4.2 Article

Short time-scale impacts of hydropeaking on benthic invertebrates in an Alpine stream (Trentino, Italy)

Journal

LIMNOLOGICA
Volume 40, Issue 4, Pages 281-290

Publisher

ELSEVIER GMBH
DOI: 10.1016/j.limno.2009.11.012

Keywords

Drift; Invertebrates; Flow regime; Hydropower impacts; Italian Alps

Categories

Funding

  1. Adige River Authority
  2. Natural Science Museum of Trento
  3. Department of Civil and Environmental Engineering of the University of Trento

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The impact of a single hydropeaking event was studied in the Alpine stream Noce Bianco. Four stations were selected, one upstream and three, respectively, at 0.25, 6, and 8 km downstream from a hydropower plant. We collected drifting invertebrates during a planned water release that increased the discharge 7-fold. At the onset of the hydropeaking wave the number of invertebrates lost from the riverbed per minute to the drift increased 9-fold at the first downstream station and the same effects propagated 8 km downstream. The drift was composed mainly of aquatic insect larvae (Chironomidae, Plecoptera, Ephemeroptera Baetidae, and Psychodidae, with Chironomidae as the most abundant taxon at all stations) and partly by larval and adult riparian insects, and by Oligochaeta, which were particularly abundant at the station 6 km downstream. We monitored drift for 30 min from the start of the water release: peaks in drifting invertebrates occurred within 5-10 min of the beginning of the hydropeaking wave, and most of the invertebrates were washed out within the first 15 min of the water release. The different timeframes were possibly due to habitat preferences (most of the taxa that increased in the drift at the arrival of the wave were associated with algae and organic debris, which were washed off quickly by the increase in discharge) and/or behavioral adaptations (other taxa initially resisted the shear stress and began to drift with a delay of 5-10 min). The temporal pattern and drift composition corresponded well with those reported in literature, and indicate that repeated high-flow events of similar magnitude cause considerable losses from benthic populations to drift. (C) 2009 Elsevier GmbH. All rights reserved.

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