Abstract
In 1987, the Scheldt estuary was sampled during winter and spring to study the behaviour of Cd, Cu and Zn. The results show that seasonal mechanisms control the behaviour of trace metals.
During spring the river water entering the estuary is anoxic. The low concentration of dissolved trace metals in the fresh water is caused by precipitation of metal sulphides. After estuarine mixing, oxidation of these compounds leads to apparent desorption of Cd, Cu and Zn. In the lower estuary, phytoplankton blooms cause subsequent removal of dissolved Cd and Zn.
During winter, dissolved Cu and Zn concentrations in the fresh water entering the estuary are high since the river water is not completely anoxic. The existence of a turbidity maximum in the low salinity region causes rapid removal of dissolved Cu and Zn during the very first stages of estuarine mixing. Several mechanisms (oxidation of metal sulphides, desorption induced by chloride complexation, resuspension of reduced bottom sediments) can explain the subsequent increase of dissolved metal concentrations in the lower estuary.
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Zwolsman, J.J.G., van Eck, G.T.M. (1990). The Behaviour of Dissolved Cd, Cu and Zn in the Scheldt Estuary. In: Michaelis, W. (eds) Estuarine Water Quality Management. Coastal and Estuarine Studies, vol 36. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-75413-5_61
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DOI: https://doi.org/10.1007/978-3-642-75413-5_61
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