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contributor authorNing Liu
contributor authorZuyu Chen
contributor authorJianxin Zhang
contributor authorWei Lin
contributor authorWuyi Chen
contributor authorWenjie Xu
date accessioned2017-05-08T21:50:52Z
date available2017-05-08T21:50:52Z
date copyrightNovember 2010
date issued2010
identifier other%28asce%29hy%2E1943-7900%2E0000264.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64073
description abstractThis paper documents the emergency breaching of an approximately 110-m-high landslide dam that was created at Tangjiashan during the 2008 Wenchuan earthquake of China’s Southwest Sichuan Province. As an emergency measure, a 13-m-deep channel was excavated to reduce the volume and head of the released water during the dam breaching and to create a controlled flood that was intended to prevent catastrophic consequence for 1.2 million people downstream. From detailed monitoring and survey works carried out during and after the dam break it was found that (1) the breaching initiated at a pool water level of 742.1 m with an estimated flow velocity of 2.4 m/s, and virtually terminated at a pool water level of 720.3 m with an estimated velocity of 2.5 m/s, which can be regarded as the incipient velocity that initiated erosions for the soils at this particular site; (2) a controlled flood released
publisherAmerican Society of Civil Engineers
titleDraining the Tangjiashan Barrier Lake
typeJournal Paper
journal volume136
journal issue11
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)HY.1943-7900.0000241
treeJournal of Hydraulic Engineering:;2010:;Volume ( 136 ):;issue: 011
contenttypeFulltext


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