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强地震作用引起的近断层地表破裂分 析方法:逆断层 ANAPPROACHTOEVALUATEGROUNDSURFACERUPTURECAUSED BYREVERSALFAULTMOVEMENT 赵纪生1,2陶夏新1,3师黎静1 1.中国地震局工程力学研究所(InstituteofEngineeringMechanics,ChinaEarthquakeAdministration) 2.中国科学院国家冻土工程重点试验室(StateKeyLaboratoryofFrozenSoilEngineering,CAREERI,CAS) 3.哈尔滨工业大学土木工程学院(SchoolofcivilEngineering,HarbinInstituteofTechnology) 2006.3 CONTENT •OVERVIEW •METHODOLOGY •ONSETOFSTRAINLOCALIZATION •EVOLUTIONOFSLIPPAGELINE •CONSTITUTIVEMODEL •INPUTOFTHEPROBLEM •EXAMPLESANDDISCUSSIONS •SOMEPROBLEMS 1.OVERVIEW •PhenomenaofSurfaceRupture --Mostsurfaceruptureisconfinedtoarelativelynarrow zoneafewfeettoafewtensoffeetwide. --insomecasesprimarysurfacerupturealongbranch faultscanbedistributedacrosszoneshundredsoffeet wideormanifestedasbroadwarps •CasualtyandEconomicalDamage TheCountermeasure •reinforcestructure? --takemeasurestoaccommodatewarpingand distributivedeformation •Awayformwheresurfacerupturemaytakeplace --definesetbackdistances EstimationofScaleofSurface •RuptureEmpiricalformulaebasedonearthquake investigation; •NumericalmethodbasedonMechanics StrongFormofAnalysisModel WeakFormofAnalysisModel KeyPoints •SomeConcepts •DetectOnsetConditionoftheRupture •EvolutionPropertiesoftheRupture •ConstitutiveEquationofStressedSoils •NumericalMethod StabilityorFailureofMaterials Stationarywave,Flutter Positivenessofthesecondorderpowerofmaterials, theuniquenessofsolutionofgoverningequations, thebifurcationvariationalprinciples. Bifurcation, Unstable Weakdiscontinuity---strain Strongdiscontinuity---displacementFailure OnsetandEvolutionoftheRupture ConstitutiveEquation(Intact) ConstitutiveEquation(Interface) NumericalMethods •LEM(LocalEnrichmentMethods) •Multigrid-likeprocedures •Generalizedmathematicalhomogenizationtheory •Multiscaleenrichmentbasedonpartitionofunity method •Meshfree •XFEM+PU •XFEM+LevelSet TwostepsandOnestep •Onsetoftheslipline •Evolutionoftheline •Onset+Evolutionoftheline 2.METHODOLOGY •Elasto-plasticsoilbodyunderdislocation •