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Understanding and managing the morphology of branches incising into sand-clay deposits in the Dutch Rhine Delta

International Journal of Sediment Research 2013年第2期28卷 127-138页

作者： Kees SLOFF(C.J.) Ary VAN SPIJK Esther STOUTHAMER Arjan SIEBEN Deltares and Delft University of Technology PO Box 1772600MH Delftthe Netherlands Assis.Prof. Water management Rijkswaterstaat Zuid HollandPO Box 5563000 AN Rotterdamthe Netherlands Senior Advisor Utrecht University Faculty of GeosciencesPO Box 801153508 TCUtrechtthe Netherlands AssisProf. Water management Rijkswaterstaat Center for Water ManagementPO Box 178200 AA Lelystadthe Netherlands Senior Advisor

In the Rhine-Meuse delta in the south-western part of the Netherlands,the morphology of the river branches is highly dependent on the erodibility of the *** processes that were initiated after closure of the Haringvliet estuary branch by a dam(in 1970),caused a strong incision of several connecting *** to the geological evolution of this area the lithology of the subsoil shows large variations in highly erodible sand and poorly erodible peat and clay *** study shows how the geological information can be used to create 3D maps of the erodibility of the sub-soil, and how this information can be used to schematize the sub-soil in computational models for morphological *** incisement of sand patches between areas with poorly erodible bed causes deep scour holes,hence increasing the risk on river-bank instability(flow slides) and damage to constructions such as groynes,quays,tunnels, and *** types of mathematical models,ranging from 1D(SOBEK) to quasi-3D(Delft3D) have been applied to study the future development of the river bed and possible management *** results of these approaches demonstrate that models require inclusion of a layer-bookkeeping approach for sub-soil schematization, non-uniform sediment fractions(sand-mud),tidal and river-discharge boundary conditions,and capacity-reduction transport *** risk-reducing river management it has been shown how the development of the river bed can be addressed on a large scale and small *** instance,the use of sediment feeding and fixation of bed can be proposed for large-scale management,while monitoring and interventions at initiation of erosion can be proposed as response to small-scale developments that exceed predefined intervention levels.

关键词： river morphological modeling river-bed erodibility river management Erosion bed stratigraphy Bank and dike stability Mathematical model

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