Deformation of river channels in the dam stretch
The construction of small reservoirs leads to a radical change in the natural hydrologic regime of a river, this being expressed mainly in the annual redistribution of the water discharge and partial or complete retention of the sediment load by the reservoir. Scour of river channels in the lower pool, observed during operation of large reservoirs, usually leads to a drop of the water level and bottom, but in certain cases a rise of the bottom and water surface is noted. This was observed in the lower pool of the Volga-Lenin hydroelectric station. The authors present here the results of an investigation of deformations in the dam stretch of small reservoirs of Belorussia, showing that an analogous phenomenon of a rise of the bottom and water surface is observed in almost all cases.
- OSTI ID:
- 6259242
- Journal Information:
- Hydrotech. Constr.; (United States), Journal Name: Hydrotech. Constr.; (United States) Vol. 19:3; ISSN HYCOA
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
130200* -- Hydro Energy-- Site Geology & Meteorology
ASIA
BYELORUSSIAN SSR
DAMS
DEFORMATION
DISTRIBUTION
EASTERN EUROPE
ENGINEERING
EUROPE
FLUID MECHANICS
HYDRODYNAMICS
HYDROELECTRIC POWER PLANTS
HYDROLOGY
LEVELS
MASS DISTRIBUTION
MECHANICS
POWER PLANTS
RESERVOIR ENGINEERING
RIVERS
SEDIMENTS
SPATIAL DISTRIBUTION
STREAMS
SURFACE WATERS
USSR
VOLGA RIVER
WATER RESERVOIRS