Lecture 4 - Cam Clay

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    Critical-State Soil Models

    Department of Civil and Envir. Eng., Rensselaer Polytechnic Institute, Troy, NY

    April, 2014

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    Critical-State Soil Mechanics

    Developed by Roscoeand others at Cambridge inthe fifties

    Some Useful Literature:

    Schofield, A., & Wroth, P. (1968). Critical state soil mechanics.

    Wood, D. (1990). Soil behaviour and critical state soil mechanics.Cambridge University Press.

    Helwany, S. (2007).Applied soil mechanics with ABAQUS applications.John Wiley & Sons.

    Is an effective stress framework for describing soilresponse

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    Critical-State Soil Mechanics

    Critical State models tie together:

    1. Behavior of confining pressure (p)2. Behavior of deviatoric stress (q)

    3. Behavior of volume changes (e)

    Introduce concept of critical state of soils:

    State at which shear strains occur without furtherchanges in confining stress, deviatoric stress orvolume.

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    Critical-State Models Some Critical State Soil Models:

    Granta Gravel

    Cam Clay Modified Cam Clay

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    Prevosts Multi-surface Modified Cam-Clay

    Prevosts Multi-surface Modified Cam-Clay

    Kinematic hardening Isotropic hardening

    Multiple yield surfaces Yield surface and Critical Statesurface

    Yield surfaces not capped Capped yield surfaces

    Yield surface size independent of e Dependency on e

    Ignores OCR Accounts for OCR effect

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    Kinematic Hardening

    xz

    xyxy

    xz

    xy

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    Isotropic Hardening

    b

    a

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    Isotropic Hardening

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    Normal Consolidation Line and

    UnloadingReloading Lines

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    Normal Consolidation Line and

    UnloadingReloading Lines

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    Normal Consolidation Line and

    UnloadingReloading Lines

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    Critical-State

    Critical state: State at

    which shear stress

    application leads tono volume change as

    the soil is continually

    sheared.

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    Critical-State

    p (kPa)

    CSL M

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    Critical-State Line

    Elastic Yielding

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    Critical-State Line in e-p-q space

    3D Figure

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    Parameters for formulation

    or

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    Parameters for formulation

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    Inside the field surface (Elastic state)

    Elastic but

    NOT linear

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    Soil Plasticity

    Flow Rule: Describes the direction of the

    vector of plastic strain increment

    Hardening Law: Relates the magnitude of a

    plastic strain to the magnitude of an

    increment of stress as the stress traverses the

    yield surface and the material hardens

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    Yield Surface

    Yield Surface: Separates states of stress which cause only elastic

    strains from states of stress that cause plastic (and elastic) strains

    Preconsolidation Pressure

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    Plastic Strains

    Definitions:

    des:Deviatoric Elastic strain increment

    dp

    s:Deviatoric Plastic strain incrementds= d

    es+ dps

    dev:Volumetric Elastic strain incrementdpv: Volumetric Plastic strain increment

    dv= dev+ d

    pv

    0

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    Volumetric Strains

    Derived from isotropicconsolidation test:

    also:

    Differentiating:

    Elastic Volumetric

    Strains Plastic VolumetricStrains

    Total Volumetric Strains

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    Deviatoric Plastic Strains Cam Clay Model assumes an associatedflow rule

    controlled by the shape of the yield surface:

    Stress increment has same direction as strain increment

    These increments are perpendicular to the yield surface

    (normality rule)

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    Deviatoric Plastic Strains

    Yield surface:

    Using:

    Differentiating (dq/dp), we find normalof the yield surface (-dp/dq):

    2 2

    2

    M

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    Deviatoric Plastic Strains

    Normal of theyield surface

    2 2

    2PS Vd d

    M

    /P P

    S S Vd d d dp dq

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    Plastic Strains (General)

    d

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    Summary

    Volumetric Strains:

    Deviatoric Strains:

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    Critical-State Soil Models

    Department of Civil and Envir. Eng., Rensselaer Polytechnic Institute, Troy, NY

    April, 2014

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    Summary

    p

    (kPa)

    CSL

    M

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    Summary

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    Yield Surface

    Yield Surface: Separates states of stress which cause only elastic

    strains from states of stress that cause plastic (and elastic) strains

    Preconsolidation Pressure

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    Summary

    Volumetric Strains:

    Deviatoric Strains:

    G l F l i

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    General FormulationBorja, R. I., & Lee, S. R. (1990). Cam-clay plasticity, part I:

    implicit integration of elasto-plastic constitutive relations.

    Computer Methods in Applied Mechanics and

    Engineering, 78(1), 49-72

    G l F l i

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    General Formulation

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    Hardening Behavior

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    Hardening Behaviorq

    P

    e

    Critical State

    Line

    State Boundary

    Surface

    NormalConsolidation

    Line

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    Hardening Behaviorq

    P

    e

    Critical State

    Line

    State Boundary

    Surface

    NormalConsolidation

    Line

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    Softening Behavior

    S f i B h i

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    Softening Behavior

    q

    P

    e

    Critical State

    Line

    State Boundary

    Surface

    NormalConsolidation

    Line

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    Softening Behaviorq

    P

    e

    Critical State

    Line

    State Boundary

    Surface

    NormalConsolidation

    Line

    NCL

    CSL

    e

    P

    d d l

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    Extended Cam Clay

    d d C Cl

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    Extended Cam Clay

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    Effect of shape of Yield Function