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Quantum chemical study of the adsorption of water molecules on kaolinite surfaces

机译:水分子在高岭石表面吸附的量子化学研究

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Kaolinite is a kind of layered aluminosilicate showing a large variety of physicochemical properties. In this research, various gas phase properties of interactions between the Si-0 layer (Si_6O_(18)H_(12)) or Al-0 layer (Al_6O_(24)H_(30)) cluster model of kaolinite and n water molecules (n = 1-3) have been systematically explored at the B3LYP [Becke's three-parameter hybrid exchange functional (B3) and the correlation functional of Lee, Yang, and Parr (LYP)] level using the 6-31G(d) basis set. These gas phase properties include optimal structures, structural parameters, hydrogen bonds, interaction energies, natural bond orbital charge distributions, vibration frequencies, electron density characteristicse and maps of electronic potential. The most stable structures of each system have been obtained when one, two and three water molecules are adsorbed on each surface. With an increasing number of water molecules; there are also hydrogen bonds between water molecules besides the hydrogen bonds between water and the kaolinite surface. The results show that the stabilization of hydrogen bonds is closely connected with the kaolinite surface type, surface structure, and position and orientation towards the surface of water molecules. Moreover, the Al-O/water system is more stable than the Si-O/water system. Simultaneously, the hydrogen bonds formed between water molecules are the strongest, followed by those between water and the Al-O layer and lastly those between water and the Si-0 layer.
机译:高岭石是一种层状的铝硅酸盐,具有多种理化性质。在这项研究中,高岭石与n个水分子的Si-0层(Si_6O_(18)H_(12))或Al-0层(Al_6O_(24)H_(30))团簇模型之间相互作用的各种气相性质( n = 1-3)已使用6-31G(d)基集在B3LYP [Becke的三参数混合交换函数(B3)和Lee,Yang和Parr(LYP)的相关函数]级别上系统地进行了探索。 。这些气相性质包括最佳结构,结构参数,氢键,相互作用能,自然键轨道电荷分布,振动频率,电子密度特征和电子势图。当一个,两个和三个水分子吸附在每个表面上时,将获得每个系统最稳定的结构。随着水分子数量的增加;除了水和高岭石表面之间的氢键外,水分子之间还存在氢键。结果表明,氢键的稳定与高岭石的表面类型,表面结构以及对水分子表面的位置和取向密切相关。而且,Al-O /水系统比Si-O /水系统更稳定。同时,水分子之间形成的氢键最强,其次是水和Al-O层之间的氢键,最后是水和Si-0层之间的氢键。

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