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Reaction Activity of Kaolinite Surfaces: Quantum Chemistry Calculations

机译:高岭石表面的反应活性:量子化学计算

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The anion-kaolinite surface interactions and AuS~- adsorption onto the surfaces of kaolinite were studied using the self-consistent-field discrete variation (SCF -X_(alpha)-DV) method. Electronic structure and energies of the system of anion AuS~- adsorbed on an atomic cluster of kaolinite were calculated. The results show that the systems with lower total energy are those AuS~- adsorbed on the edge surfaces, which indicates that the systems of adsorption of AuS~- on the edges are more stable relative to those adsorbed on the basal plane. On the other hand, bond order data suggest that significant shifting of atomic charge and the overlapping of electronic cloud between Au (I) of the AuS~- and the surface ions of kaolinite would take place in the systems with AuS~- being adsorbed on the edges, especially at the site near Al octahedra. Therefore, it can be concluded that edge sites will dominate the complexation reactions of the surfaces of kaolinite, with negligible contributions from other functional groups on the basal plane, which are dominated by either siloxane sites in silica layers or aluminol sites in gibbsite layers.
机译:使用自洽场离散变化(SCF-X_α-DV)方法研究了阴离子-高岭石表面相互作用和AuS〜-在高岭石表面上的吸附。计算了吸附在高岭石原子簇上的AuS〜-阴离子的电子结构和能量。结果表明,具有较低总能量的系统是那些吸附在边缘表面上的AuS--,这表明相对于在基面上吸附的AuS--在边缘上的吸附系统更稳定。另一方面,键序数据表明,在吸附有AuS〜-的系统中,AuS〜-的Au(I)与高岭石的表面离子之间原子电荷的显着移动和电子云的重叠将发生。边缘,特别是在八面体附近的位置。因此,可以得出结论,边缘位点将主导高岭石表面的络合反应,而在基面上的其他官能团的贡献可忽略不计,这些官能团由二氧化硅层中的硅氧烷位点或三水铝石层中的氧化铝位点支配。

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