How Do Fractures Influence Hyporheic Exchange in Sedimentary Rock Riverbeds?

Bedrock rivers represent a hydrogeological environment in which surface water flows along an exposed bedrock surface. Studies of hyporheic exchange have exclusively involved rivers composed of unconsolidated fluvial sediments, leaving a critical knowledge gap. This study evaluates the conditions tha...

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Veröffentlicht in:	Water resources research 2021-07, Vol.57 (7), p.n/a
Hauptverfasser:	Chow, R., Parker, B. L., Steelman, C. M., Thoms, A., Nowak, W.
Format:	Artikel
Sprache:	eng
Schlagworte:	Attenuation Bedforms Bedrock bedrock river Computational fluid dynamics Contaminants dual porosity Evaluation Exchanging Flow velocity Fluid flow Fluvial sedimentation Fluvial sediments fracture connectivity Fractures Geology Hydrodynamics Hydrogeology hyporheic exchange Mathematical models Natural attenuation Porous media Properties Residence time Residence time distribution River beds Riverbeds Rivers Sedimentary rocks Sedimentary structures Sediments Solutes stochastic framework Surface water Trace contaminants Tracers Variability Water flow Water pollution
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