Yuan Rongfeng, Napoli Joseph A, Yan Chang, Marsalek Ondrej, Markland Thomas E, Fayer Michael D
Department of Chemistry, Stanford University, Stanford, California 94305, United States.
Charles University, Faculty of Mathematics and Physics, Ke Karlovu 3, 121 16 Prague 2, Czech Republic.
ACS Cent Sci. 2019 Jul 24;5(7):1269-1277. doi: 10.1021/acscentsci.9b00447. Epub 2019 May 23.
Proton transfer in water is ubiquitous and a critical elementary event that, via proton hopping between water molecules, enables protons to diffuse much faster than other ions. The problem of the anomalous nature of proton transport in water was first identified by Grotthuss over 200 years ago. In spite of a vast amount of modern research effort, there are still many unanswered questions about proton transport in water. An experimental determination of the proton hopping time has remained elusive due to its ultrafast nature and the lack of direct experimental observables. Here, we use two-dimensional infrared spectroscopy to extract the chemical exchange rates between hydronium and water in acid solutions using a vibrational probe, methyl thiocyanate. Ab initio molecular dynamics (AIMD) simulations demonstrate that the chemical exchange is dominated by proton hopping. The observed experimental and simulated acid concentration dependence then allow us to extrapolate the measured single step proton hopping time to the dilute limit, which, within error, gives the same value as inferred from measurements of the proton mobility and NMR line width analysis. In addition to obtaining the proton hopping time in the dilute limit from direct measurements and AIMD simulations, the results indicate that proton hopping in dilute acid solutions is induced by the concerted multi-water molecule hydrogen bond rearrangement that occurs in pure water. This proposition on the dynamics that drive proton hopping is confirmed by a combination of experimental results from the literature.
质子在水中的转移无处不在,是一个关键的基本过程。通过水分子间的质子跳跃,质子扩散的速度比其他离子快得多。200多年前,格罗特斯首次发现了水中质子传输的反常性质问题。尽管现代进行了大量研究,但关于水中质子传输仍有许多未解决的问题。由于质子跳跃时间极快且缺乏直接的实验观测手段,其实验测定一直难以实现。在此,我们使用二维红外光谱,利用振动探针硫氰酸甲酯来提取酸性溶液中水合氢离子与水之间的化学交换速率。从头算分子动力学(AIMD)模拟表明,化学交换主要由质子跳跃主导。实验观测和模拟得出的酸浓度依赖性,使我们能够将测量得到的单步质子跳跃时间外推至稀溶液极限,在误差范围内,该值与通过质子迁移率测量和核磁共振线宽分析推断出的值相同。除了通过直接测量和AIMD模拟获得稀溶液极限下的质子跳跃时间外,结果还表明,稀酸溶液中的质子跳跃是由纯水中发生的多水分子协同氢键重排所引发的。文献中的一系列实验结果证实了这一关于驱动质子跳跃动力学的观点。