Non‐Darcy Flow Through a Natural Streambed in a Disconnected Stream

Seepage flux from disconnected streams can be a main source of groundwater recharge in arid and semiarid regions. The seepage into the streambed will respond to a change in stream stage; however, the relationship between seepage flux and stream stage is uncertain due to a lack of in situ observation...

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Veröffentlicht in:	Water resources research 2022-03, Vol.58 (3), p.n/a
Hauptverfasser:	Ma, Zhitong, Wang, Wenke, Zhao, Ming, Hou, Xinyue, Wang, Zhan, Zheng, Haochang
Format:	Artikel
Sprache:	eng
Schlagworte:	Arid regions critical criterion Diameters Evaluation flow regime Fluid flow Fluxes Groundwater Groundwater recharge Intermittent streams natural streambed non‐Darcy seepage model Particle size Porosity Regional development Reynolds number Rivers Seepage Semi arid areas Semiarid zones Streambeds Surface water Surface-groundwater relations
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