Research Article
Jul 1970

Nonequilibrium Transport of Suspended Sediment

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Publication: Journal of the Hydraulics Division
Volume 96, Issue 7

Abstract

The nonequilibrium transport of suspended sediment in an open channel is studied at an abrupt change from a nonerodible to an erodible bed. The convective-diffusion equation is solved for the case of constant velocity distribution and parabolic eddy diffusion coefficient. Diffusion in the direction of flow is neglected. Graphs of the concentration distribution, the channel-depth average concentration and the scour rate are presented.

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Journal of the Hydraulics Division
Volume 96Issue 7July 1970
Pages: 1567 - 1586

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Published in print: Jul 1970
Published online: Feb 3, 2021

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Allen T. Hjelmfelt, AM.ASCE
Assoc. Prof. of Civ. Engrg., Univ. of Missouri at Columbia, Columbia, M. O
Charles W. Lenau, AM.ASCE
Assoc Prof. of Civ. Engrg., Univ. of Missouri at Columbia, Columbia, M. O

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