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The Diffusion of Tc-99 in Beishan Granite-Temperature Effect

机译:Tc-99在北山花岗岩中的扩散-温度效应

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In the safety assessment of a potential site for high-level radioactive wastes (HLW) disposal, the investigation on the geochemical behaviors of key radionuclides with the possibility for releasing from the potential repository is an important aspect. Due to the high mobility of technetium under most repository conditions, lots of research works were performed to investigate the diffusion of technetium in different potential rocks. In spite of these studies, there remains a lack of data addressing temperature effects. In this paper, the diffusion of 99Tc in Beishan granite at temperatures from 25℃ to 55℃ was studied with laboratory small scale diffusion devices. The experimental data were fitted with a finite difference scheme to get the effective diffusion coefficient (De) of . The results indicated that the relationship of De with temperatures could be described as the modified Stokes-Einstein equation, and the formation factor of Beishan granite was constant in the temperature range of 25℃ - 55℃ with the value of (3.91 ± 1.77) × 10-4.
机译:在对高放废物潜在处置场所的安全评估中,对关键放射性核素的地球化学行为以及可能从潜在处置库中释放的可能性进行调查是一个重要方面。由于most在大多数储层条件下具有很高的流动性,因此进行了大量研究工作以研究investigate在不同潜在岩石中的扩散。尽管进行了这些研究,但是仍然缺乏解决温度影响的数据。本文采用实验室小型扩散装置研究了99Tc在北山花岗岩在25℃至55℃温度下的扩散。实验数据采用有限差分方案拟合,得到的有效扩散系数(De)。结果表明,De与温度的关系可以用修正的Stokes-Einstein方程来描述,北山花岗岩的形成因子在25℃〜55℃的温度范围内是恒定的,取值(3.91±1.77)× 10-4。

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