The Influence of Thermal Erosion at River Bed Deformation in Permafrost Areas

The study is focused on the deformations caused by the impact of water flow in a river channel composed of meltable permafrost bed materials. It is based on the results of laboratory and mathematical simulation. The results of numerical calculations are compared with data of laboratory and field observations. The study shows that a comprehensive and adequate model of river channel deformations should take into account not only ablation, but also other factors, including heat transfer in the soil, sediment transport, and bank slope collapses. Experiments in a hydraulic flume were good enough to reproduce the effect of delayed collapse, consisting in nonsimultaneous impacts of channel-forming rock melting and a freshet. The major factors that have an effect on channel transformations in permafrost-zone rivers are identified. © 2021 American Society of Civil Engineers.

Authors
Debolskaya E.1 , Debolskiy V.1 , Maslikova O. 1 , Gritsuk I. 2 , Ivanov A. 3
Publisher
American Society of Civil Engineers (ASCE)
Language
English
Pages
14-26
Status
Published
Year
2021
Organizations
  • 1 Water Problems Institute, Russian Academy of Sciences, Moscow, Russian Federation
  • 2 Water Problems Institute, Russian Academy of Sciences, RUDN Univ., Moscow, Russian Federation
  • 3 Politecnico di Torino, Corso Duca degli Abruzzi, Torino, Italy
Keywords
Deformation; Flow of water; Heat transfer; Rivers; Sediment transport; Bed deformation; Bed materials; Field observations; Laboratory simulation; Mathematical simulations; Numerical calculation; Permafrost area; River bed; River channels; Thermal erosion; Permafrost
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