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Recent catastrophic debris flows in Luding county, SW China: geological hazards, rainfall analysis and dynamic characteristics

机译:中国西南Lu定县近期的灾难性泥石流:地质灾害,降雨分析和动力特征

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摘要

About 127 debris flow gullies have been identified, and debris flows have been an important type of geological hazards in Luding County, affecting cities, towns, rural areas, scenic spots and human's engineering projects, such as mining and waterpowerutilizing equipments. In this summary paper, recent two catastrophic debris flow events occurred on June 30, 2005, in Chuni town, in the central of the county, and on August 11, 2005, in Hailuogou scenic spot, in the southwest of the county, respectively, are reviewed. The debris flow events are introduced on the basis of field investigation and RS interpretation and the triggering factors for flow occurrence are identified. Furthermore, the rainfall related to flow occurrence including antecedent rainfall and intraday rainfall is analyzed, and a power-law function which can be used as a basic warning line is established based on both antecedent effective rainfall and intraday rainfall. Then dynamic parameters such as flow velocity and flow dischargeare calculated, respectively. Through comparison and discussion, some conclusions are made including (1) The antecedent rainfall played an important role for debris flows which generated predominately based on the slope-instability due to the saturated loose sediments; (2) Despite slower flow velocity and smaller magnitude, the slope-type debris flows just like 2005-6-30 debris flows usually lead to serious damages for the difficulty to forecast and to prevent; (3) The mistaken recognition on debris flow hazards and lack of prevention consciousness strengthen the hazard and damage degree. This research is of certain significance for the prevention and mitigation of debris flow hazards and for the planning of the town building and tourism development inthe future.
机译:在Lu定县,已发现约127个泥石流沟,泥石流已成为一种重要的地质灾害类型,影响到城市,城镇,农村地区,风景名胜区和人类工程项目,例如采矿和水力利用设备。在本摘要文件中,最近的两次灾难性泥石流事件分别于2005年6月30日发生在县中心的Chuni镇和2005年8月11日发生在县西南部的海螺沟风景区,被审查。在实地调查和遥感解释的基础上介绍了泥石流事件,并确定了发生泥石流的触发因素。此外,分析了与流量发生有关的降雨,包括前期降雨和日内降雨,并基于前期有效降雨和日内降雨建立了可以用作基本警告线的幂律函数。然后分别计算动力学参数,例如流速和流量。通过比较和讨论,得出以下结论:(1)前期降雨对泥石流起了重要作用,这些泥石流主要是由于饱和疏松沉积物引起的边坡失稳而产生的; (2)尽管流速较慢且幅值较小,但类似于2005-6-30的泥石流通常会由于难以预测和预防而造成严重破坏; (3)对泥石流危险性的错误认识和防范意识的缺乏,加剧了危险性和破坏程度。这项研究对于预防和减轻泥石流灾害以及对未来城镇建设和旅游业发展的规划具有重要意义。

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