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Modelling interactions between hydrologic dynamics and biogeochemical processes in a riparian wetland of a low-order stream

机译:模拟低序河岸湿地水文动力学与生物地球化学过程之间的相互作用

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Low order streams often show complex, nonlinear relationships between hydrologic conditions in the riparian zone, streamflow generation and the chemical signature of the stream water. Dynamic surface and subsurface flow paths create a mosaic of biogeochemical conditions that affect the transformation and export of solutes. These relationships are explored in a virtual modelling study of a riparian wetland that links an integrated surface-subsurface flow model with a stream tube approach for biogeochemical reactions along individual flow paths. It is shown that the interplay between water table depth and surface micro-topography in the riparian zone results in distinct shifts between surface and subsurface flow dominance and the development of specific surface flow connectivity. Distinct nonlinear relationships between water table depth and stream discharge that reproduce relationships observed in the field were found. Simulated hydrologic dynamics and the resulting flow paths result in biogeochemical patterns in the riparian zone that are congruent with patterns observed in the field.
机译:低阶水流通常在河岸带的水文条件,水流产生和水流化学特征之间表现出复杂的非线性关系。动态的表面和地下流动路径会形成生物地球化学条件的马赛克,从而影响溶质的转化和输出。在对河岸湿地的虚拟建模研究中探索了这些关系,该研究将整合的地表-地下水流模型与流管方法联系起来,以沿着单个流路进行生物地球化学反应。结果表明,沿岸带的地下水位深度与表面微观形貌之间的相互作用导致了表层和地下流动优势之间的明显转移,以及特定表层流动连通性的发展。发现在地下水位深度和溪流流量之间存在明显的非线性关系,这些关系再现了现场观察到的关系。模拟的水文动力学和由此产生的流动路径导致河岸带的生物地球化学模式与野外观察到的模式一致。

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