TECHNICAL PAPERS
Mar 1, 1992

Fully Coupled Unsteady Mobile Boundary Flow Model

Publication: Journal of Hydraulic Engineering
Volume 118, Issue 3

Abstract

A fully coupled, one‐dimensional river model, capable of predicting sediment‐transport and bed‐level changes under unsteady flow conditions is described. The governing equations for mass and momentum balance of sediment‐water mixture under unsteady flow conditions in natural rivers with irregular geometries, are solved simultaneously using the Preissmann four‐point linear implicit scheme with weighting factors for space and time coordinates. The resulting system of algebraic equations is solved using a solution procedure that bridges upstream and downstream boundary nodal values by successive substitutions. The friction slope is expressed in a consistent form that allows the consideration of the changing alluvial roughness effect. The system of governing equations is explicitly coupled by introducing the term representing the rate of change of bed level. The fully coupled unsteady mobile boundary flow model (FCM) is applied to the classical problem of sediment deposition upstream of a dam with an arbitrary sediment hydrograph at the upstream boundary as well as to some other proof‐of‐concept tests to demonstrate its original features.

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 118Issue 3March 1992
Pages: 476 - 494

History

Published online: Mar 1, 1992
Published in print: Mar 1992

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Authors

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LuíR. P. Correia
Res. Asst., Laboratoire de Recherches Hydrauliques, Ecole Polytechnique Fédérate, Lausanne, Switzerland
Bommanna G. Krishnappan
Nat. Water Res. Inst., Canada Ctr. for Inland Waters, Burlington, Ontario, Canada; formerly, Visiting Prof., Laboratoire de Recherches Hydrauliques, Ecole Polytechnique Fédérale, Lausanne, Switzerland
Walter H. Graf
Prof., Laboratoire de Recherches Hydrauliques, Ecole Polytechnique Fédérale, Lausanne, Switzerland

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