Experimental Study at the Reservoir Head of Run-Of-River Hydropower Plants in Gravel Bed Rivers. Part I: Delta Formation at Operation Level
| Autor: | Kevin Reiterer, Christoph Hauer, Thomas Gold, Helmut Habersack, Christine Sindelar |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2020 |
| Předmět: |
Hydrology
Delta lcsh:TD201-500 lcsh:Hydraulic engineering Flood myth business.industry Geography Planning and Development sediment management strategies Sediment Aquatic Science Biochemistry Head (geology) Volumetric flow rate lcsh:Water supply for domestic and industrial purposes lcsh:TC1-978 Environmental science Mean flow sediment mixtures run-of-river hydropower plants business delta formation sediment continuity Sediment transport Hydropower Water Science and Technology |
| Zdroj: | Water, Vol 12, Iss 2035, p 2035 (2020) Water Volume 12 Issue 7 |
| ISSN: | 2073-4441 |
| Popis: | This study concerns scaled physical model tests of the delta formation process at the head of a run-of-river hydropower plant (RoR). It forms part of a larger research project to provide a scientific base for RoR sediment management strategies in medium-sized gravel bed rivers. The physical model consisted of an idealized river having a width of 20 m, a mean slope of 0.005, a mean flow rate of 22 m3/s and a 1-year flood flow of 104 m3/s. The model scale was 1:20. For the experiments, five different grain sizes were used, covering a range of 14 to 120 mm at 1:1 scale. Experiments were carried out under mobile-bed conditions at flow rates which correspond to 50%&ndash 80% of a 1-year flood HQ1. Even at the head of the reservoir, which is least influenced by the backwater effect of the RoR, sediment transport practically ceases for sediment fractions > 14 mm for a flow rate of 0.7 × HQ1. The whole sediment load coming from the undisturbed upstream section accumulates at the head of the reservoir. This delta formation is accompanied by a substantial rise in water levels. A spatio-temporal scheme of the delta formation was derived from the experiments. The study proved that the delta formation increases the flood risk at the head of the reservoir. Conversely, reservoir drawdowns at flood events of high probability may be a promising strategy to enhance sediment connectivity under the specified boundary conditions. |
| Databáze: | OpenAIRE |
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