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Characteristics and hazard prediction of large-scale debris flow of Xiaojia Gully in Yingxiu Town, Sichuan Province, China

机译:四川省映秀镇小家沟大尺度泥石流特征及危害预测

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摘要

The Wenchuan earthquake of May 12,2008 produced large amounts of loose solid material that can lead to the development of devastating debris flows. In 5 years since the earthquake, large numbers of large-scale debris flows occurred and caused great damage to the resettled population and the reconstruction efforts. The reconstructed Yingxiu Town suffered debris flow and its secondary disaster in the past 5 years, and will be in the risk range of debris flow hazard in the future. It is very important to predict debris flow and its secondary hazard (especially the dam-breaking flood) near the town. The debris flow of the Xiaojia Gully was described and analyzed as a typical large-scale case in the Yingxiu area. The study aimed to describe the debris flow event, investigate the sediment supply conditions, analyze the characteristics of the debris flow deposition, calculate the river-blocking parameters, and predict the damage of dam-breaking flood to Yingxiu Town under different debris flow frequencies. Debris flows in Xiaojia Gully were well developed and occurred several times, resulting in frequent interruption of traffic on the S303 road. The interpretation of satellite images showed that landslide deposition, channel deposition, and soil erosion sediment were three kinds of sediment supply types for debris flow formation. 188 sediment supply sites in total were identified in the catchment. The total area for the supply of sediment for debris flows is about 0.99 km2, giving a total volume of 532.09 × 10~4 m~3. If the Yuzi River is blocked by debris flow material, the dam-breaking flood can cause potential damage to the newly constructed Yingxiu Town. The calculation results reveal that debris flows with a frequency of 5% and 10% are impossible to cause river-blockage, and consequently, the Yingxiu Town is safe in these situations. However, debris flows with a frequency of 1% and 2% may cause river blockage and the dam-breaking flood can cause damage to the Yingxiu Town.
机译:2008年5月12日的汶川地震产生了大量松散的固体物质,这些物质可能导致破坏性泥石流的发展。地震发生后的5年中,大量泥石流发生,对安置人口和重建工作造成了严重破坏。重建的映秀镇近5年遭受泥石流灾害和二次灾害,未来将处于泥石流灾害的危险范围。预测城镇附近的泥石流及其次生危害(尤其是溃坝洪水)非常重要。肖家沟的泥石流被描述和分析为映秀地区的典型大规模案例。该研究旨在描述泥石流事件,调查泥沙供应条件,分析泥石流沉积特征,计算阻水参数以及预测在不同泥石流频率下溃坝洪水对映秀镇的破坏。小家沟的泥石流发育良好,发生了几次,导致S303公路上的交通频繁中断。卫星图像的解释表明,滑坡沉积,河道沉积和土壤侵蚀沉积物是泥石流形成的三种沉积物供应类型。流域共有188个沉淀物供应地点。泥石流的沉积物供应总面积约为0.99 km2,总体积为532.09×10〜4 m〜3。如果鱼子河被泥石流阻塞,那么溃坝洪水将对新建的映秀镇造成潜在的破坏。计算结果表明,频率为5%和10%的泥石流不可能引起河道阻塞,因此,映秀镇在这种情况下是安全的。但是,泥石流的频率为1%和2%可能会造成河道阻塞,而溃坝的洪水可能会损坏映秀镇。

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