Department of Chemical Engineering, Vanderbilt University, Nashville, Tennessee, United States.
Langmuir. 2011 Jul 19;27(14):8700-9. doi: 10.1021/la2005826. Epub 2011 Jun 16.
Two different terminations of the (1010) surface of quartz (α and β) interacting with water are simulated by classical (CMD) (using two different force fields) and ab initio molecular dynamics (AIMD) and compared with previously published X-ray reflectivity (XR) experiments. Radial distribution functions between hydroxyl and water show good agreement between AIMD and CMD using the ClayFF force field for both terminations. The Lopes et al. (Lopes, P. E. M.; Murashov, V.; Tazi, M.; Demchuk, E.; MacKerell, A. D. J. Phys. Chem. B2006, 110, 2782-2792) force field (LFF), however, underestimates the extent of hydroxyl-water hydrogen bonding. The β termination is found to contain hydroxyl-hydroxyl hydrogen bonds; the quartz surface hydroxyl hydrogens and oxygens that hydrogen bond with each other exhibit greatly reduced hydrogen bonding to water. Conversely, the hydroxyl hydrogen and oxygens that are not hydrogen bonded to other surface hydroxyls but are connected to those that are show a considerable amount of hydrogen bonding to water. The electron density distribution of an annealed surface of quartz (1010) obtained by XR is in qualitative agreement with electron densities calculated by CMD and AIMD. In all simulation methods, the interfacial water peak appears farther from the surface than observed by XR. Agreement among AIMD, LFF, and XR is observed for the relaxation of the near-surface atoms; however, ClayFF shows a larger discrepancy. Overall, results show that for both terminations of (1010), LFF treats the near-surface structure more accurately whereas ClayFF treats the interfacial water structure more accurately. It is shown that the number of hydroxyl and water hydrogen bonds to the bridging Si-O-Si oxygens connecting the surface silica groups to the rest of the crystal is much greater for the α than the β termination. It is suggested that this may play a role in the greater resistance to dissolution of the β termination than that of the α termination.
两种不同的石英(α 和 β)(1010)表面的终止方式与水相互作用,通过经典(CMD)(使用两种不同的力场)和从头算分子动力学(AIMD)进行模拟,并与之前发表的 X 射线反射(XR)实验进行比较。羟基与水之间的径向分布函数在使用 ClayFF 力场时,AIMD 和 CMD 对两种终止方式都显示出良好的一致性。然而,Lopes 等人的力场(Lopes, P. E. M.; Murashov, V.; Tazi, M.; Demchuk, E.; MacKerell, A. D. J. Phys. Chem. B2006, 110, 2782-2792)(LFF)低估了羟基-水氢键的程度。β 终止方式被发现包含羟基-羟基氢键;与彼此氢键结合的石英表面羟基氢和氧对水的氢键结合大大减少。相反,没有与其他表面羟基氢键结合但与氢键结合的羟基氢和氧显示出与水相当大的氢键结合。通过 XR 获得的石英(1010)退火表面的电子密度分布与通过 CMD 和 AIMD 计算的电子密度分布定性一致。在所有模拟方法中,界面水峰出现在比 XR 观察到的表面更远的位置。AIMD、LFF 和 XR 之间观察到近表面原子的弛豫一致;然而,ClayFF 显示出更大的差异。总体而言,结果表明,对于(1010)的两种终止方式,LFF 更准确地处理近表面结构,而 ClayFF 更准确地处理界面水结构。结果表明,与β终止方式相比,与将表面硅氧基团连接到晶体其余部分的桥接 Si-O-Si 氧连接的羟基和水氢键的数量对于α终止方式要多得多。有人认为这可能在β终止方式比α终止方式更难溶解方面发挥作用。