An integrated geophysical approach for investigating hydro-geological characteristics of a debris landslide in the Wenchuan earthquake area

被引:63
|
作者
Su, Li-jun [1 ,2 ,4 ]
Xu, Xing-qian [1 ,3 ,4 ]
Geng, Xue-yu [5 ,6 ]
Liang, Shuang-qing [1 ,4 ]
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Earth Surface Proc, Chengdu 610041, Sichuan, Peoples R China
[2] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[3] Yunnan Agr Univ, Coll Water Conservancy, Kunming 650201, Yunnan, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[5] Univ Warwick, Sch Engn, Coventry CV4 7AL, W Midlands, England
[6] Qingdao Technol Univ, Sch Civil Engn, Qingdao 266033, Shandong, Peoples R China
关键词
Hydro-geology; Pipe-network seepage system; Debris landslides; Geophysical investigation; Wenchuan earthquake; GROUND-PENETRATING RADAR; MULTICHANNEL ANALYSIS; FRENCH ALPS; SWISS ALPS; SURFACE; SLOPE; RESISTIVITY; FRANCE; CHINA; MODEL;
D O I
10.1016/j.enggeo.2016.11.020
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Debris landslides are one of the most widely distributed types of landslides in the Wenchuan earthquake area. The hydro-geological structure characteristics are the fundamental basis for stability evaluation, performing protection and administration of a landslide. The rock and soil mass of a debris landslide was highly non-uniform and preferential seepage paths were normally developed in it. Therefore, in situ identification of the underground water seepage system became particularly important. Recently, investigations on the seepage paths of underground water in debris landslides were restricted to indoor model testing and site observation, which were far from meeting the actual demand for landslide prevention and mitigation. To locate the seepage paths, we conducted survey work on a debris landslide seated in the Xishan Village, Li County, Sichuan Province, China, by combing four different geophysical methods. They were multichannel analysis of surface wave (MASW), electrical resistivity tomography (ERT), ground penetrating radar (GPR) and microtremor survey method (MSM). The geophysical interpretation was verified with field engineering surveys and monitoring data. The results suggested that a dendritic pipe-network seepage system usually developed in debris landslides. Varisized infiltration pipes showed the characteristics of inhomogeneity and concentration of the seepage. This work highlighted that geophysical parameters (shear wave velocity Vs, dielectric constant epsilon and resistivity value rho) could provide reliable qualitative and quantitative information about the colluvial layer, bedrock interface, potential sliding surface and underground water seepage system of a landslide. The optimum combination of geophysical methods was suitable to survey the hydro-geological characteristics of debris landslides in the Wenchuan earthquake area. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:52 / 63
页数:12
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  • [1] Characteristics of rainfall responsible for debris flows in Wenchuan Earthquake area
    Guo, Xiaojun
    Cui, Peng
    Marchi, Lorenzo
    Ge, Yonggang
    [J]. ENVIRONMENTAL EARTH SCIENCES, 2017, 76 (17)
  • [2] Characteristics of rainfall responsible for debris flows in Wenchuan Earthquake area
    Xiaojun Guo
    Peng Cui
    Lorenzo Marchi
    Yonggang Ge
    [J]. Environmental Earth Sciences, 2017, 76
  • [3] Characteristics and countermeasures of debris flow in Wenchuan area after the earthquake
    Cui, Peng
    Zhuang, Jian-Qi
    Chen, Xing-Chang
    Zhang, Jian-Qiang
    Zhou, Xiao-Jun
    [J]. Sichuan Daxue Xuebao (Gongcheng Kexue Ban)/Journal of Sichuan University (Engineering Science Edition), 2010, 42 (05): : 10 - 19
  • [4] The spatial distribution characteristics of shallow fissures of a landslide in the Wenchuan earthquake area
    Xing-qian Xu
    Li-jun Su
    Chao Liu
    [J]. Journal of Mountain Science, 2016, 13 : 1544 - 1557
  • [5] The spatial distribution characteristics of shallow fissures of a landslide in the Wenchuan earthquake area
    XU Xing-qian
    SU Li-jun
    LIU Chao
    [J]. Journal of Mountain Science, 2016, 13 (09) : 1544 - 1557
  • [6] The spatial distribution characteristics of shallow fissures of a landslide in the Wenchuan earthquake area
    Xu Xing-qian
    Su Li-jun
    Liu Chao
    [J]. JOURNAL OF MOUNTAIN SCIENCE, 2016, 13 (09) : 1544 - 1557
  • [7] The June 2017 Maoxian landslide:Geological disaster in an earthquake area after the Wenchuan Ms 8.0 earthquake
    YIN YuePing
    WANG WenPei
    ZHANG Nan
    YAN JingKai
    WEI YunJie
    [J]. Science China(Technological Sciences), 2017, 60 (11) : 1762 - 1766
  • [8] The June 2017 Maoxian landslide: Geological disaster in an earthquake area after the Wenchuan Ms 8.0 earthquake
    Yin YuePing
    Wang WenPei
    Zhang Nan
    Yan JingKai
    Wei YunJie
    [J]. SCIENCE CHINA-TECHNOLOGICAL SCIENCES, 2017, 60 (11) : 1762 - 1766
  • [9] The June 2017 Maoxian landslide:Geological disaster in an earthquake area after the Wenchuan Ms 8.0 earthquake
    YIN YuePing
    WANG WenPei
    ZHANG Nan
    YAN JingKai
    WEI YunJie
    [J]. Science China Technological Sciences, 2017, (11) : 1762 - 1766
  • [10] The June 2017 Maoxian landslide: Geological disaster in an earthquake area after the Wenchuan Ms 8.0 earthquake
    YuePing Yin
    WenPei Wang
    Nan Zhang
    JingKai Yan
    YunJie Wei
    [J]. Science China Technological Sciences, 2017, 60 : 1762 - 1766