Department of Matserials Science and Engineering, Rutgers University, 607 Taylor Road, Piscataway, New Jersey 08855, United States.
J Phys Chem B. 2023 Apr 20;127(15):3392-3401. doi: 10.1021/acs.jpcb.2c06490. Epub 2023 Apr 10.
Molecular simulations of auto-dissociation of water molecules in an 81,000 atom bulk water system show that the electric field variations caused by local bond length and angle variations enhance proton transfer within ∼600 fs prior to auto-dissociation. In this paper, auto-dissociation relates to the initial separation of a proton from a water molecule to another, forming the HO and OH ions. Only transfers for which a proton's initial nearest covalently bonded oxygen remained the same for at least 1 ps prior to the transfer and for which that proton's new nearest acceptor oxygen remained the same for at least 1 ps after the transfer were evaluated. Electric fields from solvent atoms within 6 Å of a transferring proton (H*) are dominant, with little contribution from farther molecules. However, exclusion of the accepting oxygen in such electric field calculations shows that the field on H* from the other solvent atoms weakens as the time to transfer becomes less than 600 fs, indicating the primary importance of the accepting oxygen on enabling auto-dissociation. All resultant OH and HO ion pairs recombined at times greater than 1 ps after auto-dissociation. A concentration of 8.01 × 10 cm for these ion pairs was observed. The simulations indicate that transient auto-dissociation in water is more common than that inferred from dc-conductivity experiments (10 vs 10) and is consistent with the results of calculations that include nuclear quantum effects. The conductivity experiments require the rearrangement of farther water molecules to form hydrogen-bonded "water wires" that afford long-range and measurable proton transport away from the reaction site. Nonetheless, the relatively large number of picosecond-lived auto-dissociation products might be engineered within 2D layers and oriented external fields to offer new energy-related systems.
对 81000 个原子的 bulk 水体系中水分子自动离解的分子模拟表明,在自动离解之前约 600fs 内,局部键长和键角变化引起的电场变化增强了质子转移。在本文中,自动离解与质子从一个水分子向另一个水分子的初始分离有关,形成 HO 和 OH 离子。仅评估那些质子最初与其共价键合的氧在转移前至少 1ps 内保持相同,并且该质子的新最近受体氧在转移后至少 1ps 内保持相同的转移。距转移质子(H*)6Å 内溶剂原子的电场占主导地位,来自更远分子的贡献很小。然而,在这些电场计算中排除接受氧表明,当转移时间小于 600fs 时,来自其他溶剂原子的 H*上的场变弱,这表明接受氧在实现自动离解方面的主要重要性。所有生成的 OH 和 HO 离子对在自动离解后大于 1ps 的时间重新结合。观察到这些离子对的浓度为 8.01×10cm。模拟表明,水中的瞬态自动离解比从直流导率实验推断的更常见(10 比 10),并且与包括核量子效应的计算结果一致。电导率实验需要重新排列更远的水分子,以形成氢键“水线”,从而提供远离反应位点的长程和可测量的质子传输。尽管如此,在二维层内和外部取向场中可能会设计出相对大量的皮秒寿命的自动离解产物,以提供新的与能量相关的系统。