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Atomic Scale Formation Mechanism of Edge Dislocation Relieving Lattice Strain in a GeSi overlayer on Si(001)

机译:Si(001)上GeSi覆盖层中位错释放晶格应变的原子尺度形成机理

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摘要

Understanding how edge misfit dislocations (MDs) form in a GeSi/Si(001) film has been a long standing issue. The challenge is to find a mechanism accounting for the presence of these dislocations at the interface since they are not mobile and cannot nucleate at the surface and glide towards the interface. Furthermore, experiments can hardly detect the nucleation and early stages of growth because of the short time scale involved. Here we present the first semi-quantitative atomistic calculation of the formation of edge dislocations in such films. We use a global optimization method and density functional theory calculations, combined with computations using potential energy functions to identify the best mechanisms. We show that those previously suggested are relevant only for a low film strain and we propose a new mechanism which accounts for the formation of edge dislocations at high film strain. In this one, a 60° MD nucleates as a “split” half-loop with two branches gliding on different planes. One branch belongs to the glide plane of a complementary 60° MD and therefore strongly favors the formation of the complementary MD which is immediately combined with the first MD to form an edge MD.
机译:长期以来,了解GeSi / Si(001)薄膜中边缘失配位错(MD)的形成方式一直是一个长期的问题。面临的挑战是找到一种机制,以解决这些位错在界面处的存在,因为它们不移动并且不能在表面成核并滑向界面。此外,由于所涉及的时间短,实验几乎无法检测出成核和生长的早期阶段。在这里,我们介绍了这种薄膜边缘位错形成的第一个半定量原子计算。我们使用全局优化方法和密度泛函理论计算,并结合使用势能函数的计算来确定最佳机制。我们表明,以前提出的那些仅与低膜应变有关,并且我们提出了一种新机制,该机制解释了在高膜应变下边缘位错的形成。在该图中,一个60°MD成“分裂”半环成核,两个分支在不同平面上滑动。一个分支属于互补60°MD的滑行平面,因此强烈支持互补MD的形成,该互补MD立即与第一MD结合以形成边缘MD。

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