Thur

From REFORM wiki
Revision as of 17:34, 8 January 2010 by Admin (Talk | contribs)

Jump to: navigation, search

Thur


Factsheet: Thur

General
Country CH
River Name Thur
Site Name Thur
River Characterisation
{{{rivertypes}}}
River typology
Location (Lat Lon) 47.5919253276985, 8.76691818237305
Altitude high: > 800 m
Catchment area large: > 1000 - 10000 km2
Geology Calcareous
National code/
River type name
XXX

Biological quality elements
{{{bqe}}}
Ecosystem Services
{{{egands}}}
EU Directives
{{{eedandp}}}
Pressures
Morphological alterations
Channelisation/Cross section alteration
Measures
Working with physical form and function of river and floodplains
River bed raising or lowering
Structural modifications
Construction of new structures
Modify/replace existing structures
Changes in system operation
Appropriate vegetation management plan
Other
Project size 1 km2
Approximate costs 0
Synergy Flood control
Status Realised
Period of realization 1999
Evaluation Yes


Attention:The information presented below has been reproduced from the ECRR brochure[1].


The Thur river is one of the main rivers in the Cantons St. Gallen, Thurgau and Zürich in Switzerland. It has a lenght of 127 km and a catchment area of 1,750 km2 with about 456 creeks and brooks. The highest point is the summit of Säntis at 2,551 masl. The 100 years flow is estimated at 1,350 m3/s, the lowest runoff is 2,24 m3/s, and the average flow is 47 m3/s. The Thur is a wild river with no lake or dam or big floodplain for retention.

The first flood control works were constructed in the second half of the 19th century. Today, the ancient dikes and other measures applied in the late 19th century no longer adequately cope with modern discharge conditions, mainly due to insufficient heights, inappropriate construction materials, and poor maintenance. The river bed has been filled with sediment deposits, limiting discharge capacity and increasing flood peaks, while the increased human occupation of the valley in some places limits the extent of the floodplain and interferes with surface roughness (trees) in others.

After the catastrophic flooding due to the breaking of the dikes in 1978, urgent response measures included the repairing and heightening of the dikes and the removal of surface layer sediments from the confined stream bed. The increased attention paid to ecological aspects in later years resulted in a removal of the old stonewall parallel to the stream bed, while groynes were build in combination with obliquely placed blocks and willow trees.

Widening of the Thur river, Switzerland

The resulting variety of river works provide both protection while allowing the river a greater freedom to spread and move. Over a length of 1,500 m and a width of 500 m the Thur river now can redevelop its natural course, in which erosion and sediment deposition processes freely alternate. Scours and rapids as well as wandering gravel beds have once again become a part of the river. This new design of the river was successfully tested by the flood of 1999 (Q 1,000m3/s), in which only a few blocks were moved downstream, and no extensive repairing appeared necessary.

The river restoration works also proved a great success for the ecological state of the Thur river. Fish species like the Chondrostoma nasus and bird species like the Actitis hypoleucos found new habitats within the new river landscape.

The experiences with the river restoration project of the Thur river provide important perceptions for further projects on other rivers. More space for rivers gives opportunities to restore natural wild flora and fauna. Besides, the character of the river changes from a dull canal to a diversified river environment, offering opportunities for tourism and recreation. The Thur river restoration project shows that flood control by means of nature friendly technical river works not necessarily oppose nature conservation interests.

References:

  1. ECRR brochure (click here for online source) ISBN 12-2345-5556