CHANNEL DEFORMATION AT DIFFERENT PHASES OF STREAM-FLOW REGIME (SECTOR OF MIDDLE OB' AS AN EXAMPLE)

I. N. Kargapolova; V. V. Surkov

doi:10.15356/0435-4281-2003-3-54-61

CHANNEL DEFORMATION AT DIFFERENT PHASES OF STREAM-FLOW REGIME (SECTOR OF MIDDLE OB' AS AN EXAMPLE)

I. N. Kargapolova, V. V. Surkov

https://doi.org/10.15356/0435-4281-2003-3-54-61

Abstract

Channel deformation rate at different phases of water regime was analysed. Conditions of sediment accumulation and breaking-up were determined and mobility of sediment was evaluated. The phase of maximum channel deformation intensity corresponds to the moments of channel-forming discharge.

About the Authors

I. N. Kargapolova

Lomonosov Moscow State University
Russian Federation

V. V. Surkov

Lomonosov Moscow State University
Russian Federation
Geographical Department

Review

For citations:

Kargapolova I.N., Surkov V.V. CHANNEL DEFORMATION AT DIFFERENT PHASES OF STREAM-FLOW REGIME (SECTOR OF MIDDLE OB' AS AN EXAMPLE). Geomorfologiya. 2003;(3):54-61. https://doi.org/10.15356/0435-4281-2003-3-54-61