The effect of flow velocity distribution on matter transport in a curved channel segment with the effect of moving ships taken into account

Ship transport produces a special type of bank waves, which have a specific effect on the boundaries of water bodies other than that of the wind-induced waves. In addition, the extent of frozen-bank erosion at a bend of river channel is determined by the entering flow velocity, which can increase in winter because of channel constriction due to freezing or ice jams and gorges. The accompanying vortices have a considerable effect on the flow velocity pattern. © 2019 IOP Publishing Ltd. All rights reserved.

Authors
Maslikova O.Y. 1 , Gritsuk I.I. 1, 2, 3 , Debol'Skaya E.I.1, 4
Conference proceedings
IOP Conference Series: Earth and Environmental Science
Publisher
Institute of Physics Publishing
Number of issue
1
Language
English
Status
Published
DOI
10.1088/1755-1315/321/1/012026
Number
012026
Volume
321
Year
2019
Organizations
  • 1 Water Problems Institute, Russian Academy of Sciences, Moscow, 119333, Russian Federation
  • 2 RUDN University, Moscow, 117198, Russian Federation
  • 3 Moscow Automobile and Road Construction State Technical University, Moscow, 125319, Russian Federation
  • 4 Moscow State University of Civil Engineering, Moscow, Russian Federation
Keywords
Catchments; Reservoirs (water); Runoff; Ships; Velocity distribution; Bank erosion; Curved channels; Ice jams; River channels; Specific effects; Velocity patterns; Waterbodies; Wind induced waves; Flow velocity
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