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分子模拟揭示高岭土中由水介导的醋酸钾插层作用

Water-mediated potassium acetate intercalation in kaolinite as revealed by molecular simulation.

作者信息

Ható Zoltán, Makó Éva, Kristóf Tamás

机构信息

Institute of Chemistry, Department of Physical Chemistry, University of Pannonia, P.O. Box 158, 8201, Veszprém, Hungary.

出版信息

J Mol Model. 2014 Mar;20(3):2140. doi: 10.1007/s00894-014-2140-9. Epub 2014 Feb 19.

Abstract

Molecular simulations are suitable tools to study the adsorption and intercalation of molecules in clays. In this work, a recently proposed thermodynamically consistent force field for inorganic compounds (INTERFACE, Heinz H, Lin TJ, Mishra RK, Emami FS (2013) Langmuir 29:1754-1765), which enables accurate simulations of inorganic-organic interfaces, was tested for a two-sheet type clay mineral. All-atom NpT molecular dynamics simulations were used to describe the characteristics (basal spacing, loading, molecular orientation) of some intercalate complexes of kaolinite with potassium acetate and the results were compared with the available experimental data. The most probable structural configurations of the kaolinite/potassium acetate intercalate complexes were determined from the simulations. Our examinations confirmed some supposed (single- or double-layered) arrangements of guest molecules. The need of interlayer water in the intercalate complex, which can be produced by the basic synthesis procedure in air atmosphere, was verified.

摘要

分子模拟是研究分子在粘土中的吸附和插层的合适工具。在这项工作中,最近提出的一种用于无机化合物的热力学一致力场(INTERFACE,海因茨·H,林TJ,米什拉RK,埃马米FS(2013年)《朗缪尔》29:1754 - 1765),该力场能够精确模拟无机 - 有机界面,针对一种双片层型粘土矿物进行了测试。采用全原子NpT分子动力学模拟来描述高岭石与醋酸钾的一些插层复合物的特征(基面间距、负载量、分子取向),并将结果与现有的实验数据进行比较。通过模拟确定了高岭石/醋酸钾插层复合物最可能的结构构型。我们的研究证实了客体分子的一些假定(单层或双层)排列。插层复合物中层间水的需求得到了验证,这种水可通过在空气气氛中的基本合成程序产生。

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