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Niesten et al. - 2024 - Publications
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Lithological Control on Scour Hole Formation in the Rhine-Meuse Estuary Geomorphology

YmkjeHuismans, Hilde Koopmans, AneWiersma, Tjalling de Haas, Koen Berends, Kees Sloff, Esther Stouthamer - 16/07/2021
Geomorphology

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Multidecadal Analysis of an Engineered River System Reveals Challenges for Model-Based Design of Human Interventions

Berends KD, Gensen MRA, Warmink JJ, Hulscher SJMH - 14/07/2021 - RiverCare
Models predict water level decrease, but measurements are too uncertain for now. This reveals a challenge for validation model predictions of human intervention

Subsite Publication Publication open access

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Assessing Habitat suitability for native and alien freshwater mussels in the River Waal (the Netherlands), using hydroacoustics and species sensitivity distributions

Flores, N.Y., F.P.L. Collas, K. Mehler, M.M. Schoor, C.K. Feld & R.S.E.W. Leuven - 09/07/2021
Environmental Modeling and Assessment

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Anthropogenic Effects on the Contemporary Sediment Budget of the Lower Rhine‐Meuse Delta Channel Network

01/07/2021 - Rivers2Morrow
In this research, we construct sediment budgets which quantify annual changes for the urbanized Rhine‐Meuse Delta of the Netherlands, a typical urban delta experiences changing fluvial and coastal fluxes of sediment, engineering works and dredging and dumping activities. The delta shows a negative sediment budget (more outgoing than incoming sediment) since the 1980s, due to anthropogenic intervention.

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Antropogene effecten op de hedendaagse sedimentbegroting van het kanaalnetwerk van de Nederrijn-Maasdelta

01/07/2021 - Rivers2Morrow
In this research, we construct sediment budgets which quantify annual changes for the urbanized Rhine‐Meuse Delta of the Netherlands, a typical urban delta experiences changing fluvial and coastal fluxes of sediment, engineering works and dredging and dumping activities. The delta shows a negative sediment budget (more outgoing than incoming sediment) since the 1980s, due to anthropogenic intervention.

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Gravitational Circulation as Driver of Upstream Migration of Estuarine Sand Dunes

W.M. van der Sande, P.C. Roos, T. Gerkema, S.J.M.H. Hulscher - 30/06/2021 - SALTISolutions

Subsite estuarine sand dunes gravitational circulation linear stability analysis migration direction morphodynamic modeling

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Anthropogenic Effects on the Contemporary Sediment Budget of the Lower Rhine-Meuse Delta Channel Network

J. R. Cox, Y. Huismans, S. M. Knaake, J. R. F. W. Leuven, N. E. Vellinga, M. van der Vegt, A. J. F. Hoitink, M. G. Kleinhans - 30/06/2021 - Rivers2Morrow

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Predicting Outflow Hydrographs of Potential Dike Breaches in a Bifurcating River System Using NARX Neural Networks

Anouk Bomers - 16/06/2021

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Anthropogenic effects on the Contemporary Sediment Budget of the Lower Rhine-Meuse Delta Channel Network

J.R. Cox, Y. Huismans, S.M. Knaake, J.R.F.W. Leuven, N.E. Vellinga, M. van der Vegt, A.J.F Hoitink, M.G. Kleinhans - 10/06/2021 - All-Risk
The Rhine-Meuse Delta has a negative budget: Its entire network of channels is losing sediment annually. The reason for this negative budget is the high amounts of sand and mud removed for navigation to inland ports and from harbors which are periodically dredged. A strategy is required to deal with channel degradation and find ways to maintain sediment in the system.

Subsite Publication open access journal

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Anthropogenic effects on the Contemporary Sediment Budget of the Lower Rhine-Meuse Delta Channel Network

J.R. Cox, Y. Huismans, S.M. Knaake, J.R.F.W. Leuven, N.E. Vellinga, M. van der Vegt, A.J.F Hoitink, M.G. Kleinhans - 10/06/2021 - All-Risk
De Rijn-Maasdelta heeft een negatieve balans: Het hele netwerk van kanalen kanalen verliest jaarlijks sediment. De reden voor deze negatieve is te wijten aan de grote hoeveelheden zand en slib die voor de scheepvaart naar binnenhavens en uit havens die periodiek worden gebaggerd. Een strategie is vereist om de aantasting van kanalen aan te pakken en manieren te vinden om de sediment in het systeem te houden.

Subsite Publication open access journal

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