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Carrying Capacity of a Flow with Flow Rounding under Permafrost Conditions

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Power Technology and Engineering Aims and scope

Under natural conditions in winter, narrowing of a flow due to partial freezing of the channel and formation of a slush ice run or ice jam, as a result of which flow speeds increase in sections of the turn of the channel, is characteristic. Laboratory experiments that have been carried out in the rotary installation of the hydraulics laboratory at the to model such a section, have shown that if the flow speeds entering the curvature increase or there is an increase in the Reynolds number, vortex motions and counterflows at the inner slope inevitably occur, which inevitably is shown in the nature of the channel washout.

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References

  1. E. I. Debol’skaya, V. K. Debol’skii, I. I. Gritsuk, O. Ya. Maslikova, and D. N. Ionov, “Modeling the deformations of channels made by frozen ground as the environmental temperature rises,” Led i Sneg, No. 1(121), 104 – 110 (2013).

  2. V. K. Debol’skii, O. Ya. Maslikova, D. N. Ionov, I. I. Gritsuk, and N. T. Dzhumagulova, “Laboratory study of the effect of flow on the thawing of an underwater slope and the rates of bank erosion under permafrost conditions,” Vestn. RUDN. Ser. Inzh. Issl., No. 2, 182 – 192 (2017).

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  4. I. I. Gritsuk, V. K. Debol’skii, O. Ya. Maslakova, and N. K. Ponomarev, “The effect of precipitates in the form of rain on the deformation of a bank slope of river channels under conditions of long-term frozen soils,” Led i Sneg, No. 3(119), 73 – 78 (2012).

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Correspondence to V. K. Debol’skii.

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Translated from Gidrotekhnicheskoe Stroitel’stvo, No. 3, March 2020, pp. 36 – 40.

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Debol’skii, V.K., Maslikova, O.Y. & Gritsuk, I.I. Carrying Capacity of a Flow with Flow Rounding under Permafrost Conditions. Power Technol Eng 54, 313–317 (2020). https://doi.org/10.1007/s10749-020-01208-9

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  • DOI: https://doi.org/10.1007/s10749-020-01208-9

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