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Theoretical study of interactions of dickite and kaolinite with small organic molecules

机译:地开石和高岭石与有机小分子相互作用的理论研究

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摘要

Intercalates and adsorbates of two minerals of the kaolin group (kaolinite and dickite) with formamide (FA), N-methyl-formamide (MFA) and dimethylsulfoxide (DMSO) were investigated using the B3LYP/3-21G~* method of representative cluster models. Geometry optimisation of interacting molecules as well as of outer -OH groups of the octahedral sheet of the dickite and kaolinite layer was performed. Positions of molecules with respect to mineral layers were found. Formations and orientations of hydrogen bonds between intercalated or adsorbed molecules and layers were indicated. Interaction energies of intercalates and adsorbates were calculated and corrected to the basis set superposition error (BSSE). Intercalation energies are significantly larger than adsorption ones, thus showing the importance of additional stabilisation of the intercalated molecule in the interlayer space. The order of the stabilisation of intercalates is dickite-FA > dickite-MFA > kaolinite-DMSO. The same order is also observed for adsorbed systems.
机译:使用代表性簇模型的B3LYP / 3-21G〜*方法研究了高岭土类两种矿物(高岭石和重沸石)与甲酰胺(FA),N-甲基甲酰胺(MFA)和二甲基亚砜(DMSO)的插层和吸附物。 。对地开石和高岭石层的八面体片的相互作用分子以及外部-OH基团进行了几何优化。发现了相对于矿物层的分子位置。指出了插入或吸附的分子与层之间氢键的形成和取向。计算了嵌入物和吸附物的相互作用能,并将其校正为基组叠加误差(BSSE)。插层能量明显大于吸附能,因此显示出在层间空间中进一步稳定插层分子的重要性。插层物的稳定顺序为地开石-FA>地开石-MFA>高岭石-DMSO。对于吸附系统也观察到相同的顺序。

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