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contributor authorDennis A. Lyn
date accessioned2017-05-08T20:39:39Z
date available2017-05-08T20:39:39Z
date copyrightJanuary 1987
date issued1987
identifier other%28asce%290733-9429%281987%29113%3A1%281%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22678
description abstractThe standard one‐dimensional equations of unsteady sediment‐transport are examined, and multiple time (or length) scales are identified. The existence of multiple scales may lead to a singularly perturbed behavior that should be taken into account in any general numerical model. Previous models, which reduce the number of conservation equations solved simultaneously from three to two, are seen to be unable to satisfy exactly either a general boundary condition or a general initial condition. Implications for numerical modeling are explored. Numerical results for the model problem of sediment‐deposition upstream of a dam illustrate the analytical argument.
publisherAmerican Society of Civil Engineers
titleUnsteady Sediment‐Transport Modeling
typeJournal Paper
journal volume113
journal issue1
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(1987)113:1(1)
treeJournal of Hydraulic Engineering:;1987:;Volume ( 113 ):;issue: 001
contenttypeFulltext


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