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Coastal Guide on Dune Management |
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The
regeneration of wet slacks and blow outs in the Meijendel and Berkheide
dune areas
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Keywords:
mainland barrier dunes
hydrology
dune dynamics
drinking water recovery
Contact: DZH (Dunewater Company of South Holland), Department
of Communication, telephone +31 70 3577634
Location: Atlantic region, The Netherlands, Meijendel
dune area
Meijendel and Berkheide dunes
The Meijendel and the Berkheide dunes are part of the great barrier
dune system of the Dutch mainland coast, where many parabolic
dunes formed since about 1000 A.D. The dune areas are managed
by the DZH. (Dunewater Company South Holland). The DZH provides
drinking water but also takes responsibility for nature conservation
and recreation. In 1874 the extraction of drinking water in the
Meijendel dunes started. A canal was dug in the dunes to provide
the city of The Hague of drinking water. Between 1880 and 1955
most of the natural dune slacks had dried out as a result of the
lowering of the groundwatertable. With the increasing population,
the amount of extracted water also increased thereby pumping up
brackish water. In 1955 artificial infiltration of river water
started and some dune valleys became wet again. For the production
of drinking water an extensive infrastructure has been created.
One of the features is a stretch of artificial lakes in the middle
of the dune area for the infiltration of the drinking water.
Management
Main functions of the Meijendel dune area are nature conservation,
drinking water recovery, coastal defence and recreation.
With the artificial recharge of the water table in the dunes,
some dune slacks reappeared but the typical vegetation was
only established locally. The infiltration lakes are well spreaded
over the area to maintain the natural dune relief.
In 1990 deep well drilling was introduced. River water is pumped
into deeper soil layers at 40 to 60 m below sealevel and
extracted at the same deep level. This way the upper groundwatertable
is hardly interrupted and wet slacks can develop under natural
circumstances. The area where the hydrology is more or less natural
must be enlarged, so that the characteristic dune forming processes
like blowouts and wet slacks are encouraged. Regeneration measures
in the Meijendel dune area included the removal of infiltration
lakes and the removal of a 25 cm thick sediment layer. The
natural relief has recovered. The blowing of sand on a large scale
is not permitted in the drinking water production zones.
The new management policy aims at small scale blowouts, and recovery
of wet dune slacks by reducing the area where artificial infiltration
is taking place by intensifying the production in a smaller area.
Also the drinking water production and nature values are optimized.
Results
The first results are an increase in valuable plant species in
wet dune slacks. The dune morphology is more natural because
of less restriction. Locally blowouts have developed. The natural
hydrology is restored by regeneration projects.
References:
- Bakker, TH.W.M. & R.N.A. Kramer, Meijendel, a dune area
in a densely populated part of the Netherlands, Coastline 1993-3,
Coastline special (EUCC library code KJd).
- Bakker,TH.W.M., Fifty years of recreational planning in the
Meijendel dunes near The Hague. A short story about cars and
parking places, Coastal Dunes Recreation and Planning, Drees,J.M.
(ed), EUCC Leiden, The Netherlands, 1997 (EUCC library code
DRC 97)
- Jungerius, P.D. & van der Meulen, F., Aeolian dynamics
in relation to vegetation in a blowout complex in the
Meijendel dunes, The Netherlands, Journal of Coastal Conservation
1997-3, pp 63-70, EUCC Leiden (EUCC library code KJC 97a)
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