...
首页> 外文期刊>The Journal of Chemical Physics >Structure and dynamics of water confined in silica nanopores
【24h】

Structure and dynamics of water confined in silica nanopores

机译:限制在二氧化硅纳米孔中的水的结构和动力学

获取原文
获取原文并翻译 | 示例
           

摘要

We report the results of molecular simulation of water in silica nanopores at full hydration and room temperature. The model systems are approximately cylindrical pores in amorphous silica, with diameters ranging from 20 to 40. The filled pores are prepared using grand canonical Monte Carlo simulation and molecular dynamics simulation is used to calculate the water structure and dynamics. We found that water forms two distinct molecular layers at the interface and exhibits uniform, but somewhat lower than bulk liquid, density in the core region. The hydrogen bond density profile follows similar trends, with lower than bulk density in the core and enhancements at the interface, due to hydrogen bonds between water and surface non-bridging oxygens and OH groups. Our studies of water dynamics included translational mean squared displacements, orientational time correlations, survival probabilities in interfacial shells, and hydrogen bond population relaxation. We found that the radial-axial anisotropy in translational motion largely follows the predictions of a model of free diffusion in a cylinder. However, both translational and rotational water mobilities are strongly dependent on the proximity to the interface, with pronounced slowdown in layers near the interface. Within these layers, the effects of interface curvature are relatively modest, with only a small increase in mobility in going from the 20 to 40 diameter pore. Hydrogen bond population relaxation is nearly bulk-like in the core, but considerably slower in the interfacial region.
机译:我们报告了在完全水合和室温下二氧化硅纳米孔中水的分子模拟结果。模型系统是无定形二氧化硅中的近似圆柱孔,直径范围为20到40。使用大正则蒙特卡罗模拟制备填充的孔,并使用分子动力学模拟计算水的结构和动力学。我们发现水在界面处形成两个不同的分子层,并在核心区域显示出均匀但略低于本体液体的密度。氢键密度分布遵循相似的趋势,由于水与表面非桥连氧和OH基团之间的氢键,核中的密度低于堆密度,界面处的密度增加。我们对水动力学的研究包括平移均方位移,方向时间相关性,界面壳中的生存概率以及氢键种群弛豫。我们发现平移运动中的径向-轴向各向异性很大程度上遵循圆柱体中自由扩散模型的预测。但是,平移和旋转水的流动性都强烈地取决于与界面的接近度,界面附近各层的明显减慢。在这些层中,界面曲率的影响相对较小,从20到40直径的孔进入时,迁移率只有很小的增加。氢键种群的弛豫在岩心中几乎是块状的,但是在界面区域中则要慢得多。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号