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• W1540386087 abstract "The sedimentary dynamics of a lowland river system can be defined as the whole ofprocesses that involve erosion, transport or deposition of sediment in the system –including the floodplains – on every possible spatial and temporal scale. Thesedimentary dynamics of the river Rhine in the Netherlands have been influenced bymany human activities in the past. A major human intervention has been theembankment around 1300 AD, by which the so far free meandering river wasconfined between dikes. Previous studies analyzed the impact of human interventionsin the period after the embankment. The present study focuses on the sedimentarydynamics of the natural river Rhine. We reconstructed the amount of sedimentationand erosion that is involved with lateral migration of the river, and estimated theresidence time of the sediment on the floodplain. Lateral migration was reconstructedwith a one-dimensional bank erosion model. Lateral migration rates of meander bendswere modeled based on channel parameters (e.g. bend radius, discharge) and bankmaterial, all derived from detailed borehole reconstructions of sub-recent channelbelts from previous studies. Model results will be used to compare the sedimentarydynamics of the natural river Rhine, with dynamics in human-influenced periods, andhence to predict present and future sedimentation and erosion processes. Moreover,results of reworked sediment volumes can be included in existing large-scalesediment budgets of the river Rhine to evaluate the dynamics within these slices" @default.
• W1540386087 created "2016-06-24" @default.
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• W1540386087 date "2011-04-11" @default.
• W1540386087 modified "2023-09-23" @default.
• W1540386087 title "Decadal to century‐scale sediment dynamics in the Rhine delta" @default.
• W1540386087 hasPublicationYear "2011" @default.
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