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Numerical modeling of bentonite extrusion and radionuclide migration in a saturated planar fracture

机译:饱和平面裂缝中膨润土挤压和放射性核素迁移的数值模拟

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A case study of limited scope is presented in order to assess the potential of the performance of the engineered barrier in terms of the effects of bentonite extrusion on radionuclide transport in a water-saturated planar fracture. Under saturated conditions, bulk bentonite in the engineered barrier system will swell when contacted by groundwater. Due to this swelling, the bentonite will extrude into the intersecting fracture. A coupled mathematical model that describes the mass conservation of radionuclides in the fracture and the extrusion of bentonite into the fracture is established. The model for radionuclide migration incorporates spatial and temporal change in fluid porosity in the extrusion region due to movement of solid particles in the intersecting fracture. Finite element solutions have been derived for the fluid porosity in the bentonite extrusion region and the radionuclide concentration in the fracture. Numerical simulations of this model produced spatial distributions for radionuclide concentration. Results indicate that with sufficiently strong sorption, the radionuclide is observed to be confined within the region of bentonite extrusion. These results imply that the performance of the engineered barrier to limit radionuclide release is potentially enhanced and warrant more rigorous modeling studies of this phenomenon.
机译:提出了一个范围有限的案例研究,以评估膨润土挤压对水饱和的平面裂缝中放射性核素迁移的影响,从而对工程屏障的性能进行了评估。在饱和条件下,工程隔离系统中的膨润土在与地下水接触时会膨胀。由于这种膨胀,膨润土将挤入相交的裂缝中。建立了耦合数学模型,该模型描述了裂缝中放射性核素的质量守恒和膨润土向裂缝中的挤出。放射性核素迁移模型考虑了固体颗粒在相交裂缝中的运动,从而在挤出区域吸收了流体孔隙度的时空变化。对于膨润土挤出区域的流体孔隙率和裂缝中的放射性核素浓度,已经导出了有限元解决方案。该模型的数值模拟产生了放射性核素浓度的空间分布。结果表明,在足够强的吸附下,观察到放射性核素被限制在膨润土挤压区域内。这些结果表明,工程隔离层限制放射性核素释放的性能可能得到增强,并且需要对此现象进行更严格的建模研究。

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