We present a semiempirical model of the bottom turbulent boundary layer aimed at the application as one of the components of the procedure of evaluation of the vertical distribution of the concentration of suspensions in the coastal region of the sea. The model is based on data of laboratory experiments and is suitable for the sand bottom in a broad range of amplitudes of the bottom velocities of the wave origin.
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V. A. Ivanov (Ed.), Methods and Means of Monitoring of the Marine Environment [in Russian], Marine Hydrophysical Institute, Ukrainian Academy of Sciences, Sevastopol (2006).
J. F. A. Sleat, “Turbulent oscillatory flow over rough beds,” J. Fluid Mech., 182, 369–409 (1987).
H. Schlichting, Boundary-Layer Theory, McGraw-Hill, New York (1955).
A. S. Monin and A. M. Yaglom, Statistical Fluid Mechanics, Dover, New York (2007), Vol. 1.
B. Le Meote, An Introduction to Hydrodynamics and Water Waves, Springer, New York (1976).
J. O. Hinze, Turbulence, McGraw-Hill, New York (1975).
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Translated from Morskoi Gidrofizicheskii Zhurnal, No. 2, pp. 49–62, March–April, 2010.
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Dykman, V.Z., Efremov, O.I. & Ivanov, V.A. A model of the bottom turbulent layer in the shallow-water region. Phys Oceanogr 20, 122–135 (2010). https://doi.org/10.1007/s11110-010-9072-4
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DOI: https://doi.org/10.1007/s11110-010-9072-4