Uhlig Manuel R, Benaglia Simone, Thakkar Ravindra, Comer Jeffrey, Garcia Ricardo
Instituto de Ciencia de Materiales de Madrid, CSIC, c/Sor Juana Inés de la Cruz 3, 28049 Madrid, Spain.
Nanotechnology Innovation Center of Kansas State, Department of Anatomy and Physiology, Kansas State University, Manhattan, Kansas 66506, USA.
Nanoscale. 2021 Mar 18;13(10):5275-5283. doi: 10.1039/d1nr00351h.
Hydration layers are formed on hydrophilic crystalline surfaces immersed in water. Their existence has also been predicted for hydrophobic surfaces, yet the experimental evidence is controversial. Using 3D-AFM imaging, we probed the interfacial water structure of hydrophobic and hydrophilic surfaces with atomic-scale spatial resolution. We demonstrate that the atomic-scale structure of interfacial water on crystalline surfaces presents two antagonistic arrangements. On mica, a common hydrophilic crystalline surface, the interface is characterized by the formation of 2 to 3 hydration layers separated by approximately 0.3 nm. On hydrophobic surfaces such as graphite or hexagonal boron nitride (h-BN), the interface is characterized by the formation of 2 to 4 layers separated by about 0.5 nm. The latter interlayer distance indicates that water molecules are expelled from the vicinity of the surface and replaced by hydrocarbon molecules. This creates a new 1.5-2 nm thick interface between the hydrophobic surface and the bulk water. Molecular dynamics simulations reproduced the experimental data and confirmed the above interfacial water structures.
水合层形成于浸入水中的亲水性晶体表面。对于疏水性表面,也有人预测过它们的存在,但实验证据存在争议。我们使用三维原子力显微镜成像,以原子尺度的空间分辨率探测了疏水性和亲水性表面的界面水结构。我们证明,晶体表面界面水的原子尺度结构呈现出两种相互对立的排列方式。在云母(一种常见的亲水性晶体表面)上,界面的特征是形成了两到三层水合层,层间距约为0.3纳米。在疏水性表面,如石墨或六方氮化硼(h-BN)上,界面的特征是形成了两到四层,层间距约为0.5纳米。后者的层间距离表明水分子从表面附近被排挤出去,并被碳氢化合物分子取代。这在疏水性表面和本体水之间形成了一个新的1.5 - 2纳米厚的界面。分子动力学模拟重现了实验数据,并证实了上述界面水结构。