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Modeling potential scenarios of the Tangjiashan Lake outburst and risk assessment in the downstream valley

机译:唐家山湖爆发的潜在情景建模及下游河谷的风险评估

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摘要

This research is devoted to Tangjiashan Lake, a quake landslide-dammed lake, situated in Sichuan Province, China, which was formed by a landslide triggered by the Wenchuan Earthquake on 12 May 2008. A STREAM_2D two-dimensional hydrodynamic model of Russia was applied to simulate the process of two flood scenarios: 1, lake dam outbreak, and 2, dam overtopping. An artificial dam outbreak was made after the earthquake to lower the water level of the lake in 2008, which led to a great flood with a maximum water discharge of more than 6400 m(3)/s. The negative impact of the flood was reduced by a timely evacuation of the population. Flood hazards still remain in the event of new landslides into the lake and lake dam overtopping (Scenario 2), in which case a maximum water discharge at the dam crest would reach 5000 m(3)/s, placing the population of Shabacun and Shilingzi villages in the zone of flood impact.
机译:这项研究致力于唐家山湖,这是一个位于中国四川省的地震滑坡坝湖,它是由2008年5月12日汶川地震引发的滑坡形成的。俄罗斯的STREAM_2D二维水动力模型被应用于模拟两种洪水情景的过程:1,湖泊大坝暴发和2,水坝越界。地震发生后,在2008年发生了人工大坝暴发,从而降低了湖中的水位,导致了大洪水,最大排水量超过6400 m(3)/ s。及时撤离人口减少了洪水的负面影响。如果新的山体滑坡进入湖泊和湖泊大坝超顶(方案2),洪水风险仍然存在,在这种情况下,坝顶的最大排水量将达到5000 m(3)/ s,这将使Shabacun和Shilingzi人口洪水泛滥区的村庄。

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