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contributor authorP. R. Wormleaton
contributor authorR. D. Hey
contributor authorR. H. Sellin
contributor authorT. Bryant
contributor authorJ. Loveless
contributor authorS. E. Catmur
date accessioned2017-05-08T20:45:12Z
date available2017-05-08T20:45:12Z
date copyrightAugust 2005
date issued2005
identifier other%28asce%290733-9429%282005%29131%3A8%28665%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/25956
description abstractMeasurements of velocity distributions, depth variation, and sediment transport have been made under bankfull and overbank flow conditions in meandering channels with a graded sand bed, using the large-scale U.K. Flood Channel Facility. The overbank conditions depend upon the relative strength of opposing secondary circulation cells generated by shear at the channel crossover and centrifugal forces around the meander bend. Generally the shear-generated secondary flow either reversed or weakened the centrifugal circulation around the next downstream bend. This led to considerable modification of the main channel bed morphology, which, in turn, altered flow distributions. Measurements of the lateral distribution of bed load were made using a
publisherAmerican Society of Civil Engineers
titleBehavior of Meandering Overbank Channels with Graded Sand Beds
typeJournal Paper
journal volume131
journal issue8
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(2005)131:8(665)
treeJournal of Hydraulic Engineering:;2005:;Volume ( 131 ):;issue: 008
contenttypeFulltext


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