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首页> 外文期刊>Journal of Applied Physics >Nuclear microanalysis of oxygen concentration in liquid‐phase epitaxial gallium phosphide
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Nuclear microanalysis of oxygen concentration in liquid‐phase epitaxial gallium phosphide

机译:液相外延磷化镓中氧浓度的核微分析

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摘要

The total bulk oxygen concentration has been determined in GaP layers grown by liquid-phase epitaxy. Layers were grown doped with 18O enriched oxygen, and the 18O concentrations were measured by detecting α particles emitted during proton irradiation using the nuclear reaction 18O(p, a)15N. The relative concentrations of 18O and 16O were determined from exciton luminescence of the LiILiGaOP complex at 4.2°K after Li diffusion, thus enabling the total bulk oxygen concentrations to be determined. The total solid solubility of oxygen in GaP containing the optimum zinc concentration for efficient luminescence from Zn-O nearest-neighbor pairs, 5 × 1017 cm-3, ranged from [sine wave] 5 × 1016 cm-3 at [sine wave] 1040°C to [sine wave] 9 × 1016 cm-3 at ≳1100°C. Measurements on a layer doped with tellurium and oxygen failed to detect any 18O, indicating that the total oxygen concentration was probably ≪ 4 × 1016 cm-3. The experimental results confirmed the presence of Ga2O3 coprecipitates when the oxygen added to the liquid phase was greater than the solubility. Channeling experiments to determine the oxygen site location were done, but the results were inconclusive. The methods of crystal preparation and 18O doping are described, and the techniques employed to prevent oxygen isotope exchange are discussed. Other experimental techniques which are described include a large solid angle α-particle detector arrangement which also allowed sample orientation, a graded thickness foil which stopped backscattered protons and preserved the α-particle resolution, and the methods for minimizin g and correcting for boron background which occurs through the reaction 11B(p, α)8Be*.
机译:已经通过液相外延生长的GaP层中确定了总的总氧浓度。使层生长掺杂有富含18O的氧气,并使用核反应18O(p,a)15N通过检测质子辐照期间发射的α颗粒来测量18O浓度。由LiILiGaGaOP络合物在Li扩散后于4.2°K的激子发光确定18O和16O的相对浓度,因此可以确定总的总氧浓度。 GaP中氧气的总固溶度,其中包含用于从Zn-O最近邻居对有效发光的最佳锌浓度的最佳锌浓度5×1017 cm-3,在[正弦波] 1040时,范围为[正弦波] 5×1016 cm-3。 °C至[正弦波]在1100°C下为9×1016 cm-3。在掺杂了碲和氧的层上进行的测量未能检测到任何18 O,表明总氧浓度可能约为4×1016 cm-3。实验结果证实,当添加到液相中的氧大于溶解度时,Ga2O3会共沉淀。进行了确定氧位点位置的通道实验,但结果尚无定论。描述了晶体制备和18O掺杂的方法,并讨论了用于防止氧同位素交换的技术。描述的其他实验技术包括也可以使样品定向的大立体角α粒子检测器装置,可阻止质子向后散射并保持α粒子分辨率的渐变厚度箔片以及最小化和校正硼背景的方法,通过反应11B(p,α)8Be *发生。

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    《Journal of Applied Physics》 |1973年第10期|共11页
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  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
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  • 正文语种 eng
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