岩土材料质量分布与变形之间的相互作用原理(第2版)

岩土材料质量分布与变形之间的相互作用原理(第2版)
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作者:
出版社: 科学出版社
2013-12
版次: 2
ISBN: 9787030389060
定价: 56.00
装帧: 平装
开本: 16开
纸张: 胶版纸
页数: 147页
正文语种: 简体中文
分类: 工程技术
  •   Rockandsoilarethemajorconstituentmaterialsofthelithosphereoftheearth.Theyarealsothemostwidelyusedengineeringmaterials.Rockandsoilexhibitsomeremarkablecharacteristicsofdeformationandstrengthbehavior,suchasthepressuresensitivity(orpressuredependency),sheardilatancy,dependencyofstresspathetc.Thetwophenomenaofpressuresensitivityandsheardilatancyhavelongbeenknownbypeople.However,theiroriginofgenerationisnotexplainedrationallyyet. Prefacetothesecondedition
    Prefacetothefirstedition

    Chapter1IntroductiontoContinuumMechanics
    1.1Thedefinitionofacontinuum
    1.2Deformation
    1.3Stress
    1.4Velocityfields
    1.5Theclassicalconservationlawsandfieldequations
    1.5.1LagrangeandEulerdescriptionsofthemotionofacontinuum
    1.5.2Theequationofcontinuity
    1.5.3Theequationsofmotion
    1.5.4Momentofmomentum

    Chapter2FundamentalsofThermodynamics
    2.1Introduction
    2.2Basicconceptsofthermodynamics
    2.3Temperatureandthezerothlawofthermodynamics
    2.4Energy
    2.5Thefirstlawofthermodynamics
    2.6Thesecondlawofthermodynamics
    2.7Reversibleandirreversibleprocesses
    2.8EntropyandClausius-Duheminequality
    2.9Internalvariablesandaccompanyingequilibriumstate

    Chapter3FundamentalCharacteristicsofDeformationBehaviorforGeotechnicalMaterials
    3.1Introduction
    3.2Pressuresensitivity
    3.3Sheardilatancy
    3.4Dependencyofstresspath

    Chapter4ConstitutiveModelingforGeotechnicalMaterials
    4.1Introduction
    4.2Theplasticpotentialtheory
    4.3Theapproachbasedonthethermodynamicsofirreversibleprocesses
    4.4Thecriticalstateandcriticalstateline
    4.4.1Criticalstate
    4.4.2Criticalstateline

    Chapter5ThePrincipleofInteractionbetweenPlasticVolumetricandShearStrains
    5.1Background
    5.2Theprincipleofinteractionbetweenplasticvolumetricandshearstrains
    5.3Effectsoftheplasticshearstrainonplasticvolumetricstrains
    5.4Effectsoftheplasticvolumetricstrainonplasticshearstrains
    5.5Thephysicalmeaningoftheprincipleofinteraction

    Chapter6SymmetryandInteractionbetweenPlasticVolumetricandShearStrainFields
    6.1Introductiontothegaugefieldtheory
    6.2Symmetriesofplasticstrainfields
    6.2.1Introductiontotransformationgroups
    6.2.2Thelocalsymmetriesofplasticstrainfieldsandconstitutivefieldequations
    6.3Characteristicsoftheinteractionbetweenmassdistributionanddeformation
    6.4Summary

    Chapter7TheMechanismofGenerationofDependencyofStressPathandCriticalStateLine
    7.1Thedependencyofstresspath
    7.2Thecurvaturehardening
    7.3Thecriticalstateline

    Chapter8TheConstitutiveEquationsforGeotechnicalMaterials
    8.1Theobjectiveofconstitutivemodeling
    8.2Quantitativerepresentationoftheinteractionbetweenplasticvolumetricandshearstrains
    8.3Thermodynamicvariablesandstatepotential
    8.4Dissipationfunctional
    8.5Theconstitutiveequationsforgeotechnicalmaterials

    Chapter9DamagesofEngineeringandGeotechnicalMaterials
    9.1Themechanismofdamageofmetalsandsomeengineeringmaterials
    9.2Thedamageofgeotechnicalmaterials
    9.3Thedescriptionofdamageevolution

    Chapter10TheNumericalMethodofConstitutiveModelingforGeoteehnicalMaterials
    10.1Introduction
    10.2Thenumericalmethodofconstitutivemodeling
    10.3Plasticity-basedmodelsforclayandsandunderdifferentstresspaths
    10.4Concludingremarks

    Chapter11TheInteractionbetweenMassDistributionandDeformationinUnsaturatedSoils
    11.1Introduction
    11.2Theinteractionbetweenplasticvolumetricandshearstrainsinunsaturatedsoils
    11.3Thedualpropertyofmatricsuction
    11.4Theshearstrengthofunsaturatedsoils
    11.5Theconstitutivefieldequationsforunsaturatedsoils
    11.6Thedependencyofstresspathandcriticalstatelineinunsaturatedsoils
    References
    Index
  • 内容简介:
      Rockandsoilarethemajorconstituentmaterialsofthelithosphereoftheearth.Theyarealsothemostwidelyusedengineeringmaterials.Rockandsoilexhibitsomeremarkablecharacteristicsofdeformationandstrengthbehavior,suchasthepressuresensitivity(orpressuredependency),sheardilatancy,dependencyofstresspathetc.Thetwophenomenaofpressuresensitivityandsheardilatancyhavelongbeenknownbypeople.However,theiroriginofgenerationisnotexplainedrationallyyet.
  • 目录:
    Prefacetothesecondedition
    Prefacetothefirstedition

    Chapter1IntroductiontoContinuumMechanics
    1.1Thedefinitionofacontinuum
    1.2Deformation
    1.3Stress
    1.4Velocityfields
    1.5Theclassicalconservationlawsandfieldequations
    1.5.1LagrangeandEulerdescriptionsofthemotionofacontinuum
    1.5.2Theequationofcontinuity
    1.5.3Theequationsofmotion
    1.5.4Momentofmomentum

    Chapter2FundamentalsofThermodynamics
    2.1Introduction
    2.2Basicconceptsofthermodynamics
    2.3Temperatureandthezerothlawofthermodynamics
    2.4Energy
    2.5Thefirstlawofthermodynamics
    2.6Thesecondlawofthermodynamics
    2.7Reversibleandirreversibleprocesses
    2.8EntropyandClausius-Duheminequality
    2.9Internalvariablesandaccompanyingequilibriumstate

    Chapter3FundamentalCharacteristicsofDeformationBehaviorforGeotechnicalMaterials
    3.1Introduction
    3.2Pressuresensitivity
    3.3Sheardilatancy
    3.4Dependencyofstresspath

    Chapter4ConstitutiveModelingforGeotechnicalMaterials
    4.1Introduction
    4.2Theplasticpotentialtheory
    4.3Theapproachbasedonthethermodynamicsofirreversibleprocesses
    4.4Thecriticalstateandcriticalstateline
    4.4.1Criticalstate
    4.4.2Criticalstateline

    Chapter5ThePrincipleofInteractionbetweenPlasticVolumetricandShearStrains
    5.1Background
    5.2Theprincipleofinteractionbetweenplasticvolumetricandshearstrains
    5.3Effectsoftheplasticshearstrainonplasticvolumetricstrains
    5.4Effectsoftheplasticvolumetricstrainonplasticshearstrains
    5.5Thephysicalmeaningoftheprincipleofinteraction

    Chapter6SymmetryandInteractionbetweenPlasticVolumetricandShearStrainFields
    6.1Introductiontothegaugefieldtheory
    6.2Symmetriesofplasticstrainfields
    6.2.1Introductiontotransformationgroups
    6.2.2Thelocalsymmetriesofplasticstrainfieldsandconstitutivefieldequations
    6.3Characteristicsoftheinteractionbetweenmassdistributionanddeformation
    6.4Summary

    Chapter7TheMechanismofGenerationofDependencyofStressPathandCriticalStateLine
    7.1Thedependencyofstresspath
    7.2Thecurvaturehardening
    7.3Thecriticalstateline

    Chapter8TheConstitutiveEquationsforGeotechnicalMaterials
    8.1Theobjectiveofconstitutivemodeling
    8.2Quantitativerepresentationoftheinteractionbetweenplasticvolumetricandshearstrains
    8.3Thermodynamicvariablesandstatepotential
    8.4Dissipationfunctional
    8.5Theconstitutiveequationsforgeotechnicalmaterials

    Chapter9DamagesofEngineeringandGeotechnicalMaterials
    9.1Themechanismofdamageofmetalsandsomeengineeringmaterials
    9.2Thedamageofgeotechnicalmaterials
    9.3Thedescriptionofdamageevolution

    Chapter10TheNumericalMethodofConstitutiveModelingforGeoteehnicalMaterials
    10.1Introduction
    10.2Thenumericalmethodofconstitutivemodeling
    10.3Plasticity-basedmodelsforclayandsandunderdifferentstresspaths
    10.4Concludingremarks

    Chapter11TheInteractionbetweenMassDistributionandDeformationinUnsaturatedSoils
    11.1Introduction
    11.2Theinteractionbetweenplasticvolumetricandshearstrainsinunsaturatedsoils
    11.3Thedualpropertyofmatricsuction
    11.4Theshearstrengthofunsaturatedsoils
    11.5Theconstitutivefieldequationsforunsaturatedsoils
    11.6Thedependencyofstresspathandcriticalstatelineinunsaturatedsoils
    References
    Index
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