Institute of Multidisciplinary Research for Advanced Materials, Tohoku University, Sendai, 980-8577, Japan.
Langmuir. 2012 Oct 9;28(40):14284-90. doi: 10.1021/la303003u. Epub 2012 Sep 26.
We investigated interfacial water, formed by adsorption or phase separation (prewetting transition), on a silica surface in water-cyclohexane binary liquids using a combination of colloidal probe atomic force microscopy (AFM) and sum frequency generation (SFG) vibrational spectroscopy. At 33 ± 9 ppm water, the long-range attraction extending to 19.4 ± 2.9 nm appeared, which was caused by the contact of water layers formed on silica surfaces. The attraction range increased with increasing water concentration and reached 97 ± 17 nm at the saturation concentration of water in cyclohexane (C*), indicating that the thickness of the water layer formed on silica was ca. 50 nm. The interfacial energy between the water adsorption layer and bulk solution (γ = 79.3 ± 2.0 mN/m) was estimated from the pull-off force, and was significantly larger than the value for the bulk water/cyclohexane interface (γ = 50.1 mN/m). SFG spectroscopy demonstrated that the interfacial water formed an icelike structure at C*. These results indicated that the interfacial water molecules formed an icelike ordered structure induced by the hydrogen bonding with surface silanol groups, resulting in the free OH groups being more exposed to the bulk solution. On the other hand, the water adsorption layer induced by phase separation at water concentrations above C* was found to be less ordered and its structure at the adsorption layer/bulk interface was almost the same as that of bulk water, although its thickness was almost the same as that formed at C*. To our knowledge, this is the first report of the observation of liquid adsorption layers formed by chemical interaction up to saturation and by the wetting transition above saturation, and their differences in the structure and properties at the molecular level.
我们使用胶体探针原子力显微镜(AFM)和和频发生(SFG)振动光谱相结合的方法,研究了水-环己烷二元液体中吸附或相分离(预润湿转变)形成的二氧化硅表面界面水。在 33±9ppm 的水浓度下,出现了延伸至 19.4±2.9nm 的长程吸引力,这是由在二氧化硅表面形成的水层接触引起的。随着水浓度的增加,吸引力范围增加,在环己烷中达到水的饱和浓度(C*)时达到 97±17nm,表明在二氧化硅上形成的水层厚度约为 50nm。从拉起力估计了吸附层和本体溶液之间的界面能(γ=79.3±2.0mN/m),该值明显大于本体水/环己烷界面的值(γ=50.1mN/m)。SFG 光谱表明,在 C时界面水形成了类似冰的结构。这些结果表明,界面水分子通过与表面硅醇基团的氢键形成了类似冰的有序结构,导致更多的游离 OH 基团暴露在本体溶液中。另一方面,在 C以上的水浓度下,通过相分离形成的水吸附层被发现结构无序,其在吸附层/本体界面处的结构与本体水几乎相同,尽管其厚度与在 C*处形成的厚度几乎相同。据我们所知,这是首次报道在分子水平上观察到化学相互作用直至饱和以及超过饱和的润湿转变形成的液体吸附层,以及它们在结构和性质上的差异。