ПРОГНОЗ ВЛИЯНИЯ КУРУМОВ НА ОБЪЕМ ВОДОХРАНИЛИЩ

Abstract

The impact on the volume of reservoirs Kurume manifested during the action of two processes opposite direction. First - volume reduction due to the filling cap by debris and silt as a result of processes rock streams morpholithogenesis. The second process - the increase in the cup volume as a result of thawing ice of flooded rock streams and subsequent drawdown rudaceous mass. The method of quantitative assessment of the impact of rock streams on the volume reservoir is suggested. It is concluded that the effect of rock streams for during operation Kolyma HPP expressed in the slight increase in its bowl.