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Initial stage of the 2D-3D transition of a strained SiGe layer on a pit-patterned Si(001) template

机译:应变siGe层的二维3D转换的初始阶段   凹坑图案的si(001)模板

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摘要

We investigate the initial stage of the 2D-3D transition of strained Gelayers deposited on pit-patterned Si(001) templates. Within the pits, whichassume the shape of inverted, truncated pyramids after optimized growth of a Sibuffer layer, the Ge wetting layer develops a complex morphology consistingexclusively of {105} and (001) facets. These results are attributed to astrain-driven step-meandering instability on the facetted side-walls of thepits, and a step-bunching instability at the sharp concave intersections ofthese facets. Although both instabilities are strain-driven, their coexistencebecomes mainly possible by the geometrical restrictions in the pits. It isshown that the morphological transformation of the pit surface into low-energyfacets has strong influence on the preferential nucleation of Ge islands at theflat bottom of the pits.
机译:我们调查沉积在凹坑图案的Si(001)模板上的应变Gelayers的2D-3D过渡的初始阶段。在凹坑内,假设Sibuffer层经过优化生长后,倒置的,截顶的金字塔形状,Ge浸润层形成复杂的形貌,仅包含{105}和(001)面。这些结果归因于凹坑的刻面侧壁上的应变驱动阶梯弯曲不稳定性,以及这些刻面的尖锐凹面交点处的阶梯束不稳定性。尽管这两种不稳定性都是由应变驱动的,但它们的共存主要是由于坑中的几何限制而可能实现的。结果表明,凹坑表面向低能小面的形态转化对凹坑平坦底部的Ge岛的优先成核有很大影响。

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