Zobrazeno 1 - 10
of 14
pro vyhledávání: '"E. I. Debolskaya"'
Publikováno v:
Лëд и снег, Vol 52, Iss 3, Pp 73-78 (2015)
We studied in the lab the interaction of river runoff from frozen soil, simulating the upper, active-layer, changing the thermal (warming) and mechanical (impact of rain) external influences. We determined the time of thawing of ground and infiltrati
Externí odkaz:
https://doaj.org/article/a1b0102096b1458e8d17ab6757e27daa
Publikováno v:
Лëд и снег, Vol 53, Iss 1, Pp 104-110 (2015)
This paper is devoted to investigation of the influence of river flow and of the temperature rise on the deformation of the coastal slopes composed of permafrost with the inclusion of ice layer. The method of investigation is the laboratory and mathe
Externí odkaz:
https://doaj.org/article/09dd41d4c5fb4473bfc31f761c7d5ec3
Autor:
E. I. Debolskaya, A. V. Ostyakova
Publikováno v:
Лëд и снег, Vol 53, Iss 4, Pp 107-112 (2015)
A common problem for the Arctic region is pollution by persistent organic compounds and other substances that have accumulated over the years in these areas. With temperature increasing, these substances can get out of the snow, ice, permafrost in th
Externí odkaz:
https://doaj.org/article/82bc9bb69ffb4fe0b709d4791c064e67
Publikováno v:
Water Resources. 50:252-263
Autor:
E. I. Debolskaya, G. A. Saminsky
Publikováno v:
Power Technology and Engineering. 55:881-887
Publikováno v:
Power Technology and Engineering. 55:384-389
Publikováno v:
PROCEEDINGS OF THE INTERNATIONAL CONFERENCE ON ENGINEERING RESEARCH 2021 (ICER 2021), MOSCOW, RUSSIA.
Publikováno v:
Permafrost 2021.
Publikováno v:
E3S Web of Conferences, Vol 163, p 01003 (2020)
The study is focused on the deformations caused by the impact of water flow in a river channel composed of melt-able permafrost rocks. It is based on the results of laboratory and mathematical simulation. The results of numerical calculations are com
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 321:012026
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