Case study:Herinrichting beekdal Tongelreep: Difference between revisions
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|Contact organisation url=www.stowa.nl/contact | |Contact organisation url=www.stowa.nl/contact | ||
|Multi-site=No | |Multi-site=No | ||
|Project summary= | |Project summary=The Tongelreep enters the Netherlands at the Achelse Kluis and then flows into the river Dommel near Eindhoven. The Tongelreep is part of the Dommel catchment. Since the 1990s, stream restoration measures were taken to allow the river more space to meander after it had previously, in the past century, been straightened for a faster discharges. As a result of this straightening, parts of woodland, moors and wetlands were at risk of drying out. In addition to these traditional restoration measures, Building with Nature measure were implemented. The Tongelreep is the only Dutch stream where, for building with Nature purposes, gravel beds were introduced near Aalst in addition to dead wood patches. This was done to enrich the stream flora and fauna. | ||
|Monitoring surveys and results=Water depth, flow velocity and substrate cover were measured four times in 2016/2017. In addition, the position of the gravel beds was measured twice per year in the years 2015, 2016 and 2017. These measurements also revealed limited sedimentation, which was 80% gravel in late 2017. The gravel areas moved by on average 1.0m (+/- 0.3m), indicating that they mostly remained in place over a five year period. After the introduction of gravel beds, total species abundance and the number of species typical for an R5-type stream both increased significantly. | |||
|Monitoring surveys and results= | |||
Source: http://edepot.wur.nl/468347 | |||
|Lessons learn= | |Lessons learn=These measurements show the potential of stimulating the origination of gravel beds. Actively introducing gravel would be a technological approach, which may be undesirable. If gravel is already naturally present in the stream, extra gravel may be added, but otherwise, a Building with Nature approach is considered more desirable. | ||
Flow velocity variation can also be stimulated by main channel mowing or by introducing dead wood. When there is insufficient space for these natural measures, (as is the case for the Tongelreep), introducing gravel is an option. Providing sufficient shade over the gravel area is important. | |||
|Project title=Herinrichting beekdal Tongelreep | |Project title=Herinrichting beekdal Tongelreep | ||
}} | }} |
Latest revision as of 13:03, 1 April 2021
Project overview
Status | Complete |
---|---|
Project web site | http://rhk.maps.arcgis.com/apps/MapSeries/index.html?appid=b9cf56c10d7f4d1db891cecec33d1d96 |
Themes | Environmental flows and water resources, Fisheries, Habitat and biodiversity, Hydromorphology |
Country | Netherlands |
Main contact forename | Ineke |
Main contact surname | Barten |
Main contact user ID | |
Contact organisation | STOWA |
Contact organisation web site | http://www.stowa.nl/contact |
Partner organisations | |
Parent multi-site project | |
This is a parent project encompassing the following projects |
No |
Project summary
The Tongelreep enters the Netherlands at the Achelse Kluis and then flows into the river Dommel near Eindhoven. The Tongelreep is part of the Dommel catchment. Since the 1990s, stream restoration measures were taken to allow the river more space to meander after it had previously, in the past century, been straightened for a faster discharges. As a result of this straightening, parts of woodland, moors and wetlands were at risk of drying out. In addition to these traditional restoration measures, Building with Nature measure were implemented. The Tongelreep is the only Dutch stream where, for building with Nature purposes, gravel beds were introduced near Aalst in addition to dead wood patches. This was done to enrich the stream flora and fauna.
Monitoring surveys and results
Water depth, flow velocity and substrate cover were measured four times in 2016/2017. In addition, the position of the gravel beds was measured twice per year in the years 2015, 2016 and 2017. These measurements also revealed limited sedimentation, which was 80% gravel in late 2017. The gravel areas moved by on average 1.0m (+/- 0.3m), indicating that they mostly remained in place over a five year period. After the introduction of gravel beds, total species abundance and the number of species typical for an R5-type stream both increased significantly.
Source: http://edepot.wur.nl/468347
Lessons learnt
These measurements show the potential of stimulating the origination of gravel beds. Actively introducing gravel would be a technological approach, which may be undesirable. If gravel is already naturally present in the stream, extra gravel may be added, but otherwise, a Building with Nature approach is considered more desirable.
Flow velocity variation can also be stimulated by main channel mowing or by introducing dead wood. When there is insufficient space for these natural measures, (as is the case for the Tongelreep), introducing gravel is an option. Providing sufficient shade over the gravel area is important.
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Other case studies in this subcatchment: Beekherstel Beekloop BmN, Beekherstel Keersop, Beekherstel Reusel Baarschot-Diessen, Boven-Dommel, Buulder Aa, Grote Aa, Kleine Aa, traject Smalwater Noord, Kleine Beerze
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MonitoringHydromorphological quality elements
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