Difference between revisions of "Drava - Kleblach"
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| + | The Austrian river Drava (in German “Drau”) is part of the Danube catchment. The source of the river is in the Italian municipality Toblach where it continues its flow 264 km along the border between the Central Alps and the Southern Alps and across the Austrian federal states Tyrol and Carinthia. In Osijek (Croatia), the river joins the Danube River after 707 km in total. The site of the restoration project is located near the village of Klebach in Carinthia. At this point the Drava has a discharge basin of roughly 2500 km². The average annual flow of the river near the site is 63m³/s. The river at the site was historically braided with gravel banks in the channel. Until approximately 140 years ago, the Upper Drava was a free flowing, meandering mountain river with numerous braiding stretches due to alluvial cones of the tributaries. In this dynamic river system with its annual floods and high bed load transport, the river course frequently changed. A braiding river - floodplain system with large gravel banks, grey alder, willow wetlands, and wetland meadows characterized the valley. | ||
==Measures selection== | ==Measures selection== | ||
Revision as of 12:14, 12 February 2014
Drava - Kleblach
Key features of the case study
As part of the LIFE Nature project “Restoration of the wetland and riparian area at the Upper Drau River” several measures were implemented at the site of Kleblach. Bank stabilization structures were removed and the river bed was widened. Lateral erosion increased the sediment input and initialized the development of gravel / sand bars and islands. Furthermore the river bed incision decreased. One of the former side arms was reconnected to the river for annual flooding, and a second side arm was widened to a width of 30 m, creating diverse instream structures and increasing aquatic habitat diversity.
Site description
The Austrian river Drava (in German “Drau”) is part of the Danube catchment. The source of the river is in the Italian municipality Toblach where it continues its flow 264 km along the border between the Central Alps and the Southern Alps and across the Austrian federal states Tyrol and Carinthia. In Osijek (Croatia), the river joins the Danube River after 707 km in total. The site of the restoration project is located near the village of Klebach in Carinthia. At this point the Drava has a discharge basin of roughly 2500 km². The average annual flow of the river near the site is 63m³/s. The river at the site was historically braided with gravel banks in the channel. Until approximately 140 years ago, the Upper Drava was a free flowing, meandering mountain river with numerous braiding stretches due to alluvial cones of the tributaries. In this dynamic river system with its annual floods and high bed load transport, the river course frequently changed. A braiding river - floodplain system with large gravel banks, grey alder, willow wetlands, and wetland meadows characterized the valley.
Measures selection
Success criteria
Ecological response
Hydromorphological response
Monitoring before and after implementation of the project
Socio-economic aspects
Contact person within the organization
Extra background information
References
Related Measures
- Increase flood frequency and duration in riparian zones or floodplains
- Link flood reduction with ecological restoration
- Widen water courses
- Remove bank fixation
- Remove or modify in-channel hydraulic structures
- Recreate gravel bar and riffles
- Adjust land use to develop riparian vegetation
- Remove bank fixation
- Lower river banks or floodplains to enlarge inundation and flooding
- Reconnect backwaters and wetlands
- Restore wetlands
Related Pressures
- Hydropeaking
- Hydrological regime modification
- Artificial barriers downstream from the site
- Artificial barriers upstream from the site
- Alteration of instream habitat
- Sand and gravel extraction
- Embankments, levees or dikes
- Loss of vertical connectivity
- Impoundment
- Alteration of riparian vegetation
- Channelisation / cross section alteration
