Distribution of velocities in an ice-covered stream

descriptionPublicationkeyboard_double_arrow_right Article 01 Feb 1967 English Publisher:Springer Science and Business Media LLCJournal:Hydrotechnical Construction, volume 1, pages 143-145 (issn: 0018-8220, eissn: 1570-1468,

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Authors: V. I. Sinotin;

doi: 10.1007/bf02379134

Distribution of velocities in an ice-covered stream

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Abstract

1. An analysis of the uniform motion of fluid in a wide channel, which was carried out by L. K. Nikitin, makes possible the development of a pattern of velocity structure for a stream flowing between two surfaces with different roughness. 2. The velocity structure of an ice-covered stream, determined on the basis of relations founded on considerable experimental data, corresponds for all practical purposes to the structure obtained by Academician N. N. Pavlovskii, utilizing the principle of maximum discharge capacity of a channel.

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