汶川地震崩滑灾害影响因素分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
为研究汶川地震崩滑灾害主要影响因素,在掌握汶川地震灾区公路沿线地震崩滑灾害资料基础上,选取典型段进行灾害统计分析,研究表明动力条件下斜坡失稳主要受斜坡岩体结构特征、地震动峰值加速度和斜坡动力响应特征三方面因素影响。地震动峰值加速度越高,地震崩滑灾害越发育。斜坡动力响应特征主要取决于地形地貌和地层岩性,陡坡硬岩段为地震崩滑灾害高发区。斜坡岩体结构是控制斜坡变形破坏的主要因素,从研究斜坡动力失稳角度,提出了斜坡岩体结构类型的划分,分为土层及强风化层——基岩二元结构、块状结构、层状及似层状结构、碎裂结构、土层等5个大类12个亚类。
Based on the investigation information along the highway with a total length about 3 200km in the earthquake area,through statistical analysis of typical sections,study the influence factors of earthquake induced landslides and rock falls.The study shows that the earthquake induced slope failure mainly influenced by three factors,that is slope geological structure,Peak ground acceleration and response feature of slope to the earthquake.The higher of peak acceleration of ground motion,the earthquake induced landslides and collapse were more developed.response feature of slope to the earthquake are depends on the topography and stratum lithologies,the steep and hard rock slope are the high incidence areas of seismic geo-hazards.Under the dynamic conditions,the slope structures are also the main control factors to the deformation and destroy of the slope.For the study of slope dynamic instability,five geologic structure models are put forward.There are rock-soil and strong weathered rock structure,block structure,layered structure and quasi-lamellar structure,cataclastic texture,soil layers,and twelve sub geologic structure models.
引文
[1]唐永建,庄卫林,吉随旺,等.“5.12”汶川大地震四川灾区公路应急调查与抢通[M].北京:人民交通出版社,2008:1-15.TANG Yongjian,ZHUANG Weilin,JI Suiwang,et al.Emergency investigation and reopened of Sichuan highwayin"5.12"Wenchuan Earthquake[M].Beijing:ChinaCommunications Press,2008:1-15.
    [2]吉随旺,唐永建,胡德贵,等.四川省汶川地震灾区干线公路典型震害特征分析[J].岩石力学与工程学报,2009,28(6):1250-1260.JI Suiwang,TANG Yongjian,HU Degui,et al.Analysis oftypical seismic damages of highways in Wenchuanearthquake-induced hazard areas in Sichuan province[J].Chinese Journal of Rock Mechanics andEngineering,2009,28(6):1 250-1 260.
    [3]殷跃平.汶川八级地震地质灾害研究[J].工程地质学报,2008,16(4):433-444.YIN Yueping.Researches on the Geo-hazards triggeredby Wenchuan earthquake,Sichuan[J].Journal ofEngineering Geology,2008,16(4):433-444.
    [4]王秀英,聂高众,王登伟.汶川地震诱发滑坡与地震动峰值加速度对应关系研究[J].岩石力学与工程学报,2010,29(1):82-89.WANG Xiuying,NIE Gaozhong,WANG Dengwei.Research on relationship between landslides and peakground accelerations induced by Wenchuan earthquake[J].Chinese Journal of Rock Mechanics andEngineering,2010,29(1):82-89.
    [5]祁生文,许强,刘春玲,等.汶川地震极重灾区地质背景次生斜坡灾害空间发育规律[J].工程地质学报,2009,17(1):39-49.QI Shengwen,XU Qiang,LIU Chunling,et al.Slopeinstabilities in the severest disaster areas of Wenchuanearthquake[J].Journal of Engineering Geology,2009,17(1):39-49.
    [6]李秀珍,孔纪名,崔云,等.汶川地震滑坡与地震参数及地质地貌因素之间的相关关系[J].工程地质学报,2010,18(1):8-14.LI Xiuzhen,KONG Jiming,CUI Yun,et al.Statisticalrelations between landslides induced by Wenchuanearthquake and earthquake parameters,geological as wellas geomorphological factors[J].Journal of EngineeringGeology,2010,18(1):8-14.
    [7]BURCHFIEL B C,CHEN Z,LIU Y,et al.Tectonics ofthe Longmenshan and adjacent regions[J].InternationalGeology Review,1995,37(8):661-735.
    [8]谷德振.岩体工程地质力学基础[M].北京:科学出版社,1979:198-247.GU Dezhen.Foundation of rockmass engineeringgeomechanics[M].Beijing:Science Press,1979:198-247.
    [9]孙广忠.岩体结构力学[M].北京:科学出版社,1988:182-251.SUN Guangzhong.Rockmass structural mechanics[M].Beijing:Science Press,1988:182-251.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心