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contributor authorDonatella Termini
date accessioned2017-05-08T21:50:33Z
date available2017-05-08T21:50:33Z
date copyrightJuly 2009
date issued2009
identifier other%28asce%29hy%2E1943-7900%2E0000083.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63882
description abstractMeanders of large amplitude often exhibit asymmetric planform shape or subsidiary bends. The present work is aimed at improving on understanding of the morphodynamic phenomena affecting the bed evolution of large amplitude meandering channels. Attention is focused on the development of the steady point bar-pool configuration and of the superimposed large-scale migrating bed forms; of particular interest is the role of the changing channel curvature and bed topography variation on flow pattern. A series of experiments was carried out in a sine-generated large-amplitude meandering flume, for two values of width-to-depth ratio. Maps documenting the bed topography and the flow pattern along the meandering bends are reported. Two point bars per bend were observed and seem to be part of a series of damped oscillations developing in response to the changing channel curvature. In response to the bed deformation, the maximum flow velocity moves at the outer bank at the entrance of the bend.
publisherAmerican Society of Civil Engineers
titleExperimental Observations of Flow and Bed Processes in Large-Amplitude Meandering Flume
typeJournal Paper
journal volume135
journal issue7
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)HY.1943-7900.0000046
treeJournal of Hydraulic Engineering:;2009:;Volume ( 135 ):;issue: 007
contenttypeFulltext


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