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DFT Study of Interactions of Water on Kaolinite and Goethite Surfaces

机译:高岭土和甲石表面水相互作用的DFT研究

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Quantum-chemical DFT based simulations (relaxation and/or molecular dynamics) have been performed on models of surfaces of kaolinite and goethite minerals. Various structural models of surface sites, which are active in adsorption processes, have been investigated. Chemical activities of these sites have been estimated on the base of calculated interaction energies of water. It has been shown that hydrogen bonds represent a dominant mechanism in the formation of surface complexes with polar molecules. If the surface is formed from hydroxyl groups (the octahedral surface of kaolinite and the (110) surface of goethite) these OH groups are very flexible and are able to act as proton donors or acceptors in hydrogen bonds. On the other hand, if the surface is formed only from basal oxygen atom (the tetrahedral surface of kaolinite) only weak hydrogen bonds are formed with polar molecules. It has been possible to estimate energy of hydration for kaolinite on the base of calculated averaged energies from molecular dynamics for kaolinite surfaces covered wit a water layer. It has been shown that the goethite (110) surface offers several adsorption sites for the water molecules. The computed interaction energies for the goethite surface sites are larger (in absolute value) than for the octahedral kaolinite surface.
机译:对基于量子化学DFT基的模拟(放松和/或分子动力学)已经在高岭石和甲硝矿物质的型号上进行。研究了在吸附过程中活跃的各种结构模型。这些位点的化学活性估计了水的互动能量的基础上。已经表明,氢键在形成具有极性分子的表面络合物中表示主要机理。如果表面由羟基形成(高岭土的八面体表面和甲磺酸盐的(110)表面),则这些OH基团非常灵活,并且能够作为质子供体或氢键的受体。另一方面,如果表面仅从基础氧原子(高岭石的四面体表面)形成,则仅使用极性分子形成弱氢键。有可能估计高岭土的高岭石的水合能量,从覆盖水层的高岭石表面的分子动力学的计算平均能量。已经表明,鹅料(110)表面为水分子提供了几个吸附部位。用于Geethite表面位点的计算的相互作用能量比八面体高岭石表面更大(绝对值)。

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