Author(s): Aleksey A. Kosarev
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Keywords: No Keywords
Abstract: The special transition VL 100 kV Zaovrazhie-Solvychegodsk is situated 2 km downstream the river Vychegda from the town Solvychegodsk between the Solvychegodsky and the upper Sheshurovsky rapids. Recently intensive erosion of the left bank near the transition support №34 has been found out. The change of the river natural hydrological mode owing to the simulated rectification of the riverbed executed in 1987-1988 caused this erosion. To work out the guidelines on the avoidance of the bank erosion it is necessary to have the data about the hydrological and ice mode of the Vychegda in the transition region including parametric observations of the spring ice run in 2003.
Year: 2004