In 2012 verloren we Jean Jacques Peters, voormalig ingenieur van het Waterbouwkundig Laboratorium (1964 tot 1979) en internationaal expert in sedimenttransport, rivierhydraulica en -morfologie. Als eerbetoon aan hem hebben we potamology (http://www.potamology.com/) gecreëerd, een virtueel gedenkarchief dat als doel heeft om zijn manier van denken en morfologische aanpak van rivierproblemen in de wereld in stand te houden en te verspreiden.
Het merendeel van z’n werk hebben we toegankelijk gemaakt via onderstaande zoekinterface.
Mud floc observations in the turbidity maximum zone of the Scheldt estuary during neap tides
Manning, A.J.; Martens, C.; De Mulder, T.; Vanlede, J.; Winterwerp, J.C.; Ganderton, P.; Graham, G.W. (2007). Mud floc observations in the turbidity maximum zone of the Scheldt estuary during neap tides. J. Coast. Res. Spec. Issue 50: 832-836
In: Journal of Coastal Research. Coastal Education and Research Foundation: Fort Lauderdale. ISSN 0749-0208; e-ISSN 1551-5036
Significant changes of sediment concentration and shear can occur within an estuarine turbidity maximum. Prediction of mud transport depends on a good specification of the settling velocity and the mass settling flux. This can only be achieved by using field measurements of floc settling dynamics that can be implemented in sediment transport models. This paper describes flocculation observations conducted during a neap tide in the Lower Scheldt Estuary. The data forms part of the Deurganckdok tidal dock field survey commissioned by the Flemish government. The findings showed that within the turbidity maximum zone the suspended sediment concentration reached 277 mg 1-1 and the floc mass distribution was bi-modal, with 80% of the population comprising macroflocs up to 507 micrometer in diameter. These macroflocs had individual settling velocities ranging from 1 to 11 mm s-1. In the turbidity maximum the macroflocs represented 88% of the floc mass, had a Wsmacro = 3.9 mm s-1 and contributed to 97% to the total settling flux. In contrast, at peak turbulence, the floc mass distribution was now weighted 58%:42% in favour of the smaller microflocs.
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