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The Significance of Carbon 14 in Graphite Reactor Components at End of Generation

机译:石墨反应堆组件中碳14的生成末期的意义

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It is estimated that there are at least 250,000 tonnes of irradiated graphite worldwide that will require eventual disposal. This graphite arises from a number of sources, but principally comprises moderator and structural materials for experimental reactors, production reactors, commercial power reactors and fuel assemblies. In the UK, a significant proportion of its irradiated graphite is classified as Intermediate Level Waste. Such waste is not heat generating but has a radioactive content exceeding 4 GBq per tonne alpha or 12 GBq per tonne beta/gamma activity. While the classification of waste is not consistent across states and proposals by individual states for the management of their graphite waste vary considerably, a common interest is the nature and distribution of its radioactive content. The radionuclides in irradiated graphite presenting the most significant long-term hazard are Carbon 14 (C-14) and Chlorine 36 (Cl-36) with half-lives of 5730 and 301,000 years respectively. For a better understanding of the way in which C-14 is produced, its distribution within irradiated graphite and realistic quantification of activity can potentially lead to improved characterization to validate its status within current or future waste classifications, segregation to reduce Intermediate Level Waste volumes, or treatment to reduce activity enabling re-classification as Low Level Waste. This paper reviews all these issues and then focuses on the significance of C-14. Some findings from a National Nuclear Laboratory study of C-14 levels in carbonaceous deposits and the underlying Magnox reactor graphite are presented to illustrate the need for thorough characterization of the waste material. These results are discussed in the context of aqueous leaching of C-14 from irradiated graphite and potential treatment options to minimize aqueous release. The paper concludes with some broader observations on the significance of C-14 in nuclear reactor graphite components and how these issues should be considered when preparing the lifetime management of new nuclear plant.
机译:据估计,全世界至少有25万吨的辐照石墨需要最终处置。该石墨来自多种来源,但主要包括用于实验反应堆,生产反应堆,商业动力反应堆和燃料组件的减速剂和结构材料。在英国,很大比例的辐照石墨被归类为中级废物。此类废物不是发热的,而是放射性含量超过每吨alpha 4毫克当量或每吨beta /γ活性12 GBq。虽然各州之间的废物分类不一致,并且各个州关于其石墨废物管理的建议相差很大,但共同的兴趣是其放射性含量的性质和分布。辐射石墨中表现出最大的长期危险性的放射性核素是碳14(C-14)和氯36(Cl-36),半衰期分别为5730年和301,000年。为了更好地了解C-14的生产方式,其在辐照石墨中的分布以及对活性的现实量化可能会改善表征,以验证其在当前或将来的废物分类中的状态,进行分类以减少中级废物量,或减少活动的处理方法,从而可以重新分类为低放废物。本文回顾了所有这些问题,然后重点介绍了C-14的重要性。美国国家核实验室对碳质沉积物中C-14含量和潜在的Magnox反应堆石墨的一些研究结果表明,需要彻底表征废物。这些结果在辐照石墨从C-14中水浸出的讨论中,并讨论了将水释放降至最低的潜在处理方法。本文以对C-14在核反应堆石墨组件中的重要性以及在准备新核电站的寿命管理时应如何考虑这些问题的更广泛的观察得出结论。

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