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Numerical modeling of radionuclide migration through a borehole disposal site

机译:放射性核素通过钻孔处置场迁移的数值模拟

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摘要

The migration of radionuclides from a borehole repository located about 20 km from the Akwapim fault line which lies in an area of high seismicity was analyzed for some selected radionuclides. In the event of a seismic activity, fractures and faults could be rejuvenated or initiated resulting in container failure leading to the release of radionuclides. A numerical model was solved using a two-dimensional finite element code (Comsol Multiphysics) by taking into account the effect of heterogeneities. Results showed that, the fractured medium created preferential pathways indicating that, fault zones generated potential paths for released radionuclides from a radioactive waste repository. The results obtained showed that variations in hydraulic conductivity as a result of the heterogeneity considered within the domain significantly affected the direction of flow.
机译:对于一些选定的放射性核素,分析了位于距阿克瓦皮姆断层线约20 km的钻孔储层中放射性核素的迁移,该断层线位于高地震活动区。如果发生地震活动,则可能使裂缝和断层恢复活力或引发断裂,从而导致容器失效,从而导致放射性核素释放。考虑到异质性的影响,使用二维有限元代码(Comsol Multiphysics)求解了数值模型。结果表明,破裂的介质创造了优先路径,表明断层带为从放射性废物处置库释放的放射性核素生成了潜在的路径。获得的结果表明,由于在域内考虑的非均质性导致的水力传导率变化显着影响了流向。

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