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Intercomparison of reactive transport models applied to UO_2 oxidative dissolution and uranium migration

机译:适用于UO_2氧化溶解和铀迁移的反应性传输模型的比对

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摘要

Oxidative dissolution of uranium dioxide (UO_2) and the subsequent migration of uranium in a subsurface environment and an underground waste disposal have been simulated with reactive transport models. In these systems, hydrogeological and chemical processes are closely entangled and their interdependency has been analyzed in detail, notably with respect to redox reactions, kinetics of mineralogical evolution and hydrodynamic migration of species of interest. Different codes, where among CASTEM, CHEMTRAP and HYTEC, have been used as an intercomparison and verification exercise. Although the agreement between codes is satisfactory, it is shown that the discretization method of the transport equation (i.e. finite elements (FE) versus mixed-hybrid FE and finite differences) and the sequential coupling scheme may lead to systematic discrepancies.
机译:使用反应性运输模型模拟了二氧化铀(UO_2)的氧化溶解以及铀在地下环境中的后续迁移以及地下废物的处置。在这些系统中,水文地质和化学过程紧密地纠缠在一起,并详细分析了它们的相互依赖性,特别是在氧化还原反应,矿物演化动力学和感兴趣物种的水动力迁移方面。在CASTEM,CHEMTRAP和HYTEC中使用了不同的代码作为比对和验证活动。尽管代码之间的一致性令人满意,但是表明传输方程的离散化方法(即有限元(FE)与混合杂交有限元和有限差分)和顺序耦合方案可能导致系统差异。

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