NATURAL-ANTHROPOGENIC DEFORMATIONS OF THE OKA RIVER BED NEAR RYAZAN'

K. M. Berkovitch; L. V. Zlotina; L. A. Turykin

doi:10.15356/0435-4281-2009-2-26-32

NATURAL-ANTHROPOGENIC DEFORMATIONS OF THE OKA RIVER BED NEAR RYAZAN'

K. M. Berkovitch, L. V. Zlotina, L. A. Turykin

https://doi.org/10.15356/0435-4281-2009-2-26-32

Abstract

The trend of channel vertical deformations in the Ryazan' stretch of the Oka river was discovered by analysis of long-term channel volume changes and their comparison with bed sediment excavation volume. Sand excavations are the main factor of channel volume changes, while the natural process remaining under such conditions is weak and corresponds to slow accumulation.

About the Authors

K. M. Berkovitch

Moscow State University, Moscow
Russian Federation
Geographical Department

L. V. Zlotina

Moscow State University, Moscow
Russian Federation
Geographical Department

L. A. Turykin

Moscow State University, Moscow
Russian Federation
Geographical Department

References

1. Беркович К.М. Современная трансформация продольного профиля верхней Оки // Геоморфология. 1993. № 3. С. 43–49.

2. Проектирование судовых ходов на свободных реках. / Тр. ЦНИИЭВТ. М.: Транспорт, 1964. Вып. 36. 261 с.

3. Маккавеев Н.И. Русло реки и эрозия в ее бассейне. М.: Изд-во АН СССР, 1955. 348 с.

Review

For citations:

Berkovitch K.M., Zlotina L.V., Turykin L.A. NATURAL-ANTHROPOGENIC DEFORMATIONS OF THE OKA RIVER BED NEAR RYAZAN'. Geomorfologiya. 2009;(2):26-32. https://doi.org/10.15356/0435-4281-2009-2-26-32