Abstract
The Wenchuan Earthquake triggered tens of thousands of landslides and many areas became susceptible to debris flow. From 12th to 14th, August 2010, heavy rain dropped in Wenchuan Earthquake disaster area, Sichuan province, China. The heavy rain triggered simultaneous occurrence of many debris flows in Qingping town in Mianzhu city, resulting in heavy casualty and property loss. Within the range of 4 km in Qingping Segment of Mianyuan River, 11 debris flows occurred simultaneously and the total runout deposits were about 600 × 104 m3 mainly from Wenjia and Zoumaling gully. Field investigation indicated that the sediment supply was mainly derived from landslide deposits. The debris flows could be classified into three types, including gully erosion starting, branch gully starting and source area starting. It is suggested that Wenchuan earthquake areas are still prone to debris flows. Therefore it is important to regulate and restrict use of hazard areas as well as to arrange relocation of people currently living in areas susceptible to debris flows.
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References
Dai FC, Xu C, Yao X, Lu L, Tu XB, Gong QM (2010) Spatial distribution of landslides triggered by the 2008 Ms 8.0 Wenchuan earthquake, China. J Asian Earth Sci 40(4):883–895
Jakob M, Hungr O (2005) Debris-flow hazards and related phenomena. Springer-Praxis, Chichester p 739
Keefer DK (1984) Landslides caused by earthquakes. Geol Soc Am Bull 95:406–421
Koi T, Hotta N, Ishigaki I, Matuzaki N, Uchiyama I, Suzuki M (2008) Prolonged impact of earthquake-induced landslides on sediment yield in a mountain watershed, the Tanzawa region, Japan. Geomorphology 101:692–702
Lin CW, Liu SH, Lee SY, Liu CC (2006) Impacts on the Chi-Chi earthquake on subsequent rain-induced landslides in central Taiwan. Eng Geol 86:87–101
Lin GW, Chen H, Chen YH, Horng MJ (2008) Influence of typhoons and earthquakes on rainfall-induced landslides and suspended sediments discharge. Eng Geol 97:32–41
Parker RN, Densmore AL, Rosser NJ, de Michele M, Li Y, Huang RQ et al (2011) Mass wasting triggered by the 2008 Wenchuan earthquake is greater than orogenic growth. Nat Geosci 4:449–452
Takahashi T (1981) Estimation of potential debris flows and their hazardous zones. J Nat Disaster Sci 3(1):57–89
Tang C, Liang JT (2008) Characteristics of debris flows in Beichuan epicenter of the Wenchuan earthquake triggered by rainstorm on September 24, 2008. J Eng Geol 16(6):751–758 (in Chinese)
Tang C, Zhu J, Ding J et al (2012) An empirical estatistical model for predicting debris-flow runout zones in the Wenchuan earthquake area. Quat Int 250:63–73
Xu Q, Zhang S, Li WL (2012) The 13 August 2010 catastrophic debris flows after the 2008 Wenchuan earthquake, China[J]. Nat Hazards Earth Syst Sci 12:201–216
Yu B, Yang YH, Su YC, Huang WJ, Wang GF (2010). Investigation of the 7 (2010) Zhouqu debris flows. J Eng Geol 18(4):434–444 (in Chinese)
Acknowledgments
This study is financially supported by the National Key Technology R&D Program (2011BAK12B01), the Key Program of National Natural Science of China (No. 41130745), the Young Foundation of National Natural Science of China (No. 41202210) and the Young Foundation of Chengdu University of Technology and the Education Department of Sichuan Province (2010QJ15 &11ZB262).
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Li, W., Huang, R., Tang, C., Xu, Q. (2013). Simultaneous Debris Flows of 13 August 2010 in the Mianyuan River Basin, China. In: Ugai, K., Yagi, H., Wakai, A. (eds) Earthquake-Induced Landslides. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-32238-9_102
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DOI: https://doi.org/10.1007/978-3-642-32238-9_102
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