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首页> 外文期刊>Journal of Materials Engineering and Performance >All-Atom Molecular-Level Analysis of the Ballistic-Impact-Induced Densification and Devitrification of Fused Silica
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All-Atom Molecular-Level Analysis of the Ballistic-Impact-Induced Densification and Devitrification of Fused Silica

机译:弹道冲击诱导的熔融石英致密化和失透的全原子分子水平分析

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All-atom molecular-level computations are carried out to infer the dynamic response and material microstructure/topology changes of fused silica subjected to ballistic impact by a hard projectile. The analysis was focused on the investigation of specific aspects of the dynamic response and of the microstructural changes such as the deformation of highly sheared and densified regions and the conversion of amorphous fused silica to SiO2 crystalline allotropic modifications (in particular, alpha-quartz and stishovite). The microstructural changes in question were determined by carrying out a post-processing atom-coordination procedure. This procedure suggested the formation of stishovite (and perhaps alpha-quartz) within fused silica during ballistic impact. To rationalize the findings obtained, the all-atom molecular-level computational analysis is complemented by a series of quantum-mechanics density functional theory (DFT) computations. The latter computations enable determination of the relative potential energies of the fused silica, alpha-quartz, and stishovite under ambient pressure (i.e., under their natural densities) as well as under imposed (as high as 50 GPa) pressures (i.e., under higher densities) and shear strains. In addition, the transition states associated with various fused-silica devitrification processes were identified. The results obtained are found to be in good agreement with their respective experimental counterparts.
机译:进行全原子分子水平的计算,以推断受到硬弹丸弹道冲击的熔融石英的动态响应和材料微观结构/拓扑变化。该分析的重点是研究动态响应和微观结构变化的特定方面,例如高剪切和致密区域的变形以及非晶态熔融二氧化硅向SiO2结晶同素异形体转变(特别是α-石英和辉石)的转化。 )。所讨论的微观结构变化是通过进行后处理原子配位程序确定的。该过程表明在弹道撞击过程中在熔融石英中形成了辉石(可能还有α-石英)。为了合理化所获得的发现,全原子分子级计算分析辅以一系列量子力学密度泛函理论(DFT)计算。后面的计算可以确定在环境压力下(即,在其自然密度下)以及在施加的压力(高达50 GPa)下(即,在较高的压力下)熔融石英,α-石英和辉石的相对势能密度和剪切应变。此外,还确定了与各种熔融石英失透过程相关的过渡态。发现获得的结果与它们各自的实验对应物良好吻合。

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