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Formation of a Ge-rich layer during the oxidation of strained Si_(1-x)Ge_x

机译:应变Si_(1-x)Ge_x氧化过程中富Ge层的形成

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摘要

The diffusion of Ge in Ge-rich layer (GRL) and the factors affecting on it during the oxidation of strained Si_(1-x)Ge_x layers were examined. Strained Si_(1-x)Ge_x layers, having different initial Ge concentrations (x=0.15 and 0.3), were oxidized at 800 and 900℃ in a dry O_2 ambient for different oxidation times. The diffusion of Ge into the underlying Si_(1-x)Ge_x layer having an initial constant composition and the resulting transformation to GRL were both enhanced with an increase in oxidation temperature. After complete transformation to GRL, GeO_2 started to become incorporated into the resulting oxide layer. The formation of GeO_2 was initiated by the Ge saturation of the GRL layer with Ge and by the differences in diffusivity of Ge atoms in Si_(1-x)Ge_x and Si substrate. The relaxation occurred when the Ge concentration in the GRL reached a critical value and was not affected by either oxidation time or temperature.
机译:研究了应变应变Si_(1-x)Ge_x层氧化过程中Ge在富Ge层(GRL)中的扩散及其影响因素。具有不同初始Ge浓度(x = 0.15和0.3)的应变Si_(1-x)Ge_x层在干燥的O_2环境中于800和900℃下氧化了不同的氧化时间。随着氧化温度的升高,Ge向具有初始恒定组成的Si_(1-x)Ge_x层中的扩散以及向GRL的转变均得到增强。在完全转化为GRL之后,GeO_2开始掺入到所得的氧化物层中。 GeO_2的形成是由于GRL层中的Ge充满了Ge,以及Si_(1-x)Ge_x和Si衬底中Ge原子扩散系数的差异所致。当GRL中的Ge浓度达到临界值且不受氧化时间或温度的影响时,就会发生弛豫。

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