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    Draining the Tangjiashan Barrier Lake

    Source: Journal of Hydraulic Engineering:;2010:;Volume ( 136 ):;issue: 011
    Author:
    Ning Liu
    ,
    Zuyu Chen
    ,
    Jianxin Zhang
    ,
    Wei Lin
    ,
    Wuyi Chen
    ,
    Wenjie Xu
    DOI: 10.1061/(ASCE)HY.1943-7900.0000241
    Publisher: American Society of Civil Engineers
    Abstract: This 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
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      Draining the Tangjiashan Barrier Lake

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    http://yetl.yabesh.ir/yetl1/handle/yetl/64073
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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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