Articles | Volume 28, issue 7
https://doi.org/10.5194/hess-28-1751-2024
https://doi.org/10.5194/hess-28-1751-2024
Research article
 | 
16 Apr 2024
Research article |  | 16 Apr 2024

Influence of bank slope on sinuosity-driven hyporheic exchange flow and residence time distribution during a dynamic flood event

Yiming Li, Uwe Schneidewind, Zhang Wen, Stefan Krause, and Hui Liu

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Latest update: 08 Nov 2024
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Short summary
Meandering rivers are an integral part of many landscapes around the world. Here we used a new modeling approach to look at how the slope of riverbanks influences water flow and solute transport from a meandering river channel through its bank and into/out of the connected groundwater compartment (aquifer). We found that the bank slope can be a significant factor to be considered, especially when bank slope angles are small, and riverbank and aquifer conditions only allow for slow water flow.