Hefei National Laboratory for Physical Sciences at the Microscale, Department of Chemical Physics, and Synergetic Innovation Center of Quantum Information & Quantum Physics, University of Science and Technology of China, Hefei, Anhui 230026, China.
J Am Chem Soc. 2021 Aug 25;143(33):13074-13081. doi: 10.1021/jacs.1c03581. Epub 2021 Aug 13.
Hydrophobic-like water monolayers have been predicted at the metal and some polar surfaces by theoretical simulations. However, direct experimental evidence for the presence of this water layer at surfaces, particularly at biomolecule and polymer surfaces, is yet to be validated at room temperature. Here we observe experimentally that an ordered molecular water layer is present at the hydrophobic fluorinated polymer such as polytetrafluoroethylene (PTFE) surface by using sum frequency generation vibrational spectroscopy. The macroscopic hydrophobicity of PTFE surface is actually hydrophilic at the molecular level. The macroscopically hydrophobic character of PTFE is indeed resulting from the hydrophobicity of the ordered two-dimension (2D) water layer, in which cyclic water tetramer structure is found. The water layer at humidity of ≤40% has a vibrational relaxation time of 550 ± 60 fs. The vibrational relaxation time in the frequency range of 3200-3400 cm shows remarkable difference from the interfacial water at the air/HO interface and the lipid/HO interface. No discernible frequency dependence of the vibrational relaxation time is observed, indicating the homogeneous dynamics of OH groups in the water layer. These insights into the water layer at the macroscopically hydrophobic surface may contribute to a better understanding of the hydrophobic interaction and interfacial water dynamics.
疏水性类似的水单分子层已经通过理论模拟预测存在于金属和一些极性表面上。然而,在室温下,在表面,特别是在生物分子和聚合物表面,仍然需要实验来验证这种水层的存在。在这里,我们通过使用和频产生振动光谱实验观察到,在疏水性氟化聚合物如聚四氟乙烯(PTFE)表面存在有序的分子水层。PTFE 表面的宏观疏水性实际上在分子水平上是亲水性的。PTFE 的宏观疏水性确实是由于有序二维(2D)水层的疏水性所致,其中发现了环状水四聚体结构。在湿度≤40%的情况下,水层的振动弛豫时间为 550±60fs。在 3200-3400cm 的频率范围内,振动弛豫时间与空气/HO 界面和脂质/HO 界面的界面水表现出显著差异。没有观察到振动弛豫时间的明显频率依赖性,这表明水层中 OH 基团的动力学是均匀的。这些对宏观疏水性表面上水层的见解可能有助于更好地理解疏水相互作用和界面水动力学。