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Thermal conductivity of isotopically enriched ~(28)Si: revisited

机译:同位素富集〜(28)Si的导热系数

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The thermal conductivity of isotopically enriched ~(28)Si (enrichment better than 99.9%) was redetermined independently in three laboratories by high precision experiments on a total of four samples of different shape and degree of isotope enrichment in the range from 5 to 300 K with particular emphasis on the range near room temperature. The results obtained in the different laboratories are in good agreement with each other. They indicate that at room temperature the thermal conductivity of isotopically enriched ~(28)Si exceeds the thermal conductivity of Si with a natural, unmodified isotope mixture by 10 +- 2%. This finding is in disagreement with an earlier report by Ruf et al. At~26 K the thermal conductivity of ~(28)Si reaches a maximum. The maximum value depends on sample shape and the degree of isotope enrichment and exceeds the thermal conductivity of natural Si by a factor of ~8 for a 99.982% ~(28)Si enriched sample. The thermal conductivity of Si with natural isotope composition is consistently found to be ~3% lower than the values recommended in the literature.
机译:在三个实验室中,通过高精度实验,对总共四个形状和同位素富集度范围从5到300 K的四个样品,分别独立地重新确定了同位素富集的〜(28)Si(富集度优于99.9%)的热导率特别强调接近室温的范围。在不同的实验室中获得的结果彼此非常吻合。他们表明,在室温下,富含同位素的〜(28)Si的热导率比具有天然未改性同位素混合物的Si的热导率高10±2%。这一发现与Ruf等人先前的报告不一致。在〜26 K时,〜(28)Si的热导率达到最大值。最大值取决于样品的形状和同位素的富集程度,对于99.982%〜(28)Si富集的样品,其比天然Si的热导率高出约8倍。一直以来发现,具有天然同位素组成的硅的热导率比文献中推荐的值低约3%。

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