Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (6): 1781-1788.doi: 10.13278/j.cnki.jjuese.201506201

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Hazard Assessment on Rainfall-Triggered Landslide and Debris Flow in the Seismic Disturbance Area at Watershed Level

Wang Meng, Jiang Yuanjun, Huang Dong, Li Qianqian   

  1. Key Laboratory of Geo-Surface Process and Mountain Hazards, Institute of Mountain Hazards and Environment, Chinese Academy of Science, Chengdu 610041, China
  • Received:2014-02-20 Published:2015-11-26

Abstract:

There are many loose slopes existed in the seismic disturbance area. Landslides and debris flow can be easily induced by a heavy or concentrated rainfall. The hazards often occur in a form of chain in an earthquake region with a severer harm than the one caused by a single disaster. In order to evaluate the geological hazards effectively, we regard the landslide and debris flow as a disaster chain and conduct the analysis synthetically. A coupled model has been developed to assess the hazard degree of debris flow induced by the different 24 h precipitation at watershed level in Baishahe watershed of Dujiangyan City in Sichuan Province. The model comprises of a landslide susceptibility evaluation model, a stability model, a hydrological model to predict unstable slopes and determine the amount of landslides to be involved, and a statistical model to evaluate the hazard degree of debris flow gully by selecting debris flow volume, frequency, basin area, main gully length, height difference, cutting density, and the ratio of unstable gully bed as the evaluation parameters. The results show that the volume of loose material involved in debris flow increase with the intensity of rainfall. However, when 24 h rainfall is over 200 mm, the hazard degree of debris flow does not change any more. Among the 17 debris flows,four debris flows are middle hazardous, twelve debris flows are high hazardous, and one debris flow is very high. It indicates that the potential geological hazard is quite serious in the study area. During the rainy season, 17 debris flows might concentratedly outbreak; which would directly threaten the nearby human lives and properties. The protection engineering and early-alert should be set to eliminate the hazards caused by the debris flows in comply with the high level fortification standard. By the way, it's necessary to take landslide and debris flow as a disaster chain to make the hazard assessment.

Key words: watershed, seismic disturbance area, landslide, debris flow, hazard assessment

CLC Number: 

  • P642.22

[1] Jibson R W, Harp E L, Michael J A.A Method for Producing Digital Probabilistic Seismic Landslide Hazard Maps[J]. Engineering Geology, 2000,58: 271-289.

[2] 崔鹏,韦方强,何思明,等.5·12汶川地震诱发的山地灾害及减灾措施[J].山地学报,2008,26(3):280-282. Cui Peng, Wei Fangqiang, He Siming,et al. Mountain Disasters Induced by the Earthquake of May 12 in Wenchuan and the Disasters Mitigation[]. Journal of Mountain Science, 2008,26(3): 280-282.

[3] Rajakumar P, Sanjeevi S, Jayaseelan S,et al. Lan-dslide Susceptibility Mapping in a Hilly Terrain Using Remote Sensing and GIS[J]. Journal of the Indian Society of Remote Sensing, 2007, 35(1): 31-42.

[4] Wang M, Qiao J P, He S M. GIS-Based Earthquake-Triggered Landslide Hazard Zoning Using Contributing Weight Model[J]. Journal of Mountain Science, 2010, 7:339-352.

[5] Lee C T, Huang C C, Lee J F,et al. Statistical Approach to Earthquake-Induced Llandslide Susceptibility[J]. Engineering Geology, 2008, 100:43-58.

[6] Carrara A, Pike R J. GIS Technology and Models for Assessing Landslide Hazard and Risk[J]. Geomorphology, 2008, 94: 257-260.

[7] 兰恒星,伍法权,周成虎,等.GIS支持下的降雨型滑坡危险性空间分析预测[J].科学通报,2003,48(5): 507-512. Lan Hengxing, Wu Faquan, Zhou Chenghu ,et al. Rainfall-Induced Landslide Hazard Spatial Analyze and Prediction Based on GIS[J]. Chinese Science Bulletin, 2003,48(5): 507-512.

[8] Muntohar A, Liao H. Rainfall Infiltration: Iinfinite Slope Model for Landslides Triggering by Rainstorm[J]. Natural Hazards, 2010, 54(3): 967-984.

[9] Baum, R L, Savage W Z, Godt J W. TRIGRS :A Fortran Program for Transient Rainfall Infiltration and Grid-Based Regional Slope Stability Analysis[J]. US Geological Survey Open-File Report,2002,424: 38.

[10] 庄建琦,彭建兵,张利勇. 不同降雨条件下黄土高原浅层滑坡危险性预测评价[J].吉林大学学报:地球科学版,2013,43(3):867-876. Zhuang Jianqi, Peng Jianbing, Zhang Liyong. Risk Assessment and Prediction of the Shallow Landslide at Different Precipitation in Loess Plateau[J]. Journal of Jilin University:Earth Science Edition, 2013, 43(3): 867-876.

[11] Montogery D R, Dietrich W E. A Physically Based Model for the Topographic Control on Shallow Landsliding[J]. Water Resources Research, 1994, 30:1153-1171.

[12] O'Loughlin E M. Prediction of Surface Saturation Zones in Natural Catchments by Topographic Analysis[J]. Water Resources Research, 1986, 22:794-804.

[13] Griswold J P, Iverson R M. Mobility and Statistics and Automated Hazard Mapping for Debris Flows and Rock Avalanches[R]. Reston, VA:U S Geological Survey. Scientific Investigations Report 2007-5276,2008:22.

[14] 刘希林,莫多闻.泥石流风险评价[M].成都:四川科学技术出版社,2003:17-22. Liu Xilin, Mo Duowen. Debris Flow Risk Assessment[M]. Chengdu: Sichuan Science and Technology Press,2003:17-22.

[15] 刘希林,唐川.泥石流危险性评价[M].北京:科学出版社,1995:1-93. Liu Xilin, Tang Chuan. Debris Flow Risk Assessment[M]. Beijing: Science Press, 1995:1-93.

[16] Guzzetti F, Ardizzone F, Cardinali M,et al. Lan-dslide Volumes and Landslide Mobilization Rates in Umbria, Central Italy[J]. Earth and Planetary Science, 2009, 279:222-229.

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