子结构和动力学。结果并未显示出完全类似液体的行为,而X射线反射率测量结果的解读及早期蒙特卡罗模拟曾暗示存在这种行为。相反,观察到表面H₂O分子的结构和取向受到更多限制,并且这种结构有序性从表面延伸到比先前预期更大的距离。即使在研究的最大表面水覆盖率下,超过20%的H₂O分子与特定吸附位点相关联,另外50%的分子相对于表面保持强烈的优先取向。这种部分有序的结构也不同于从头算MD模拟预测的具有完整单层水覆盖的系统的有序二维冰状结构。然而,与这些从头算结果一致的是,我们的模拟确实预测,就H₂O分子沿表面的最低扩散迁移率而言,完整的分子单层表面水覆盖代表一种相对稳定的表面结构。计算得到的水吸附能与现有实验数据高度吻合。