Blueprint for a coupled model of sedimentology, hydrology, and hydrogeology in streambeds. (11th April 2017)

• Record Type: Journal Article
• Authors: Partington, Daniel; Therrien, Rene; Simmons, Craig T.; Brunner, Philip
• Is Part Of: Reviews of geophysics. Volume 55:Number 2(2017)
• Page Start: 287
• Page End: 309
• Publication Date: 2017-04-11
• Subjects: hydrology -- sedimentology -- hydrogeology -- surface water‐groundwater interaction -- streambed dynamics -- physically based modeling; Geophysics -- Periodicals; 550.5
• DOI: 10.1002/2016RG000530
• Languages: English
• ISSNs: 8755-1209

Abstract

Abstract: The streambed constitutes the physical interface between the surface and the subsurface of a stream. Across all spatial scales, the physical properties of the streambed control surface water‐groundwater interactions. Continuous alteration of streambed properties such as topography or hydraulic conductivity occurs through erosion and sedimentation processes. Recent studies from the fields of ecology, hydrogeology, and sedimentology provide field evidence that sedimentological processes themselves can be heavily influenced by surface water‐groundwater interactions, giving rise to complex feedback mechanisms between sedimentology, hydrology, and hydrogeology. More explicitly, surface water‐groundwater exchanges play a significant role in the deposition of fine sediments, which in turn modify the hydraulic properties of the streambed. We explore these feedback mechanisms and critically review the extent of current interaction between the different disciplines. We identify opportunities to improve current modeling practices. For example, hydrogeological models treat the streambed as a static rather than a dynamic entity, while sedimentological models do not account for critical catchment processes such as surface water‐groundwater exchange. We propose a blueprint for a new modeling framework that bridges the conceptual gaps between sedimentology, hydrogeology, and hydrology. Specifically, this blueprint (1) fully integrates surface‐subsurface flows with erosion, transport, and deposition of sediments and (2) accounts for the dynamic changes in surface elevation and hydraulic conductivity of the streambed. Finally, we discuss the opportunities for new research within the coupled framework. Key Points: Complex feedback mechanisms exist between sedimentological processes and surface water‐groundwater flow in streams There is currently no quantitative approach that allows exploration of these feedback mechanisms A blueprint of a mathematical model is suggested that allows coupling of sedimentology, hydrology, and hydrogeology in streambeds