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Danube Rivers Morphology and Revitalization - DANUBEPARKS

Danube Rivers Morphology and Revitalization - DANUBEPARKS

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Project name:11. Morava River (Slovakia <strong>and</strong> Austria): reconnection of me<strong>and</strong>ersSituation-before/after human impactOriginally a me<strong>and</strong>ering river, more than 90 % of the river course facedintensive river regulation during the 20th century, like dike construction, canalization,<strong>and</strong> elimination of all major me<strong>and</strong>ers.Project summary:Within the project GEF-Biodiversity four cut-off me<strong>and</strong>ers were partlyreconnected to the river between 1993 <strong>and</strong> 1995 (Morava-Rkm 12, 19, 65). The aimwas to increase the flow dynamics in the former anabranches. The bypass-canalsstayed fully active, water inflow to the re-opened me<strong>and</strong>ers was limited by rock dams.Situation after restoration-The expected washout of settled sediments did not occur, <strong>and</strong> the openedme<strong>and</strong>ers suffered severe sedimentation after restoration. The morphology <strong>and</strong> thesediment layer did not develop towards an active me<strong>and</strong>er. Biotic response showedan increase of fish taxa; mainly additional rheophylic species. Invertebrate <strong>and</strong> plantcommunities shifted towards the riverine set of species, but could not be consideredequivalent to those observed in active me<strong>and</strong>ers.Another type of me<strong>and</strong>er re-opening was tried on the Austrian side of MoravaRiver at river-km 18, where the me<strong>and</strong>er was reconnected at the downstream part tothe river which leads to severe sedimentation in the outflow area of the me<strong>and</strong>er.Lessons learntThe results provide evidence that reconnected me<strong>and</strong>ers might beunsustainable if a parallel shortcutting is not blocked. It is one of the only projectswhere full me<strong>and</strong>er bends of lowl<strong>and</strong> rivers have been reconnected <strong>and</strong> the resultinghydromorphologic changes were well-documented (Phare Project Report 1999).58

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