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contributor authorGuangqian Wang
contributor authorJunqiang Xia
contributor authorBaosheng Wu
date accessioned2017-05-08T20:46:15Z
date available2017-05-08T20:46:15Z
date copyrightAugust 2008
date issued2008
identifier other%28asce%290733-9429%282008%29134%3A8%281064%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/26569
description abstractBank erosion frequently occurs in the Lower Yellow River (LYR), playing an important role in the evolution of this braided river. A two-dimensional (2D) composite model is developed herein that consists of a depth-averaged 2D flow and sediment transport submodel and a bank-erosion submodel. The model incorporates a new technique for updating bank geometry during either degradational or aggradational bed evolution, allowing the two submodels to be closely combined. Using the model, the fluvial processes in the braided reach of the LYR between Huayuankou and Laitongzhai are simulated, and the calculated results generally agree with the field measurements, including the water-surface elevation, variation of water-surface width, and variations of cross-sectional profiles. The calculated average water-surface elevation in the study reach was
publisherAmerican Society of Civil Engineers
titleNumerical Simulation of Longitudinal and Lateral Channel Deformations in the Braided Reach of the Lower Yellow River
typeJournal Paper
journal volume134
journal issue8
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(2008)134:8(1064)
treeJournal of Hydraulic Engineering:;2008:;Volume ( 134 ):;issue: 008
contenttypeFulltext


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