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contributor authorDavid W. Ostendorf
date accessioned2017-05-08T20:58:25Z
date available2017-05-08T20:58:25Z
date copyrightOctober 1986
date issued1986
identifier other%28asce%290733-9372%281986%29112%3A5%28939%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/33865
description abstractA simple model of the steady, two‐dimensional water flow through rectangular clarifiers is derived in the absence of wind and stratification. The water flow, or “hydraulics,” consists of steady velocity and turbulence intensity, and both properties are considered in the analysis. The inlet, settling, and outlet zones are marked by turbulent jet, uniform, and converging flow fields, respectively. Existing analytical solutions and turbulent jet data are invoked to generate a composite, independently calibrated set of velocity profiles that compare favorably with data from clarifier studies. The depth‐averaged turbulence intensity is an integral part of the present model and is shown to be generated by the inlet jet flow rather than bottom and wall friction. The intensity governs sediment resuspension in accordance with the Shields criterion for fine sediment, which is cast into a useful constraint on the clarifier geometry.
publisherAmerican Society of Civil Engineers
titleHydraulics of Rectangular Clarifiers
typeJournal Paper
journal volume112
journal issue5
journal titleJournal of Environmental Engineering
identifier doi10.1061/(ASCE)0733-9372(1986)112:5(939)
treeJournal of Environmental Engineering:;1986:;Volume ( 112 ):;issue: 005
contenttypeFulltext


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