Idealized Model for the Deflection of Sediment Into Lateral Branches of Lowland Rivers. Issue 6 (5th June 2020)

• Record Type: Journal Article
• Authors: Kästner, K.; Hoitink, A. J. F.
• Is Part Of: Water resources research. Volume 56:Issue 6(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-06-05
• Subjects: bifurcation -- sediment diversion -- river -- secondary flow -- idealized model -- potential flow; Hydrology -- Periodicals; 333.91
• DOI: 10.1029/2019WR026602
• Languages: English
• ISSNs: 0043-1397

Abstract

Abstract: The division of sediment at river bifurcations is crucial for the morphodynamics of anastamosing rivers and distributary delta channel networks. Many river bifurcations are strongly asymmetric and have a planform where a small channel branches off to the side. Such a configuration is also typical for man‐made diversions of water and sediment into canals. At asymmetric bifurcations, the division of sediment is influenced by the secondary current, which is caused by the turning of the flow toward the side. The secondary currents cause especially water from the lower parts of the water column to be diverted into the side branch. As the sediment concentration close to the bottom is high, side branches can receive a disproportionately large fraction of the incoming sediment load, relative to the water discharge. Lateral diversions have been extensively studied with physical and numerical experiments, with the goal to either mitigate or exploit this effect. However, a systematic mathematical analysis of the parameter space has not yet appeared in the literature. Here, we present a comprehensive analysis by way of an idealized model, revealing how the division of sediment is influenced by the width and depth of the branches. We show that the excess of sediment that is diverted into the side branch is lower when the inlet to the side branch is wider and shallower. This may have larger implications for the stability of delta channel networks, as inlets to side branches tend to be locally wider, which likely contributes to their morphological stability. Key Points: Diversion of sediment into a lateral branch of a lowland river is strongly influenced by the local size and aspect ratio at the inlet The excess amount of diverted sediment decreases with the local cross‐section area and depth at the inlet Local inlet morphodynamics likely influences the regional evolution of fluvial channel networks