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Causes,Characteristics and Mitigation of 7.21 Catastrophic Debris Flow Hazard at the Longda Watershed of Songpan County,China

机译:松潘县龙达流域7.21特大泥石流灾害的成因,特征与减灾

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摘要

Debris flow is a popular natural hazard in the mountain areas of Western China due to favorable natural conditions,and also exacerbated by mountainous exploitation projects.This paper concentrated on the causes,characteristics and mitigation of a catastrophic debris flow hazard at Longda Watershed in Songpan County,Sichuan Province,on 21 July 2011,which was expanded by mining.This debris flow deposited in the front of the No.1 dam of the tailing sediment reservoir,moved into the drainage channel for flood and then rushed into tailing sediment reservoir and made the No.2 dam breached.The outburst debris flow blocked Fu River and produced dammed lake,whose outburst flood further delivered heavy metal into the lower of Fu River,polluting the drink water source of over 1 million population.The debris flow was featured with a density of 1.87~2.15 t/m3 and the clay content of less than 1.63%.The peak velocity and flux of the debris flow at Longda Gully was over 10.0~10.9 m/s and 429.0~446.0 m3/s,respectively,which equaled to the flux of the probability of 1%.The peak flux of 7.21 debris flow was about 700 m3/s in main channel.The debris flow deposits approached 330,000m3,which deposited in the drainage tunnel (120,000~130,000 m3),the front of No.1 dam (100,000 m3) and the mouth of the watershed (100,000~110,000 m3).It was proved that debris flow would block Fu River when the peak flux and magnitude of debris flow was more than 462 m3/s and 7,423 m3.The rainstorm,with an intensity of 21.2 mm/0.5h,triggered the abundant accumulated loose material,which was composed of landslides,slope deposits,mining wastes,tailing sediments,and formed this debris flow.The losses were mainly originated from the drainage tunnel for flash flood,which was not capable for debris flow drainage,and the irrational location of tailing sediment reservoir,which resulted in chain hazards including outburst debris flows,dammed lake and outburst flood,aggravating the hazards and loss.The mitigation measures for the debris flows induced by mining were presented: (1) The disastrous debris flow watershed should be identified and prohibited from being taken as the site of mining plant; (2) The mining factory was suggested to be constructed at the safe areas; (3) Scoria plots,concentrator factory and tailing sediment reservoir are constructed in low risk areas where the feasible protection measures can be easily made to prevent debris flows; (4) the appropriate system and plan including monitoring,remote monitoring and early-warning and emergency plan is established; (5) The stability of waste dump and tailing reservoir are monitored continuously and controlled to prevent mines debris flows.
机译:由于有利的自然条件,泥石流是中国西部山区的一种普遍的自然灾害,而且山区开发项目也加剧了泥石流。本文着眼于松潘县龙大流域的特大泥石流灾害的成因,特征和缓解措施。四川省,2011年7月21日,通过采矿进行了扩建。这些泥石流沉积在尾矿库1号大坝的前部,移入排水渠进行洪水,然后冲入尾矿库中, 2号大坝被破坏。爆发的泥石流阻塞了富河,形成了堰塞湖,爆发的洪水进一步将重金属输送到了富河的下游,污染了超过100万人的饮用水水源。密度为1.87〜2.15 t / m3,粘土含量小于1.63%。龙达沟泥石流的峰值速度和通量分别大于10.0〜10.9 m / s和429.0〜446.0 m3 / s分别等于概率为1%的通量。在主要通道中,7.21泥石流的峰值通量约为700 m3 / s。泥石流沉积物接近330,000m3,沉积在排水隧道中( 120,000〜130,000 m3),1号大坝前部(100,000 m3)和分水岭口(100,000〜110,000 m3)。证明了当泥石流的峰值通量和大小为时,泥石流会阻塞Fu河。超过462 m3 / s和7,423 m3。暴雨强度为21.2 mm / 0.5h,触发了堆积的大量疏松物质,这些物质由滑坡,斜坡沉积,采矿废物,尾矿沉积物组成,并形成了泥石流。损失主要来自于山洪暴发的排水隧道,无法进行泥石流的排泄,尾矿库的位置不合理,导致链条危害,包括爆发性泥石流,大坝湖泊和爆发性洪水,加剧了泥石流。危害和损失。缓解措施介绍了采矿引起的泥石流的原因:(1)应确定灾难性泥石流分水岭,并禁止将其作为采矿厂的所在地; (2)建议在安全区建矿山厂; (3)在低风险地区建有S田,选矿厂和尾矿库,可以很容易地采取可行的防护措施,防止泥石流; (4)建立包括监测,远程监测,预警和应急预案在内的适当的制度和计划; (5)持续监测和控制废物堆放场和尾矿库的稳定性,以防止矿山泥石流。

著录项

  • 来源
  • 会议地点 Chengdu(CN)
  • 作者单位

    Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China;

    Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China;

    Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China;

    Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China;

    University of Chinese Academy of Sciences, Beijing 100049, China;

    Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;

    Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境与发展;
  • 关键词

    Debris Flow; Characteristics; Causes; Mitigation Measures; Longda Watershed;

    机译:泥石流;特征;病因;缓解措施;龙大流域;

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