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青海八大山滑坡群形成机制及稳定性评价研究

STUDY ON FORMATION MECHANISM AND STABILITY EVALUATION OF BADASHAN LANDSLIDE GROUP IN QINGHAI PROVINCE

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【作者】 崔芳鹏胡瑞林谭儒蛟杨坤于进庆张明王立朝李雄

【Author】 CUI Fangpeng1,HU Ruilin1,TAN Rujiao1,YANG Kun2,YU Jinqing1, ZHANG Ming1,WANG Lichao3,LI Xiong4 (1. Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2. College of Natural Resources and Environmental Engineering,Shandong University of Science and Technology, Qingdao,Shandong 266510,China;3. China Institute of Geoenvironmental Monitoring,Beijing 100081,China; 4. Baili Engineering Technology Limited Company,Yueyang,Hunan 414007,China)

【机构】 中国科学院地质与地球物理研究所工程地质力学重点实验室山东科技大学资源与环境工程学院中国地质环境监测院湖南百利工程科技有限公司勘察分公司 北京100029北京100029山东青岛266510北京100081湖南岳阳414007

【摘要】 在对青海八大山滑坡群进行现场勘查、室内试验和相关论证的基础上,阐述该滑坡群的基本特征和形成机制,并运用极限平衡分析法和数值模拟对该滑坡群在预设不同工况下的稳定性进行计算和评价;同时,对与750kV官亭—兰州东输电线路塔基稳定性关系密切的滑坡H3,H4,H5进行重点研究。研究结果表明,天然状态下,滑坡H3,H4,H5的整体稳定性系数均大于1.10,处于基本稳定及稳定状态,该状态下的20#,21#,22#塔基稳定性可满足要求;在暴雨工况下,滑坡H3的稳定性系数略小于1.05,处于欠稳定状态,滑坡H4处于基本稳定状态,而滑坡H5仍然处于稳定状态。受此影响,20#塔基安全性受到威胁,而21#,22#塔基仍可满足稳定要求;在烈度为VII度地震状态下,滑坡H3,H4,H5的稳定性系数均小于1.0,处于不稳定状态,20#,21#,22#塔基的稳定性也因此而无法得到保障。此外,敏感性分析结果表明,滑体内摩擦角是影响滑坡群稳定性的最敏感因素。最后,基于滑坡形成机制和定量评价结果,提出为提高滑坡稳定性应采取的工程加固措施,为输电线路的安全运行提供了物质保障,具有较高的实践和理论意义。

【Abstract】 Based on field investigation,indoor test and related studies of Badashan landslide group,the basic characteristics and formation mechanism are elaborated. According to different presupposed working conditions, the stability is calculated and evaluated by adopting limit equilibrium analysis method and numerical simulation. At the same time,landslides H3,H4 and H5,which are closely related with tower ground stability of 750 kV transmission line from Guanting to Lanzhou are mainly considered. The results show that coefficients of integral stability of landslides H3,H4 and H5 are all greater than 1.10,and therefore these landslides are under steady state in natural state. As a result,stabilities of towers No.20,21 and 22 can be satisfied. Under rainstorm state,stability coefficient of landslide H3 is slightly less than 1.05 and therefore it is under metastable state. In addition, landslides H4 and H5 are under stable state. As a result,stabilities of towers No.21,22 except for 20 can besatisfied. Under seismic loading with magnitude VIII,stability coefficients of landslides H3,H4 and H5 are all less than 1.0 and therefore they are unstable. As a result,stabilities of towers No.20,21 and 22 can not be satisfied. What′s more,sensibility analysis of stability influencing parameters on landslides H3,H4 and H5 is carried out. The analytical result shows that internal friction angle of landslide mass is the most sensitive factor that influences the landslide stability. Finally,relevant engineering strengthening measures are provided based on formation mechanism;and quantitative evaluation results of the landslides group to guarantee safe operation of the transmission line are presented. Therefore,the results are of great significance in practice.

【基金】 “十一五”国家科技支撑计划项目(2006BAC04B02);国家重点基础研究发展规划(973)项目(2002CB412702)
  • 【文献出处】 岩石力学与工程学报 ,Chinese Journal of Rock Mechanics and Engineering , 编辑部邮箱 ,2008年04期
  • 【分类号】P642.22
  • 【被引频次】29
  • 【下载频次】506
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