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四川梓潼金龙村边坡地震稳定性分析
引用本文:刘加才,张战胜. 四川梓潼金龙村边坡地震稳定性分析[J]. 江苏地质, 2014, 38(4): 687-692
作者姓名:刘加才  张战胜
作者单位:江苏省地质工程勘察院
摘    要:金龙村边坡位于四川省梓潼县境内,汶川县东,距离汶川地震中心约150 km。通过现场调查,分析了地形、地貌条件和地震等因素对该边坡稳定性的影响。发现滑动面位于土层与基岩的接触面,采用极限平衡法和数值分析法对边坡的稳定性进行了计算,2种计算得到的稳定性结果较为接近。采用动力时程分析法计算得到了边坡位移与加速度变化的关系。

关 键 词:稳定性评价  地震  变形机制  FLAC软件  强度折减  四川梓潼
收稿时间:2013-11-25
修稿时间:2014-04-03

Analysis on slope seismic stability assessment of Jinlong Village in Zitong of Sichuan
LIU Jia-cai. Analysis on slope seismic stability assessment of Jinlong Village in Zitong of Sichuan[J]. Jiangsu Geology, 2014, 38(4): 687-692
Authors:LIU Jia-cai
Affiliation:LIU Jia-cai,ZHANG Zhan-sheng(1.Geological Engineering Exploration Institute of Jiangsu Province, Nanjing 211102, China; 2. Shandong Zhengyuan Construction Co Ltd, Jinan 250014, China)
Abstract:Jinlong Village landslide was located in Zitong County,Sichuan and approximately 150 km east of Wenchuan. Field investigations indicated that the slope deformation was caused by the combined effects of unfavorable topographic and geological conditions and earthquakes. The sliding surface was along a contact between silty clay and mudstone. Wenchuan earthquake accelerated the creep,causing bulging of the ground surface. The factors of safety( FOS) were calculated using the limit equilibrium method( LEM)and the method of fast Lagrangian analysis of continua in 2 dimensions( FLAC). The results using the LEM indicated that the stability was clearly affected by seismic shaking,and when the PGA grew to 0. 08 g,the slope reached the limit state. The shear failure surface given by numerical simulation developed on the contact between the clay and silty mudstone,which confirmed the assumed the location of sliding surfaces using LEM.
Keywords:Stability assessment   Earthquake   Deformation mechanism   FLAC software   Strength reduction   Zitong, Sichuan
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