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Hydrophobicity of Talc Basal Surface~1

机译:滑石基面的疏水性〜1

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The hydrophobicity of the talc basal surface is considered in the framework of the concept which relates the properties of layered silicates and their dispersions to the differences between the characteristics of the basal and side surfaces of their particles. The ab initio calculations of the energetics and geometry of the microclusters formed by water molecules adsorbed on the active sites (oxygen ions) located at the perfect basal surface of talc are performed. It is shown that the typical property of the hydrophobic surface is the adsorption of single molecules of water on extremely scarce or weak active sites of the surface, which act as secondary adsorption sites, and subsequent adsorption of water molecules on these secondary sites which results in the formation of ring-like structures. The heat of adsorption on this surface is shown to be essentially lower than the water condensation heat, which is also indicative of the hydrophobicity of the basal surface of talc.
机译:在概念的框架内考虑了滑石基面的疏水性,该概念将层状硅酸盐的性质及其分散体与颗粒的基面和侧面特征之间的差异联系起来。从头算出了由聚集在滑石的完美基底表面上的活性位点(氧离子)上的水分子形成的微团簇的能量和几何形状。结果表明,疏水性表面的典型性质是单分子水在表面上极为稀缺或较弱的活性位点上的吸附,这些活性位点充当次级吸附位点,随后水分子在这些次级位点上的吸附导致环状结构的形成。显示在该表面上的吸附热基本上低于水凝结热,这也表明滑石基面的疏水性。

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