首页> 外文期刊>The journal of physical chemistry, C. Nanomaterials and interfaces >Molecular Dynamics Simulation of Basal Spacing, Energetics, and Structure Evolution of a Kaolinite-Formamide Intercalation Complex and Their Interfacial Interaction
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Molecular Dynamics Simulation of Basal Spacing, Energetics, and Structure Evolution of a Kaolinite-Formamide Intercalation Complex and Their Interfacial Interaction

机译:高岭土 - 甲酰胺嵌入复合物的基础间距,能量学和结构演化的分子动力学模拟及其界面相互作用

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Molecular dynamics simulations were performed on kaolinite formamide complex models with various numbers of formamide molecules loaded in the kaolinite interlayer to explore the basal spacing, energetics, and structure evolution of the kaolinite formamide complex during the intercalation process. Additionally, the interfacial interactions of formamide with kaolinite interlayer surfaces were calculated. The calculation revealed that the basal spacing of kaolinite was enlarged to 9.6 angstrom at the beginning of intercalation. Formamide was arranged as a monolayer structure in the kaolinite interlayer with the molecular plane oriented at small angles with respect to the interlayer surface. With continuous intercalation, the basal spacing readily reached a stable stage at 10.6 angstrom, where formamide rearranged its structure by rotating the molecule plane along the C N bond that was parallel to the interlayer surface, which resulted in the molecular plane orienting at higher angles with respect to the interlayer surface. During this process, the C=O groups oriented toward the hydroxyl groups on the interlayer octahedral surface, and one of N H bonds progressively pointed toward the basal oxygens on the opposing interlayer tetrahedral surface. Continuous intercalation can enlarge the basal spacing to more than 14 angstrom with the prerequisite of overcoming the energy barrier, and then formamide evolved to a disordered bilayer structure in the kaolinite interlayer. The affinity of kaolinite interlayer surfaces for formamide motivated the intercalation process. The octahedral surface displayed a relatively larger affinity toward formamide compared to the tetrahedral surface partially due to the presence of hydroxyl groups that are more active in the intermolecular interactions with formamide.
机译:在高岭石甲酰胺复合模型上进行分子动力学模拟,其中具有各种数量的甲酰胺分子在高岭石夹层中,探讨了在嵌入过程中的基础间距,能量和结构演变。另外,计算甲酰胺与高岭石层间表面的互晶相互作用。计算揭示了高岭石的基础间距在插入开始时扩大到9.6埃。甲酰胺在高岭土中间层中被布置为单层结构,其中分子面相对于中间层表面以小角度定向。通过连续插入,基部间距容易达到10.6埃的稳定阶段,其中甲酰胺通过沿着与层间表面平行的CN键旋转分子平面来重新排列其结构,这导致在较高角度上取向的分子面到层间表面。在该方法期间,朝向中间层八面体表面上的羟基取向的C = O基团,N H键之一逐渐朝向相对的中间层四面体表面上的基础氧。连续插入可以扩大基底间距到超过14埃的基础间距,并且具有克服能量屏障的先决条件,然后在高岭石中间夹层中的甲酰胺进化到无序的双层结构。高岭石层表面对甲酰胺的亲和力激励了嵌入过程。由于存在在与甲酰胺的分子间相互作用中更活跃的羟基的存在,与四面体表面相比,八面面表面与四面体表面相比显示了相对较大的亲和力。

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