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The Role of Currents and Waves in the Movement of Sediments in the Vicinity of Coastal Hydraulic Structures

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Power Technology and Engineering Aims and scope

This paper discusses the conditions of sediment accumulation in the access channel and deep-water area around the “Utrennii” terminal. The main factor of the sediment accumulation in the access channel is the movement of silt sediments by the tidal currents and extreme storm waves. The sediment accumulation in the deep-water area around the terminal is determined by the inflow of both sandy sediments and silty deposits transported by the wave currents.

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Authors and Affiliations

  1. National Research Moscow State University of Civil Engineering (NRU MGSU), Moscow, Russia

    Ghinwa Hadla, A. S. Anshakov & I. G. Kantarzhi

Authors
  1. Ghinwa Hadla
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  2. A. S. Anshakov
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  3. I. G. Kantarzhi
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Corresponding author

Correspondence to Ghinwa Hadla.

Additional information

Translated from Gidrotekhnicheskoe Stroitel’stvo, No. 10, October 2020, pp. 52 – 59.

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Hadla, G., Anshakov, A.S. & Kantarzhi, I.G. The Role of Currents and Waves in the Movement of Sediments in the Vicinity of Coastal Hydraulic Structures. Power Technol Eng 54, 841–847 (2021). https://doi.org/10.1007/s10749-021-01297-0

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  • DOI: https://doi.org/10.1007/s10749-021-01297-0

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