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Kinetics of the sorption of 3He by C60 fullerite. The quantum diffusion of 3He and 4He in fullerite

机译:C60富勒石吸附3He的动力学。 3He和4He在富勒石中的量子扩散

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摘要

The kinetics of the sorption and subsequent desorption of gaseous ~3He in a C_(60) fullerite powder has been studied in the temperature range of 2-292 K. The temperature dependences of the diffusion coefficients of ~3He and ~4He impurities in fullerite have been plotted using the measured characteristic times of filling of octahedral and tetrahedral interstices, as well as previous data. These temperature dependences of the diffusion coefficients of ~3He and ~4He impurities in fullerite are qualitatively similar. A decrease in the temperature from 292 to 79 K is accompanied by a decrease in the diffusion coefficients, which corresponds to the dominance of the thermally activated diffusion of helium isotopes in fullerite. A further decrease in the temperature to 8-10 K leads to an increase in the diffusion coefficients by more than an order of magnitude. The diffusion coefficients of ~3He and ~4He are independent of the temperature below 8 K, indicating the tunnel character of the diffusion of helium in C_(60) fullerite. The isotope effect is manifested in the difference between the absolute values of the diffusion coefficients of ~3He and ~4He atoms at the same temperatures.
机译:研究了在2-292 K的温度范围内C_(60)富铝粉中气态〜3He的吸附动力学和随后的解吸动力学。富勒石中〜3He和〜4He杂质扩散系数的温度依赖性为使用测得的八面体和四面体间隙的特征时间以及以前的数据绘制曲线。富勒石中〜3He和〜4He杂质扩散系数的这些温度依赖性在质量上相似。温度从292降低到79 K伴随着扩散系数的降低,这对应于富勒岩中氦同位素的热活化扩散的优势。温度进一步降低至8-10 K会导致扩散系数增加超过一个数量级。 〜3He和〜4He的扩散系数与8 K以下的温度无关,表明C_(60)富勒岩中氦扩散的隧道特性。同位素效应表现为在相同温度下〜3He和〜4He原子的扩散系数的绝对值之差。

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