Biodiversity
 

 

Terschelling
 
A digital terrain model for the restoration of a foredune area on Terschelling, Dutch Wadden Sea
Recreation management by zoning on Terschelling, Dutch Wadden Sea
Shoreface nourishment on Terschelling, Dutch Wadden Sea

 

 

 

 

 

 

 

 

 

 
Coastal Guide on Dune Management 
 

Shoreface nourishment on Terschelling, Dutch Wadden Sea


Keywords:
island barrier dune
shoreface nourishment
NOURTEC project
RIACON project
food web
zoobenthos

Location:  The Netherlands, Province of Friesland, Terschelling

The Wadden Sea island Terschelling
Terschelling is a barrier island situated in the Dutch Wadden Sea. It is about 30 km long and 3 to 4 km wide. Dune forming processes of this island began some 2000 years ago. The island is rich in contrasts and compared to the mainland it is influenced by a ‘specific’ climate with features from the North as well as from the South. The high biodiversity with both species normally occuring more northern and southern is due to this phenomenon. The island has national as well as international significance.

The NOURTEC and the RIACON project
The project NOURTEC (Innovative Nourishment Techniques Evaluation) is part of the MAST-II program of the EU. The effectiveness of shoreface nourishment as an alternative for beach nourishment and its relevant physical processes have been studied between May 1993 and December 1996 on different sites of the Wadden Sea area in Denmark (Torsminde, 1993), Germany (Norderney, 1992) and The Netherlands (Terschelling, 1993).
To evaluate the risk of shoreface nourishment and subaqueous sand extraction for the marine benthic community and its effect on its consumers higher up in the foodweb, an additional project was launched in 1994, the RIACON (Risk Assessment of Coastal Nourishment Techniques). Five sites along the European coastline in Belgium, Denmark, Germany, Spain and The Netherlands (Terschelling) were investigated for two years.

Nourishment on Terschelling
The objective of the Terschelling nourishment was to prevent for a period of 8 years the retreat in a 4.5 km long stretch of the coastline in the center of the island. Most of the 2 million m³  of sand (taken from 21-22 m depth approx. 7 km NW of the nourishment site) was dumped in the trough between two breaker bars. The dumped sand had similar grain sizes as the native sand, it was only slightly coarser (D50 = 200 µm and 180 µm respectively). Coastal profiles have been measured each year since 1965 with echosounding and beach levelling.

Results
It is necessary to define beforehand clear objectives and design parameters of a shoreface nourishment which can be evaluated quantitatively later. From 1965 till the nourishment the mean coastline position has shown a gradual retreat of a few meters per year. The nourishment was supposed to compensate the natural losses of 8 years (approximately 20 m). However, the result shows a much greater gain, already 30 m at the end of 1996, which still increases. The nourishment acts as a submerged breakwater trapping sand. Further advantages that may offer the shoreface nourishment are reduced costs (since some handling and the installation of, e.g. pipelines, are avoided), while any ongoing recreation is no longer hindered. So far, the experiment is declared a great success.
With respect to the ecological effects, shoreface nourishment initially caused a reduction in species diversity, abundance and biomass of zoobenthic species on the nourishment site. Also the structure of the zoobenthic community differed but approximately one year after the nourishment recovery was already in progress. After two years densities, biomass and diversity had largely regained pre-nourishment values. However, this is not due for long-living bivalve and sea urchin species. After 2 years the population structure was still unbalanced due to the absence of older year classes. The risks for fishes in food webs are expected to be relatively small. But populations of diving ducks are likely to be affected during their winter stay in the North Sea, when nourishment takes place on beds of their favorite bivalve food species.
On the extraction site, the measure significantly reduced species abundance and biomass. The sediment disturbance was followed by the development of spionid polychaetes (Spio filicornis and Spiophanes bombyx). The recovery of the original benthic fauna proceeded within one year. As on the nourishment site, this is not due to long-living bivalve and sea urchin species. The danger with respect to food webs is considered to be small because of the fast recovery of the benthic fauna and the depth of the sites, which makes them to less preferred food areas for diving ducks.

References:

  • Essink, K. (1996): Risk Assessment of Coastal Nourishment Techniques – RIACON. Wadden Sea Newsletter 1: 10-12. (18.1.3.1).
  • Essink, K. & J.A. van Dalfsen (1998): The RIACON Project. Wadden Sea Newsletter 1 (18.8).
  • Hillen, R. & J. de Ruig (1995): Dynamic Preservation on the Wadden Islands of The Netherlands. Wadden Sea Newsletter 1: 15-18. (18.1.3.1).
  • Spanhoff, R. (1998): Success of the Shoreface Nourishment at Terschelling. Wadden Sea Newsletter 1 (18.8).

 


 
 

 

 

 
 
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Each case can be found via geographical maps and via thematical texts putting the cases in an order of six interesting topics:
seashore dynamics
sand mobility
hydrology and water management
conservation management
management of forests
management in relation to recreation and tourism