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Intercalation of dodecylamine into kaolinite and its layering structure investigated by molecular dynamics simulation

机译:分子动力学模拟研究十二烷基胺嵌入高岭石中及其分层结构

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摘要

Dodecylamine was successfully intercalated into the layer space of kaolinite by utilizing the methanol treated kaolinite–dimethyl sulfoxide (DMSO) intercalation complex as an intermediate. The basal spacing of kaolinite, measured by X-ray diffraction (XRD), increased from 0.72 nm to 4.29 nm after the intercalation of dodecylamine. Also, the significant variation observed in the Fourier Transform Infrared Spectroscopy (FTIR) spectra of kaolinite when intercalated with dodecylamine verified the feasibility ofudintercalation of dodecylamine into kaolinite. Isothermal-isobaric (NPT) molecular dynamics simulation with the use of Dreiding force field was performed to probe into the layering behavior and structure of nanoconfined dodecylamine in the kaolinite gallery. The concentration profiles of the nitrogen atom, methyl group and methylene group of intercalated dodecylamine molecules in the direction perpendicular to the kaolinite basal surface indicated that the alkyl chains within the interlayer space of kaolinite exhibited an obvious layering structure. However, the unified bilayer, pseudo-trilayer, or paraffin-type arrangements of alkyl chains deduced based on their chain length combined with the measured basal spacing of organoclays were not found in this study. The alkyl chains aggregated to a mixture of ordered paraffin-type-like structure and disordered gauche conformation in the middle interlayer space of kaolinite, and some alkyl chains arranged in two bilayer structures, in which one was close to the silica tetrahedron surface, and the other was close to the alumina octahedron surface with their alkyl chains parallel to the kaolinite basal surface.
机译:通过使用甲醇处理的高岭石-二甲亚砜(DMSO)嵌入复合物作为中间体,十二烷基胺已成功嵌入高岭石的层空间中。在插入十二烷基胺后,通过X射线衍射(XRD)测量的高岭土的基础间距从0.72 nm增加到4.29 nm。同样,当高岭石与十二烷基胺嵌入时,在傅立叶变换红外光谱(FTIR)光谱中观察到的显着变化证明了将十二烷基胺嵌入高岭石的可行性。利用Dreiding力场进行了等温-等压(NPT)分子动力学模拟,以探索高岭土画廊中纳米级十二烷基胺的分层行为和结构。在垂直于高岭石基面的方向上插入的十二烷基胺分子的氮原子,甲基和亚甲基的浓度分布表明,高岭石层间空间内的烷基链表现出明显的分层结构。然而,在这项研究中没有发现基于烷基链长和有机粘土基距的推论得出的统一的双层,伪三层或石蜡型烷基链排列。烷基链在高岭石的中间层空间中聚集为有序石蜡型结构和无规状构象的混合物,一些烷基链排列成两个双层结构,其中一个靠近二氧化硅四面体表面,另一个靠近氧化铝八面体表面,其烷基链平行于高岭石基面。

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