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Case Study of the Characteristics and Dynamic Process of July 10, 2013, Catastrophic Debris Flows in Wenchuan County, China

机译:2013年7月10日汶川特大灾害性泥石流特征与动态过程的案例研究

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The Wenchuan earthquake of May 12, 2008, generated a significant amount of loose solid material that can produce devastating debris flows. In the five years since the earthquake, there have been many large-scale individual and group catastrophic debris flows that have caused lots of damage to the resettled population and the reconstruction efforts. The reconstructed towns of Yingxiu, Yinxing and Miansi have suffered debris flows and other secondary disasters in the past five years and are still not out of danger in the future. A debris-flow catastrophic event hit four towns of Wenchuan County along the Duwen Highway, part of China's National Highway 213, at midnight on July 10, 2013, following a local extreme rainfall of 176.2mm 24h-1. The debris flows occurred simultaneously along seven gullies. A total of 15000 people were affected due to the destruction of resettlement areas, factories, power stations, and houses. Because of this devastating event, traffic along the Duwen highway was completely disrupted during the disaster and recovery period. The present study focuses on the Lianshan Bridge debris flow gully; the disaster characteristics and cause of the debris flow were analyzed based on field investigations, remote sensing interpretation, and laboratory experiments. The particular dynamic parameters of the debris flow were calculated and analyzed including density, velocity, discharge, total volume and impact force. Also, the dynamic processes and changes that occurred in the debris flow were examined, and the block and burst characteristics of debris flow were studied based on statistical calculation and analysis dynamic characteristic parameters of debris flow. Finally, a program to prevent further debris flow was proposed according to the on-site investigation and based on the analysis of the features and dynamic processes of the debris flow.
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,可产生毁灭性的泥石流。地震发生以来的五年中,发生了许多大规模的个人和团体灾难性泥石流,这些泥石流对重新安置的人口和重建工作造成了很多破坏。在过去的五年中,映秀,银兴和棉寺的重建镇遭受了泥石流和其他次生灾害的影响,未来仍将处于危险之中。 2013年7月10日午夜,一场泥石流灾难性事件袭击了汶川县的四个城镇,沿杜文公路(属于中国213国道的一部分),当时当地出现了176.2mm 24h-1的极端降雨。泥石流同时沿着七个沟壑发生。由于安置区,工厂,电站和房屋的破坏,共有15,000人受到影响。由于这一灾难性事件,在灾难和恢复期间,杜温高速公路沿线的交通完全中​​断。本文的研究重点是连山桥泥石流沟。根据实地调查,遥感解释和实验室实验分析了泥石流的灾害特征和原因。计算并分析了泥石流的特定动力学参数,包括密度,速度,流量,总体积和冲击力。此外,还检查了泥石流中发生的动力学过程和变化,并基于统计计算和分析泥石流的动态特征参数,研究了泥石流的阻塞和爆发特性。最后,根据现场调查并基于对泥石流的特征和动态过程的分析,提出了防止泥石流进一步流动的程序。

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