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Study of the influence of oxygen on structural perfection of silicon single crystals by high-resolution X-ray diffraction and infrared absorption measurements

机译:高分辨率X射线衍射和红外吸收测量研究氧对硅单晶结构完善的影响

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High-resolution X-ray diffractometry, absolute integrated intensity (rho) measurements, diffuse X-ray scattering (DXS) and infrared (IR) absorption techniques were used to investigate the influence of oxygen on the structural perfection of high purity (resistivity of the order of 4 k Omega cm) float zone (FZ) grown (111) silicon single crystals. A multicrystal diffractometer set in (+, -, -, +) geometry, with Mo K alpha(1) radiation, was employed. From the infrared measurements, the oxygen concentration in the sample was determined to be 1.3 x 10(17) atoms cm(-3). High-resolution X-ray diffraction curves of the as-grown crystal had half-widths of similar to 11 arcsec; the rho value was 3.5 x 10(-5) rad. To incorporate oxygen in a controlled manner into the specimens, they were annealed under dry oxygen ambient for 8 h in the temperature range 573-1373 K tin eight steps). Up to 723 K there was no appreciable change in oxygen content or in the: degree of perfection. Annealing at temperatures (A(T)) > 873 K resulted in considerable increases in the oxygen content, as well as significant improvements in the degree of perfection. For example, as the level of oxygen increased from 1.3 x 10(17) to 3.6 x 10(17) atoms cm(-3) for A(T) = 873 K, the values of half-widths and rho decreased to similar to 7 arcsec and 2.4 x 10(-5) rad, respectively. However, annealing above 1273 K produced deterioration in lattice perfection. DXS measurements showed remarkable changes in the nature of point defects and their clusters with change in A(T). Up to A(T) = 973 K, the defects were predominantly vacancy clusters. However, with A(T) in the range 1073-1273 K, the predominent defects were isolated interstitials. Further increase in A(T) led to interstitial cluster formation, which deteriorated the lattice perfection. This study clearly demonstrates that oxygen concentration in the range similar to 3 x 10(17) to 13 x 10(17) atoms cm(-3) leads to significant improvement in structural perfection of silicon single crystals. [References: 26]
机译:高分辨率X射线衍射仪,绝对积分强度(rho)测量,漫射X射线散射(DXS)和红外(IR)吸收技术用于研究氧对高纯度结构完美性的影响数量级为4 k Omega cm)的浮区(FZ)生长的(111)硅单晶。使用多晶衍射仪,其几何形状设置为(+,-,-,+),且具有Mo K alpha(1)辐射。根据红外测量,样品中的氧气浓度确定为1.3 x 10(17)原子cm(-3)。刚生长的晶体的高分辨率X射线衍射曲线的半宽度类似于11弧秒。 rho值为3.5 x 10(-5)rad。为了以可控方式将氧气掺入样品中,将其在干燥氧气环境下(温度范围为573-1373 K(八步))退火8小时。高达723 K,氧含量或完美度没有明显变化。在> 873 K的温度下退火(A(T))导致氧含量的显着增加,以及完美度的显着提高。例如,对于A(T)= 873 K,随着氧气水平从1.3 x 10(17)原子cm(-3)增加到3.6 x 10(17)cm(-3),半角宽和rho值减小到与7 arcsec和2.4 x 10(-5)rad。但是,高于1273 K的退火会导致晶格完美度下降。 DXS测量表明,随着A(T)的变化,点缺陷及其簇的性质发生了显着变化。直到A(T)= 973 K,缺陷主要是空位簇。但是,如果A(T)在1073-1273 K范围内,则主要缺陷是孤立的插页式广告。 A(T)的进一步增加导致间隙簇的形成,从而破坏了晶格的完美性。这项研究清楚地表明,氧浓度在类似于3 x 10(17)到13 x 10(17)原子cm(-3)的范围内会导致单晶硅结构完善性的显着提高。 [参考:26]

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