院报 ›› 2023, Vol. 40 ›› Issue (1): 94-100.DOI: 10.11988/ckyyb.20210760

• 工程安全与灾害防治 • 上一篇    下一篇

北京山区泥石流的单沟预报

陈文鸿1, 余斌1, 柳清文2, 路璐3, 马超4, 孙帅5, 师春香5   

  1. 1.成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都 610059;
    2.福建省地质工程勘察院 自然资源部丘陵山地地质灾害防治重点实验室,福州 350002;
    3.北京市地质矿产勘查院 北京市地质灾害防治研究所,北京 100120;
    4.北京林业大学 水土保持学院,北京 100083;
    5.中国气象局 国家气象信息中心,北京 100081
  • 收稿日期:2021-07-23 修回日期:2021-10-13 出版日期:2023-01-01 发布日期:2023-02-24
  • 通讯作者: 余 斌(1966-),男,四川成都人,教授,博士,主要从事泥石流灾害防治与研究工作。E-mail:yubin08@cdut.cn
  • 作者简介:陈文鸿(1994-),男,广西柳州人,博士研究生,主要从事地质灾害防治与预警方面的研究 。E-mail:625006176@qq.com
  • 基金资助:
    国家自然科学基金项目(U21A2032);北京市沟道侵蚀泥石流多元预警阈值模型研究及示范工程项目(Z191100001419015)

Forcast of Single Ditch Debris Flow in Mountainous Areas of Beijing

CHEN Wen-hong1, YU Bin1, LIU Qing-wen2, LU Lu3, MA Chao4, SUN Shuai5, SHI Chun-xiang5   

  1. 1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology, Chengdu 610059,China;
    2. Key Laboratory of Geohazard Prevention of Hilly Mountain of Ministry of Land and Resources,Fujian Geological Engineering Survey Institute,Fuzhou 350002,China;
    3. Beijing Institute of Geological Hazard Prevention,Beijing Institute of Geology,Beijing 100120,China;
    4. School of Soil and Water Conservation,Beijing Forestry University,Beijing 100083,China;
    5. National Meteorological Information Center,China Meteorological Administration,Beijing 100081,China
  • Received:2021-07-23 Revised:2021-10-13 Online:2023-01-01 Published:2023-02-24

摘要: 为给北京山区单沟泥石流灾害预警预报提供理论依据,基于近十几年北京山区单沟泥石流文献资料,从泥石流灾害形成机理出发,结合目前降雨站点数据,分析诱发泥石流的地形、地质和降雨等相关因素,采用适用于北京山区泥石流预报模型P=RT0.2/G0.5 ,得出适用于北京山区单沟泥石流蓝、黄、橙、红Ⅳ级预警模型和相应临界值。研究得出的北京山区泥石流单沟Ⅳ级预警模型能很好地预报短期灾害发生,在龙潭沟等流域的验证中,可以较好地根据降雨的变化情况得出泥石流沟道不同时间段的泥石流易发程度,该模型为该区泥石流易发等级的快速识别提供了科学有效的方法。

关键词: 泥石流, 预报模型, 沟床起动, 北京山区, 单沟

Abstract: The aim of this research is to offer theoretical basis for forecasting and warning single-ditch debris flow in the mountainous area of Beijing.Factors such as topography,geology,and rainfall that induce debris flow were analyzed in line with the formation mechanism of debris flow based on literature review in recent decade and rainfall data.The model P=RT0.2/G0.5 was adopted for forecasting single-ditch debris flow in the mountainous area of Beijing,and the warning models and corresponding thresholds for blue,yellow,orange and red warning levels were obtained and further applied to forecasting the debris flow in Longtan gully for verification.Results demonstrated that the forecasting model in the present paper could well predict short-term debris flow and acquire the susceptibility of debris flow in different time periods according to rainfall changes.The model can be taken as a scientific and effective method for rapidly identifying the susceptibility level of debris flow in the mountainous area of Beijing.

Key words: debris flow, prediction model, runoff mechanism, mountainous area in Beijing, single-ditch

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