A new method for evaluating radionuclide migration in groundwater

Sheng-yang Feng, Xiaojie Chen, Yourui Jiang, Hao Tang
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Abstract

The purpose of this study is to propose a new method for evaluating the migration of nuclides of uranium tailings paste backfill in groundwater. Uranium tailings reservoir is a significant threat to the nearby environment and the health of residents. Filling the uranium tailings paste backfill into the mine goaf can effectively reduce the impact of uranium tailings on the surrounding environment. However, there is still a lack of effective methods to evaluate the effect of radionuclides in uranium tailings paste backfill on groundwater. Uranium tailings paste backfill was made from the samples collected from a uranium tailings reservoir, and leaching experiments were carried out to obtain a variation curve of uranium concentration. The fractal parameters of rock fractures are obtained from the goaf of a gypsum mine exploration. The discrete fracture network model (DFN) of underground rock mass in the goaf is established according to the fractal parameters. When the results of leaching experiments are introduced into the numerical simulation model, it is found that when the local water is in the flow state, the flow direction of uranium is consistent with that of groundwater and is related to fractures.
地下水中放射性核素迁移评价的新方法
本研究旨在提出一种评价铀尾矿膏体充填体核素在地下水中迁移的新方法。铀尾矿库对周边环境和居民健康构成重大威胁。在矿山采空区充填铀尾矿膏体,可有效降低铀尾矿对周围环境的影响。然而,目前还缺乏有效的方法来评价铀尾矿膏体充填体中放射性核素对地下水的影响。对某铀矿尾矿库样品进行了铀尾矿膏体充填,并进行了浸出试验,得到了铀浓度的变化曲线。以某石膏矿采空区为研究对象,获得了岩石裂隙的分形参数。根据分形参数,建立了采空区地下岩体的离散裂隙网络模型。将浸出实验结果引入数值模拟模型,发现局部水处于流动状态时,铀的流动方向与地下水的流动方向一致,且与裂隙有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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