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First-principles molecular-dynamics simulations of a hydrous silica melt: Structural properties and hydrogen diffusion mechanism

机译:含水二氧化硅的第一原理分子动力学模拟   熔体:结构性质和氢扩散机制

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摘要

We use {\it ab initio} molecular dynamics simulations to study a sample ofliquid silica containing 3.84 wt.% H$_2$O.We find that, for temperatures of3000 K and 3500 K,water is almost exclusively dissolved as hydroxyl groups, thesilica network is partially broken and static and dynamical properties of thesilica network change considerably upon the addition of water.Water moleculesor free O-H groups occur only at the highest temperature but are not stable anddisintegrate rapidly.Structural properties of this system are compared to thoseof pure silica and sodium tetrasilicate melts at equivalent temperatures. Thesecomparisons confirm the picture of a partially broken tetrahedral network inthe hydrous liquid and suggest that the structure of the matrix is as muchchanged by the addition of water than it is by the addition of the same amount(in mole %) of sodium oxide. On larger length scales, correlations arequalitatively similar but seem to be more pronounced in the hydrous silicaliquid. Finally, we study the diffusion mechanisms of the hydrogen atoms in themelt. It turns out that HOSi$_2$ triclusters and SiO dangling bonds play adecisive role as intermediate states for the hydrogen diffusion.
机译:我们使用分子动力学模拟研究了含有3.84 wt。%H $ _2 $ O的液态二氧化硅样品。我们发现,在3000 K和3500 K的温度下,水几乎完全溶解为羟基,二氧化硅添加水后,二氧化硅网络部分破裂,二氧化硅网络的静态和动态性质发生很大变化。水分子或游离的OH基团仅在最高温度下出现,但不稳定且迅速分解。该系统的结构性质与纯二氧化硅和四硅酸钠在等效温度下熔化。这些比较证实了含水液体中部分四面体网络的破裂,并表明与加入相同量(摩尔%)的氧化钠相比,加水改变了基体的结构。在较大的长度尺度上,相关性在质量上相似,但在含水二氧化硅液体中似乎更为明显。最后,我们研究了氢原子在主观原子中的扩散机理。事实证明,HOSi $ _2 $三角键和SiO悬空键作为氢扩散的中间态起着决定性的作用。

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