首页> 外文期刊>Geoderma: An International Journal of Soil Science >Wettability of kaolinite (001) surfaces - molecular dynamic study. (Special Issue: Advances of molecular modeling of biogeochemical interfaces in soils.)
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Wettability of kaolinite (001) surfaces - molecular dynamic study. (Special Issue: Advances of molecular modeling of biogeochemical interfaces in soils.)

机译:高岭石(001)表面的润湿性-分子动力学研究。 (特刊:土壤中生物地球化学界面的分子模型研究进展。)

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摘要

Wettability of two (001) basal kaolinite surfaces (tetrahedral and octahedral) was investigated by means of force-field molecular dynamics simulation. Water nanodroplets were deposited on the surfaces and microscopic contact angle was determined from a droplet profile. In case of the octahedral surface the nanodroplet was spread on the surface forming an incomplete monomolecular layer. Multiple, relatively strong hydrogen bonds of the water layer with the surface hydroxyl groups are responsible for the spreading. The contact angle for the octahedral surface is equal zero, thus this surface is strongly hydrophilic. In case of the tetrahedral surface water molecules of the droplet stayed together forming a deformed sphere on the surface. The computed microscopic contact angle is about 105 degrees meaning that the tetrahedral surface is hydrophobic. In spite of weak interactions of the droplet with this surface the water in the vicinity of the surface is structured and ordered into a form of monomolecular water layers with altering density what reflects a polarization effect of the surface. The experimental values of contact angle for kaolinite are about 20 degrees which indicates that the overall character of the kaolinite surface is hydrophilic and our calculations document that a key factor for this property is surface hydroxyl groups of the octahedral surface.
机译:通过力场分子动力学模拟研究了两个(001)基性高岭石表面(四面体和八面体)的润湿性。将水纳米滴沉积在表面上,并从液滴轮廓确定微观接触角。在八面体表面的情况下,纳米液滴散布在表面上,形成不完整的单分子层。水层与表面羟基的多个相对较强的氢键负责铺展。八面体表面的接触角等于零,因此该表面是强亲水性的。在四面体表面的情况下,液滴的水分子保持在一起,从而在表面上形成变形的球体。计算出的微观接触角约为105度,这意味着四面体表面是疏水的。尽管液滴与该表面的相互作用较弱,但表面附近的水仍被结构化并排列为单分子水层,其密度发生变化,反映了表面的极化作用。高岭石的接触角的实验值约为20度,这表明高岭石表面的整体特性是亲水的,我们的计算表明该特性的关键因素是八面体表面的表面羟基。

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