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Quasicontinuum simulation of fracture at the atomic scale

机译:原子尺度断裂的准连续谱模拟

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We study the problem of atomic scale fracture using the recently developed quasicontinuum method in which there is a systematic thinning of the atomic-level degrees of freedom in regions where they are not needed. Fracture is considered in two distinct settings. First, a study is made of cracks in single crystals, and second, we consider a crack advancing towards a grain boundary (GB) in its path. In the investigation of single crystal fracture, we evaluate the competition between simple cleavage and crack-tip dislocation emission. In addition, we examine the ability of analytic models to correctly predict fracture behaviour, and find that the existing analytical treatments are too restrictive in their treatment of nonlinearity near the crack tip. In the study of GB-crack interactions, we have found a number of interesting deformation mechanisms which attend the advance of the crack. These include the migration of the GB, the emission of dislocations from the GB, and deflection of the crack front along the GB itself. In each case, these mechanisms are rationalized on the basis of continuum mechanics arguments. [References: 55]
机译:我们使用最近开发的准连续谱方法研究了原子尺度断裂的问题,在该方法中,不需要原子序区域的原子级自由度在系统上变薄。在两种不同的情况下考虑骨折。首先,对单晶中的裂纹进行了研究,其次,我们认为裂纹在其路径中向晶界(GB)前进。在单晶断裂的研究中,我们评估了简单劈裂与裂纹尖端位错发射之间的竞争。此外,我们检查了分析模型正确预测断裂行为的能力,发现现有的分析处理对裂纹尖端附近非线性的处理过于严格。在GB-裂纹相互作用的研究中,我们发现了许多有趣的变形机制,它们参与了裂纹的发展。这些包括GB的迁移,GB的位错的散发以及沿GB本身的裂纹前沿的偏转。在每种情况下,这些机制都是基于连续力学原理进行合理化的。 [参考:55]

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