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Factors influencing subaqueous dunes in the Scheldt Estuary
Authors:Frederic?Francken  author-information"  >  author-information__contact u-icon-before"  >  mailto:f.francken@mumm.ac.be"   title="  f.francken@mumm.ac.be"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author,Stanislas?Wartel,Reg?Parker,Eric?Taverniers
Affiliation:(1) Royal Belgian Institute of Natural Sciences, Management Unit of the North Sea Mathematical Models, Gulledelle 100, 1200 Brussels, Belgium;(2) Royal Belgian Institute of Natural Sciences, Management of the Marine Ecosystem, Sedimentology, Vautierstraat 29, 1000 Brussels, Belgium;(3) Independent Consultant, 3 Curdleigh Lane, Blagdon Hill, Taunton, Somerset, TA3 7SH, UK;(4) Ministry of the Flemish Community, Waterways and Maritime Affairs Administration, Division Maritime Scheldt, Tavernierkaai, Antwerp, Belgium
Abstract:The size (wavelength and height) and the factors influencing the characteristics of subaqueous dunes in the river Scheldt between Antwerp and the Belgian-Dutch border were studied. More than 60 dune clusters (each cluster represented by a mean height and wavelength of mostly 10 to 20 or more observations) were analysed. A very good exponential correlation between dune height and wavelength was observed (r=0.90) which can be described by H mean=0.0321L 0.918. Length/depth ratios vary between 0.2 and 9, height/depth ratios between 0.25 and 0.01. There was no clear relationship between current velocity and dune size, as dunes of various sizes co-exist at the same current velocities. Twenty-two dunes were sampled and show grain sizes (d50) ranging between 0.1 and 0.7 mm. Seven out of eight large scale dune fields were found in sandy and/or hard bottom (gravel, coarse sand and shell fragments) environments, whereas small and medium dunes were found in muddy sand and sandy mud environments.
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