巴基斯坦北部某大型公路滑坡的形成机理
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作者:
作者单位:

1.中国科学院 山地灾害与地表过程重点实验室;中国科学院、水利部成都山地灾害与环境研究所,成都 610299;2.中国科学院大学,北京 100049;3.中国-巴基斯坦地球科学联合研究中心, 伊斯兰堡,巴基斯坦;4.Poonch Rawalakot大学,Rawalakot12350,巴基斯坦;5.Azad Jammu and Kashmir大学,Muzaffarabad13100,巴基斯坦

作者简介:

ASGHAR Aamir, PhD candidate, main research interests: assessment of landslide hazards, E-mail: aamirasghar@ imde.ac.cn.

通讯作者:

SU Lijun (corresponding author), professor, doctoral supervisor, E-mail: sulijun1976@163.com.

中图分类号:

P642.22

基金项目:


Formation mechanisms of a massive highway landslide in northern Pakistan
Author:
Affiliation:

1.Key Laboratory of Mountain Hazards and Earth Surface Process; Institute of Mountain Hazards and Environment, Chinese Academy of Sciences (CAS), Chengdu610299, P. R. China;2.University of Chinese Academy of Sciences, Beijing100049, P. R. China;3.China-Pakistan Joint Research Center on Earth Sciences, Islamabad, Pakistan;4.The University of Poonch Rawalakot, Rawalakot12350, Pakistan;5.The University of Azad Jammu and Kashmir, Muzaffarabad13100, Pakistan

Fund Project:

National Natural Science Foundation of China (No. U22A20603); Strategic Priority Research Program of the Chinese Academy of Sciences (No. XDA20030301)

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    摘要:

    滑坡是山区公路安全运行的重要威胁,开展滑坡灾害评估尤为重要,尤其是深切峡谷区域的公路滑坡。以巴基斯坦北部Muzaffarabad-Mansehra公路沿线某大型滑坡为研究对象,采用野外调查、遥感分析、地貌解译、地球物理探勘和运动学分析等多种调查手段,进行滑坡的失稳特征、触发机理、地下结构特征和边坡稳定评估等研究,结果表明:滑坡发生在Hazara地层中,该地层以顺层斜坡为主,容易发生翘曲变形等破坏,属于滑坡易发地层。地球物理探勘表明:滑坡体内部存在多个不同深度和厚度的复杂结构,低电阻率区(0.325~1 350 Ω·m)以松散、饱水的堆积体为主,高电阻率区域(1 510~26 092 Ω·m)与覆盖层有关,包括冲积层、巨石和干板岩碎片等。地震反射层分析结果表明,在高度饱和的覆盖层、改造区块和表层风化层内,P波速度较低(400~1 800 m/s);而下垫层散布着高密度岩石碎片和大块巨石,P波速度为3 000~5 000 m/s。两种地球物理探勘结果均表明滑坡体内有一条延伸30 m深的破碎带,这是触发滑坡的重要因素。滑坡顶部的滑动面在深度25~30 m处,主体处的滑动面深度在45 m处。运动学分析表明:锲形体失稳是公路滑坡的主要破坏模式。研究结果表明,采用综合技术分析滑坡灾害的潜在机制可以有效减轻此类灾害带来的相关风险。

    Abstract:

    Assessment of landslide hazards is important in highway engineering especially considering the landslide hazards along challenging roads; more research is needed to understand progressive strategies. Therefore, multidisciplinary and advanced methodologies were needed to assess the formation mechanisms and stability of complex landslides on the Muzaffarabad-Mansehra Highway in northern Pakistan. The main study objectives were to investigate slope failures, identify the triggering mechanism of layered rocks, image subsurface geometrical configurations, and assess slope stability factors using field operations, remote-sensing tools, geomorphological mapping, geophysical imaging, and kinematics analysis. The findings indicate that the foliated Hazara Formation, being buckled easily, is particularly susceptible to the geo-environmental conditions that triggered the landslide. Geophysical surveys revealed multiple layers of varying depth and thickness, highlighting the complexity of the landslide. Low resistivity zones (0.325-1 350 Ω·m) indicated the presence of un-onsolidated, water-saturated materials and highly sheared substances, whereas high resistivity zones (1 510-26 092 Ω·m) were associated with overburden, including alluvium, boulders, and dry slate fragments. Seismic refraction tomography indicated low P-wave velocities (400-1 800 m/s) within highly saturated overburdens, reworked blocks, and surficial weathering. The subsurface layers are interspersed with fragmented pieces of high-density rock and massive boulders, displaying P-wave velocities within the range of 3 000-5 000 m/s. Both tomographic methods revealed a fracture zone extending 30 m depth, which poses a significant risk of catastrophic occurrences. The sliding surface was found to be 25-30 meters depth at the crown and 45 meters depth in the main body. Kinematic analysis identified wedge failure as the primary failure mode along highway cuts. The findings of this study demonstrate the significance of employing integrated techniques to analyze the underlying mechanics of landslide hazards within the context of highway engineering. Furthermore, these integrated procedures are highly advantageous in efficiently eliminating the associated risks posed by such hazards.

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ASGHAR Aamir,苏立君,赵波,NIAZ Abrar, ULLAH Faheem.巴基斯坦北部某大型公路滑坡的形成机理[J].土木与环境工程学报(中英文),2024,46(6):51-69. ASGHAR Aamir, SU Lijun, ZHAO Bo, NIAZ Abrar, ULLAH Faheem. Formation mechanisms of a massive highway landslide in northern Pakistan[J]. JOURNAL OF CIVIL AND ENVIRONMENTAL ENGINEERING,2024,46(6):51-69.10.11835/j. issn.2096-6717.2023.131

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  • 收稿日期:2023-07-04
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  • 在线发布日期: 2024-11-27
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