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Fracture, water dissociation, and proton conduction in SiO2 nanochains

机译:SiO2纳米链中的断裂,水离解和质子传导

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摘要

A basic issue in nanoscale systems is whether large-scale behavior occurs or not. At and above the mesoscale, the water-silica interaction is known to have large effects, e.g., the geological importance of hydrolytic weakening. Here, we show that water not only substantially weakens a silica nanochain that has been the focus of much recent research but also leads to novel proton conduction. The SiO2 chain consists of a string of orthogonal (planes alternating vertically and horizontally) two-membered rings. We treat two cases of adjacent water to understand both local and collective motion in the system. The first is two water molecules, the second is a water monolayer film that coats the entire chain. Structure, charge separation, stress dependent bond breaking and formation, and proton conduction are discussed based on results obtained at the room temperature. The simulations have been performed using both first-principles molecular dynamics and a novel multiscale quantum-classical software system.
机译:纳米系统中的一个基本问题是是否发生大规模行为。在中尺度以上,已知水-二氧化硅相互作用具有很大的作用,例如,水解弱化的地质重要性。在这里,我们表明水不仅大大削弱了二氧化硅纳米链(这是许多近期研究的重点),而且还导致了新型的质子传导。 SiO2链由一串正交的(垂直和水平交替的平面)两元环组成。我们处理相邻水的两种情况,以了解系统中的局部运动和集体运动。第一个是两个水分子,第二个是覆盖整个链的水单层膜。基于在室温下获得的结果,讨论了结构,电荷分离,应力相关的键断裂和形成以及质子传导。已经使用第一性原理分子动力学和新颖的多尺度量子经典软件系统进行了模拟。

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