化学学报 ›› 2010, Vol. 68 ›› Issue (16): 1653-1660. 上一篇    下一篇

研究论文

水化锂蒙脱石层间结构和动力特征的分子模拟

王进*,1,2,王军霞1,曾凡桂3,吴秀玲2   

  1. (1西南科技大学四川省非金属复合与功能材料重点实验室 省部共建国家重点实验室培育基地 绵阳 621010)
    (2中国地质大学教育部纳米矿物材料及应用工程研究中心 材料科学与化学工程学院 武汉 430074)
    (3太原理工大学煤科学与技术教育部及山西省重点实验室 太原 030024)
  • 投稿日期:2009-08-30 修回日期:2010-02-21 发布日期:2010-04-06
  • 通讯作者: 王进 E-mail:wangjin@swust.edu.cn

Molecular Simulation of Interlayer Structure and Dynamics Properties in Lithium Montmorillonite Hydrates

Wang Jin*,1,2 Wang Junxia1 Zeng Fangui3 Wu Xiuling2   

  1. (1 State Key Laboratory Cultivation Base for Nonmetal Composite and Functional Materials, South West University of Science and Technology, Mianyang 621010)
    (2 Engineering Research Center of Nano-Geomaterials of Ministry of Education, Faculty of Materials Science and Chemical Engineering, China University of Geoscience, Wuhan 430074)
    (3 Key Laboratory of Coal Science & Technology for Ministry of Education & Shanxi Province, Taiyuan University of Technology, Taiyuan 030024)
  • Received:2009-08-30 Revised:2010-02-21 Published:2010-04-06
  • Contact: wang jin E-mail:wangjin@swust.edu.cn

利用分子力场和分子动力学(MD)的方法研究了Li-蒙脱石的结构构型, 层间阳离子的水化行为、水分子的结构特征以及它们的扩散性质. 分子力场构型优化结果表明: Li-蒙脱石的层间距、体积和密度与层间水含量有关; MD模拟的动画轨迹显示Li-蒙脱石层间Li的位置与层间电荷位置有关. 均方根位移和自扩散系数的计算结果表明: 层间阳离子、水分子在Li-蒙脱石一、二层水合物中的扩散受到上下粘土片表面的限制, 在三层水合物中开始离开粘土层面向其它方向快速扩散. 径向分布函数及其结构因子的分析结果表明Li在一、二、三层水合物中有不同的水合层; 层间水分子的结构特征说明其在蒙脱石层间有水合水分子和自由水分子之分, 且它们的比值在一、二和三层水合物中有所不同.

关键词: 锂蒙脱石, 分子力场, 分子动力学, 自扩散系数, 径向分布函数

The structure configuration, hydrated behavior of counterions, structure properties and diffusion features of water molecules in the interlayer of lithium montmorillonite were investigated by molecular force field and molecular dynamics simulation (MD). The configuration optimization results of molecular force field showed that the layer spacing, density and volume were related to the water content in the interlayer of lithium montmorillonite. The animated trajectory of molecular dynamics simulation demonstrated that the positions of Li ions in the interlayer of lithium montmorillonite were related with interlayer charge sites in clay sheets. The results of mean square displacement (MSD) and self-diffusion coefficients illustrated that the diffusion of counterions and water molecules were restricted to the surface of clay sheets when in one- and two-layer hydrates of lithium montmorillonite. In the three-layer hydrates, the Li ions and water molecules became detached from the surface and began quickly diffused towards the other direction. The analysis results of radial distribution function (RDF) and its structure factor showed that the hydrated shell of Li ions in one-, two-, and three-layer hydrates were different. The structure properties of water molecules in the interlayer of lithium montmorillonite indicated that water molecules were differentiated with molecules and free water molecules, and the ratio of them differed in one-, two- and three-layer hydrates.

Key words: lithium-montmorillonite, molecular force field, molecular dynamics, self-diffusion coefficient, radial distribution function