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Isothermal diffusion coefficient measurements of antimony doped molten germanium using the modified shear cell technique.

机译:使用改进的剪切池技术测量锑掺杂的熔融锗的等温扩散系数。

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摘要

A comparative study on the effectiveness of two different methods to reduce buoyancy driven convection to obtain an intrinsic diffusion coefficient was investigated. Both methods used the shear cell technique and antimony doped molten germanium. In the first method, the effectiveness of microgravity was investigated. In the second method, a ground-based isothermal heat pipe furnace system was used to reduce the thermal gradients. The effect of capillary size was also investigated using four capillary diameters (3.0 mm, 2.0 mm, 1.5 mm and 1.0 mm).; The antimony concentration in the solidified capillaries was characterized using Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) and a measured diffusion coefficient (Dmeasured) was determined using the long-time solution to Fick's 2nd Law. The data obtained was extrapolated to a ‘zero diameter’ capillary to yield an intrinsic diffusion coefficient (Dintrinsic).; The microgravity experiments returned a Dmeasured value for the two 3.0 mm capillaries of (5.0878 ± 0.4687) × 10−4 cm2/s and (5.6472 ± 0.5948) × 10 −4 cm2/s, with a value of (3.6911 ± 0.2563) × 10−4 cm2/s for the 1.5 mm capillary. Because of the capillary diameter dependence on Dmeasured, it was concluded that the microgravity results were contaminated with convection.; The Dintrinsic value for Sb-doped molten Ge at 1000°C was found to be (1.2230 ± 0.0624) × 10−4 cm2/s. It was found that there was no influence of capillary size. This implies that there was no contribution from buoyancy driven convection for the ground-based isothermal furnace results.; This Dintrinsic value was extrapolated to 938°C using (1) the Stokes-Einstein equation and (2) the Arrhenius equation. For the Stokes-Einstein equation: D(938) = 0.9670 × 10 −4 cm2/s. For the Arrhenius equation: D (938) = 1.0334 × 10−4 cm2/s with a range of (1.0242 to 1.0470) × 10−4 cm 2/s.; The extrapolated diffusion coefficient values was compared to the recalculated mean value of 0.522 × 10−4 cm2/s with a range of 0.240 to 0.693 × 10−4 cm 2/s reported by Burton et al. Thus, the isothermal furnace measurements were slightly above this, however, the extrapolated Dintrinsic value at 1000°C was more precise.
机译:对两种不同方法降低浮力驱动对流以获得固有扩散系数的有效性进行了比较研究。两种方法都使用剪切池技术和锑掺杂的熔融锗。在第一种方法中,研究了微重力的有效性。在第二种方法中,使用了基于地面的等温热管炉系统来减小热梯度。还使用四种毛细管直径(3.0 mm,2.0 mm,1.5 mm和1.0 mm)研究了毛细管尺寸的影响。使用电感耦合等离子体质谱法(ICP-MS)对凝固的毛细管中的锑浓度进行表征,并使用针对Fick's 2 measured ) > nd 法。所获得的数据外推至“零直径”毛细管,以产生固有扩散系数(D intrinsic )。微重力实验返回了两个3.0 mm毛细管(5.0878±0.4687)×10 -4 cm 2 / s的D 测量值,并且(5.6472±0.5948)×10 -4 cm 2 / s,值(3.6911±0.2563)×10 −4 cm <对于1.5 mm毛细管,super> 2 / s。由于毛细管直径对D 测量的的依赖性,因此得出结论,微重力结果被对流污染。发现掺Sb的熔融Ge在1000°C时的D 本征值为(1.2230±0.0624)×10 -4 cm 2 / s。发现没有毛细管尺寸的影响。这意味着浮力驱动的对流对地面等温炉的结果没有贡献。使用(1)Stokes-Einstein方程和(2)Arrhenius方程将该D 固有值外推至938°C。对于Stokes-Einstein方程:D (938) = 0.9670×10 -4 cm 2 / s。对于Arrhenius方程:D (938) = 1.0334×10 −4 cm 2 / s,范围(1.0242至1.0470)× 10 −4 cm 2 /秒。将外推扩散系数值与重新计算的平均值0.522×10 -4 cm 2 / s进行比较,范围为0.240至0.693×10 -4伯顿 et al 报告的 cm 2 / s。因此,等温炉的测量值略高于此值,但是外推的D 固有值在1000°C时更为精确。

著录项

  • 作者

    Keefer, Lara Ann.;

  • 作者单位

    Case Western Reserve University.;

  • 授予单位 Case Western Reserve University.;
  • 学科 Engineering Materials Science.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 206 p.
  • 总页数 206
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 工程材料学;
  • 关键词

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