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Coupling Surface Water and Groundwater Flows in a Laboratory Model Using Foam as Artificial Groundwater Material

机译:以泡沫为人工地下水材料的实验室模型中的地表水和地下水流耦合

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A laboratory mock-up of a surface water groundwater system with foam blocks used to replicate a groundwater material was mounted in a tidal basin in the Hydraulics Laboratory at Cardiff University, UK. River flow in the form of a channel was generated, with an oscillating weir at the lower boundary of the system producing tides or controlled water levels. The purpose of the experiment was to investigate the manner in which flow and a conservative tracer interacted between surface and sub-surface flows for simulated riverine and tidal conditions. In these controlled laboratory conditions, results obtained with respect to flows were consistent with the laws governing surface-subsurface flows. In contrast, the conservative tracer could not move through the foam for any meaningful results to be obtained, which was thought to be due to the dominance of surface tension and sorption in the foam pores.
机译:在英国卡迪夫大学水力学实验室的潮汐盆地中安装了带有泡沫块的地表水地下水系统的实验室模型,该泡沫块用于复制地下水材料。产生了河道形式的河水,在系统的下边界有一个振荡堰,产生潮汐或控制水位。该实验的目的是研究模拟河流和潮汐条件下地表水流和地下水流之间的流动和保守示踪剂相互作用的方式。在这些受控的实验室条件下,关于流量获得的结果与支配地表-地下流量的规律一致。相反,保守示踪剂不能在泡沫中移动以获得任何有意义的结果,这被认为是由于表面张力和泡沫孔中吸附的优势所致。

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