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Developmental features and evaluation of blocking dangers of big ditch debris flow in Tang jiashan Dammed Lake

机译:唐家山堰塞湖大沟泥石流发育特征及阻塞危险性评价

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Big Ditch is at the upstream side of Tang Jiashan. It was a mountain gully before the "5.12" earthquake, however due to the collapses and landslides after the earthquake, the extremely rich loose sources were formed, with all conditions of the occurrence of a debris flow. And it has become one of the serious potential dangers of geological disasters after Tang Jiashan dammed lake successful discharge, and it also controls the normal use of Tang Jiashan dammed lake. The article is through on-the-spot investigation, on the basis of identifying the distribution and stability of the groove loose source, and combines the devel- opmental situation of "6.14" debris flow, systematically analyzes the developmental and dynamic features of Big Ditch debris flow. In particular, it analyzes the possible size of the debris flow under the different rain frequencies, and it evaluates the possible dangers of the blocking size, duration and outburst forms. The re- suits of analysis were confirmed by the once in 100year debris flow on September 24, 2008.
机译:大沟位于唐家山的上游。 “ 5.12”地震之前是山区沟壑,但由于地震后的坍塌和山体滑坡,形成了极为丰富的松散震源,在所有情况下都发生了泥石流。唐家山堰塞湖成功泄洪后,已成为地质灾害的重大潜在危险之一,也制约着唐家山堰塞湖的正常利用。本文是通过现场调查,在识别出槽松散源的分布和稳定性的基础上,结合“ 6.14”泥石流的发展情况,系统地分析了大沟的发育和动力特征。泥石流。特别是,它分析了在不同降雨频率下泥石流的可能大小,并评估了阻塞大小,持续时间和突出形式的可能危险。 2008年9月24日,百年一次的泥石流证实了分析的结果。

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