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Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.

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one publication added to basket [300577]

Macro-tidal beach morphology in relation to nearshore wave conditions and suspended sediment concentrations at Mariakerke, Belgium Brand, E.; Montreuil, A.-L.; Dan, S.; Chen, M. (2018). Macro-tidal beach morphology in relation to nearshore wave conditions and suspended sediment concentrations at Mariakerke, Belgium. Regional Studies in Marine Science 24: 97-106. https://dx.doi.org/10.1016/j.rsma.2018.08.002 In: Regional Studies in Marine Science. Elsevier: Amsterdam. ISSN 2352-4855, meer

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Beschikbaar in	Auteurs
VLIZ: Non-open access 318566 [ aanvragen ]

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Trefwoorden

Earth sciences > Geology > Geomorphology > Coastal morphology > Beach morphology Belgium, Mariakerke [Marine Regions] Marien/Kust

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Auteurs		Top
Brand, E., meer Montreuil, A.-L., meer Dan, S., meer Chen, M., meer

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Abstract

This study relates changes in beach morphology to nearshore hydrodynamics and suspended sediment concentrations using in-situ measurements for a macro-tidal, sandy beach in Belgium. More than 1.5years of data were collected and analysed including wave characteristics, water level, monthly beach morphology, and 6 months of suspended sediment concentrations. The results indicate that the beachgrows when the wave steepness is very small (< 0.010) and it erodes when wave steepness is very large (> 0.018). This trend is opposite for medium wave steepness (0.012–0.016) with beach erosion under small waves and accretion under large waves. An increment of the suspended sediment concentration follows wave steepness when it is medium, which is most likely due to the start of wave breaking over a sandbank in front of the coast. Flood dominant cross-shore currents transport the suspended sediment shoreward resulting in partial compensation of the erosion by waves. A conceptual model is established to demonstrate the relation between waves, suspended sediment supply, and morphological change. It shows that the morphodynamics of macro-tidal beaches is not only controlled by wave conditions, but also by the currents and sediment supply.

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