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Numerical Analysis Of Water And Solute Transport In Variably-saturated Fractured Clayey Till

机译:饱和饱和黏土耕层中水和溶质运移的数值分析

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This study numerically investigates the influence of initial water content and rain intensities on the preferential migration of two fluorescent tracers, Acid Yellow 7 (AY7) and Sulforhodamine B (SB), through variably-saturated fractured clayey till. The simulations are based on the numerical model HydroGeoSphere, which solves 3D variably-saturated flow and solute transport in discretely-fractured porous media. Using detailed knowledge of the matrix, fracture, and biopore properties, the numerical model is calibrated and validated against experimental high-resolution tracer images/data collected under dry and wet soil conditions and for three different rain events. The model could reproduce reasonably well the observed preferential migration of AY7 and SB through the fractured till, although it did not capture the exact depth of migration and the negligible impact of the dead-end biopores in a near-saturated matrix. A sensitivity analysis suggests fast flow mechanisms and dynamic surface coating in the biopores, and the presence of a plough pan in the till.
机译:这项研究数值研究了初始含水量和降雨强度对两种荧光示踪剂酸性黄7(AY7)和磺胺多巴胺B(SB)通过可变饱和裂缝黏土的优先迁移的影响。该模拟基于数值模型HydroGeoSphere,它解决了离散裂缝多孔介质中的3D变饱和流动和溶质运移问题。利用对基质,裂缝和生物孔隙特性的详细了解,针对在干燥和湿润土壤条件下以及针对三种不同降雨事件收集的实验高分辨率示踪图像/数据,对数值模型进行了校准和验证。该模型可以很好地重现观察到的AY7和SB通过裂缝直到发育的优先迁移,尽管它不能捕获精确的迁移深度和在接近饱和的基质中死端生物孔的影响可忽略不计。敏感性分析表明,在生物孔中具有快速的流动机制和动态的表面涂层,并且在耕till中存在犁pan。

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