Articles | Volume 6, issue 1
Earth Surf. Dynam., 6, 187–201, 2018
https://doi.org/10.5194/esurf-6-187-2018
Earth Surf. Dynam., 6, 187–201, 2018
https://doi.org/10.5194/esurf-6-187-2018

Research article 07 Mar 2018

Research article | 07 Mar 2018

Establishing a sediment budget in the newly created “Kleine Noordwaard” wetland area in the Rhine–Meuse delta

Eveline Christien van der Deijl et al.

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Actueel Hoogtebestand Nederland: Actueel Hoogtebestand Nederland, available at: http://www.ahn.nl/ (last access: October 2016), 2017. a, b
Anderson, C. J. and Mitsch, W. J.: Sediment, carbon, and nutrient accumulation at two 10-year-old created riverine marshes, Wetlands, 26, 779–792, 2006. a, b
Anderson, C. J. and Mitsch, W. J.: Erratum to: Sediment, carbon, and nutrient accumulations at two 10-year-old created riverine marshes, Wetlands, 27, 774–774, 2007. a
Asselman, N. E. M. and Middelkoop, H.: Temporal variability of contemporary floodplain sedimentation in the Rhine-Meuse Delta, the Netherlands, Earth Surf. Proc. Land, 23, 595–609, 1998. a
Asselman, N. E. M. and Van Wijngaarden, M.: Development and application of a 1D floodplain sedimentation model for the River Rhine in the Netherlands, J. Hydrol., 268, 127–142, 2002. a
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Short summary
To study the effectiveness of river delta restoration, we used field observations and elevation data to quantify the magnitude and spatial patterns of aggradation and erosion in a restored wetland in the Rhine-Meuse delta. Erosion and aggradation rates decrease over time, but aggradation compensates for sea-level rise and soil subsidence. Channels in the centre had aggraded, whereas the inlet and outlet eroded. Furthermore, sediment is in general uniformly distributed over the intertidal area.