Conclusions
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1.
A theoretical system is proposed and a simplified postulation is formulated for the problem of thermally stratified flow in basins of elongated shape.
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2.
A sample calculation made on an electronic computer illustrates the characteristic features of stratified flow and the possibilities of modeling it numerically.
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3.
The proposed approach can be used for calculating hydrothermal phenomena in waterways and reservoirs of elongated shape, transporting cooling water from the discharges condensers of nuclear and thermal power stations.
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Literature Cited
S. S. Zilitinkevich, Dynamics of the Boundary Layer of the Atmosphere [in Russian], Gidrometeoizdat, Leningrad (1970).
O. F. Vasil'ev and V. I. Kvon, “Unsteady turbulent flow in a pipe,” Zh. Prikl. Mekhan. i Tekh. Fiz., No. 6 (1971).
G. S. Glushko, Turbulent Boundary Layer on a Flat Plate in a Compressible Fluid, Izv. Akad. Nauk SSSR, Mekhanika, No. 4 (1965).
Additional information
Translated from Gidrotekhnicheskoe Stroitel'stvo, No. 4, pp. 35–38, April, 1974.
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Vasil'ev, O.F., Kvon, V.I. & Chernysheva, R.T. Thermally stratified flow in a basin of elongated shape. Hydrotechnical Construction 8, 342–346 (1974). https://doi.org/10.1007/BF02406942
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DOI: https://doi.org/10.1007/BF02406942