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时间:2020-03-25
《映秀—卧龙公路沿线汶川地震地质灾害研究.pdf》由会员上传分享,免费在线阅读,更多相关内容在行业资料-天天文库。
1、JournalofEngineeringGeology工程地质学报1004-9665/2010/18(2)一0160—08映秀一卧龙公路沿线汶川地震地质灾害研究程强吴事贵苏玉杰(四川省交通厅公路规划勘察设计研究院成都610041)摘要映秀一卧龙公路是汶川地震灾区距震中最近、震害最为严重的一条公路,本文对沿线地震地质灾害进行了详细的调查研究。依据震害特征,将沿线震害划分为斜坡中上部强风化岩体及土层失稳、结构面切割岩体崩滑失稳、滑坡、泥石流等4类,并分析了沿线震害发育规律。调查表明:龙门山后⋯断裂两侧地震地质灾害呈现显著的差异性,主要是由深大断裂的消震隔震效应,地
2、貌放大效应,地质结构等三方面因素决定的。通过134条实测剖面分析,研究了地震失稳斜坡坡度和失稳部位。地震诱发失稳斜坡坡度在33。~84。之间,主要分布在41。~65。之间,可以认为地震诱发斜坡失稳灾害主要发生在4o。以上的斜坡。斜坡失稳部位主要分布在斜坡中上部以及地貌突出部位,主要失稳部位在0.4坡高以上。从研究斜坡动力失稳的角度,将沿线斜坡划分为基岩一土层及强风化层斜坡地质结构、不利外倾结构面基岩斜坡地质结构、块状构造基岩斜坡地质结构、块碎石土层斜坡地质结构等几种地质结构模型,分析论述了各种地质结构相应的地震地质灾害类型及特点。关键词汶川地震地震地质灾害斜坡
3、地质结构模型失稳坡度失稳部位影响因素中图分类号:P65文献标识码:AGEoLoGICALHAZARDSDUEToWENCHUANEARTHQUAKEALoNGYINGXIUTOWOLoNGHIGHWAYCHENGQiangWUShiguiSUYujie(SichuanProvincialCommunicationDepartmentHighwayPlanningSurveyDesignResearchImtit~e,Chengdu610041)AbstractThehighwayfromYingxiutowntoWolongtownisthenearesthi
4、ghwaytotheepicenterofWenehuanEaahquake.Thegeo—hazardslonganddamagetothehighwayarethemostserious.Thispaperpresentsacompre-hensiveinvestigationofthegeologicalhazardsduetotheea~hquakealongthehighway.Basedontheircharacteris—tics,thegeo—hazardsaredividedintofourtypes.Theyareinstabilityof
5、highlyweatheredrockmassandsoilontheupperpartoftheslopes,instabilityofrockmasscutbygeologicalstructuralsurface,landslidesanddebrisflows.Itanalyzesthedevelopmentallawofgeo—hazardsalongthehighway.Thegeo—hazardsshowsignificantdeviationsbe—tweenthetwosidesofthebackrangefaultsattheLongmen
6、Mountainfaultzone.Thereasonsaretheseismicisola—tionefectofthedeepfracture,scalingefectofthelandforms,andgeologicstructures.Theslopesteepnessandpo—sitionofseismicinstabilitieshavebeenstudiedviatheanalysisof134geologicalsections.Theresultsshowthattheslopesteepnessofseismicinstabilitie
7、saredistributedwithintherangeoffrom33。to84。.mainlyfrom40。to65。.So,itcanbeconcludedthatthegeo—hazardscausedbytheearthquakemainlytookplaceontheroadslopessteeperthan40。.Thefailurezonescausedbyseismicforcemainlydistributedontheupsideoftheroadslopes.Theinsta—bilitypositionsaremainlyupont
8、hepaaswithslopegrad
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