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contributor authorRafael Duarte
contributor authorJuliano Ribeiro
contributor authorJean-Louis Boillat
contributor authorAnton Schleiss
date accessioned2017-05-08T21:51:11Z
date available2017-05-08T21:51:11Z
date copyrightNovember 2011
date issued2011
identifier other%28asce%29hy%2E1943-7900%2E0000472.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64294
description abstractThe overall dam-break phenomenon is currently well understood for reservoirs filled with water. However, many dams face serious problems of reservoir sedimentation. Thus, regarding risk management, the influence of a large amount of sediment in the reservoir on dam-break wave propagation is of great importance. Experimental investigations were performed to investigate the influence of the silting degree of reservoirs and grain size distribution on wave heights and velocities. Dam-break waves in silted-up reservoirs are the result of a two-phase flow formed by a layer of water over a layer of saturated sediments in which complex phenomena occur simultaneously. Sediments flow such as a viscous fluid from the dam breach until complete stoppage, and clear water flows over the sediments creating bed load transport. The final sediment deposition cone, the flow of the positive front, and maximum wave heights were studied. An empirical formula is proposed to describe the celerity of the positive wave front in the case of silted-up reservoirs.
publisherAmerican Society of Civil Engineers
titleExperimental Study on Dam-Break Waves for Silted-Up Reservoirs
typeJournal Paper
journal volume137
journal issue11
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)HY.1943-7900.0000444
treeJournal of Hydraulic Engineering:;2011:;Volume ( 137 ):;issue: 011
contenttypeFulltext


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