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Tidal wetland restoration at Ketenisse polder (Schelde Estuary, Belgium): developments in the first year
Van den Bergh, E.; Vandevoorde, B.; Verbessem, I.; Spanoghe, G.; Lionard, M.; Muylaert, K.; De Regge, N.; Soors, J.; De Belder, W.; Piesschaert, F.; Meire, P. (2005). Tidal wetland restoration at Ketenisse polder (Schelde Estuary, Belgium): developments in the first year, in: Herrier, J.-L. et al. (Ed.) (2005). Proceedings 'Dunes and Estuaries 2005': International Conference on nature restoration practices in European coastal habitats, Koksijde, Belgium 19-23 September 2005. VLIZ Special Publication, 19: pp. 521-533
In: Herrier, J.-L. et al. (Ed.) (2005). Proceedings 'Dunes and Estuaries 2005': International Conference on nature restoration practices in European coastal habitats, Koksijde, Belgium 19-23 September 2005. VLIZ Special Publication, 19. Vlaams Instituut voor de Zee (VLIZ): Oostende. XIV, 685 pp., meer
In: VLIZ Special Publication. Vlaams Instituut voor de Zee (VLIZ): Oostende. ISSN 1377-0950

Beschikbaar in Auteurs | Datasets 
  • Vlaams Instituut voor de Zee: VLIZ Publications [73867] [ aanvragen ]
  • Vlaams Instituut voor de Zee: Open access 73869 [ download pdf ]
Documenttype: Congresbijdrage

Trefwoorden

Auteurs  Top | Datasets 
  • Van den Bergh, E.
  • Vandevoorde, B.
  • Verbessem, I.
  • Spanoghe, G.
  • Lionard, M.
  • Muylaert, K.
  • De Regge, N.
  • Soors, J.
  • De Belder, W.
  • Piesschaert, F.
  • Meire, P.

Abstract
    Ketenisse polder is a former intertidal brackish marsh (30ha) situated in the mesohaline part of the Schelde Estuary. In the 19th century its central part was embanked as a polder. In the mid 1980’s the area was raised above intertidal level when it was used as a dumping site for the excavated soil from the Liefkenshoek tunnel. In 2002 the area was restored, it was levelled with a weak slope below mean high water level, creating the optimal starting conditions for the development of intertidal mudflats and marshes. Geomorphological changes, sediment characteristics and colonisation by phytobenthos, vegetation, zoobenthos, water birds and breeding birds at the restored site are monitored. The monitoring results of the first year after tidal restoration are presented. Sedimentation as well as erosion between 0 and 30cm was observed in the first year. Local changes in stream current patterns caused erosion on parts of the former mudflats; sheltered depressions filled up relatively fast. Median grain size showed large variation. Organic carbon content of the sediment varied between 0.5 and 15% and was closely related to sediment medium grain size. Chlorophyll a concentrations were negatively correlated with median grain size and tended to increase from the low water line to the shore. They were comparable to nearby intertidal areas and displayed similar seasonal variability with a maximum in spring. The large surface covered wtithVaucheria was indicator of initiated succession towards tidal marsh. Scirpus maritimus and transitional vegetations to Chenopodiaceae-vegetations established with increasing altitude. The Chenopodiaceae-vegetations were relicts of earlier vegetations before the tidal restoration, and will probably disappear. The macrobenthos community was dominated by Oligochaetes, which were present in 73% of all samples and attained an average density of about 40*103 ind. m-2. Other macrobenthos species found were nematods, copepods and Corophium. On the sheltered sampling stations macrobenthic densities were high compared to those on nearby intertidal areas. In the first season, 15 breeding bird species were recorded, the most common species being the Pied Avocet (Recurvirostra avosetta). The most common waterbirds were Common Shelduck (Tadorna tadorna), Greylag Goose (Anser anser), Pied Avocet (Recurvirostra avoset) and Lapwing (Vanellus vanellus), typical species for the mesohaline part of the estuary. The first year’s results suggest that Ketenisse polder has the potential to develop towards a varied and normal functional intertidal area.

Datasets (2)
  • MNO Monitoring Waaslandhaven
  • MNO Opvolging evoluties na de afgraving van de Ketenissepolder tot slik- en schorgebied in 2002

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