soil shear strength_lecture

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  • 7/30/2019 Soil Shear Strength_Lecture

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    PBWN302

    CEM/WEE/STE

    Dr.Asmaa

    Moddather

    SoilMechanicsandFoundations

    FacultyofEngineering CairoUniversity

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    Soil fail in shear.

    Shear strength of soil is the internal resistance that the

    soil mass offer to resist failure/sliding along any plane

    .

    ear a ure w occur at po nts w ere s ear stresses exceeds soils shear stren th S .

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Shear stresses are generated into the soil mass due to

    .

    The engineer needs to know the nature of shearing

    o bearing capacity of foundations.

    o stability of slopes.

    o lateral pressure on retaining walls.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    FailuresurfaceStablemass

    Bearing

    capacity

    of

    Foundation

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Failuresurface

    Stablemass

    ta ty o s opes

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Directionofmovement

    Failuresurface

    Stablemass

    lateral ressureonretainin walls

    Failuresurface

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    1. oca a ure ta es p ace at po nts w ere s ear stresses() > shear strength (S).

    2. When local failure occurs at sufficiently large numberof oints within the soil mass a eneral failure takesplace.

    3. a ure a es e orm o s ng o a so oc over aFailure/Sliding/Slip surface within the soil mass.

    To study shear failure at a point, we need to calculate:

    1. Stresses (, ) on any plane through this point

    Dr.Asmaa Moddather PBWN302 Fall2012

    2. Shear resistance S at this point

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    ons er ng a certa n po nt ns ethe soil mass and knowing the

    y

    norma an s ear s ressesacting on two planes at this point:xy

    x

    o What is the maximum and

    minimum normal stresses

    xx

    xy

    magnitude and direction ?

    o What is the maximum shear

    xy

    stresses (magnitude anddirection)?

    y

    o What is the normal () and shear

    stresses actin on an lane?

    Dr.Asmaa Moddather PBWN302 Fall2012

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    t s a grap ca met o to presentthe state of stress along any plane

    pass ng roug any po n w n esoil mass. y

    Need to define and signxy

    x

    o For :

    xx

    xy

    Compression

    +ve sign

    Tension ve signxy

    o For :

    Rotation clockwiseve si n

    y

    Dr.Asmaa Moddather PBWN302 Fall2012

    Rotation anticlockwise +ve sign

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    y

    ane

    tressesonp anea: x,xy

    Stressesonplaneb:( , x )

    xy

    xy

    ane a

    xx

    xyMohrs circle

    xy

    y

    a

    o

    yxy

    bxy

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Mohrs circle

    x

    yxy

    xy

    Plane a

    xy

    xy

    a

    y

    ox

    yxy

    Every point on the circle represents the state of stress acting on a

    plane passing through the soil element.

    Dr.Asmaa Moddather PBWN302 Fall2012

    There are infinite number of planes passing through the element.

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    Plane b

    maxc

    xx

    xyxy

    Plane a

    aMinor principal

    plane (3, 0)Major principal

    plane (1, 0)xy

    xy

    b

    y

    mind

    Maximumandminimumnormalstresses:

    o Majorprincipalplane(1,0)

    3,

    Maximumandminimumshearstresses:

    o Planec

    + /2

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Planed((1+3)/2,min)

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    Plane b

    xx

    xyxy

    Plane a

    a xyxy

    ,

    b

    y

    Pole

    Define: Pole

    parallel to any plane, the line will intersect the circle at a point

    whose coordinates are and actin on this lane.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Plane b

    xx

    xyxy

    Plane a

    axy

    xy

    plane

    by

    Poleorizonta

    plane

    HowtofindthePole?

    Needtoknowthefollowingaboutasingleplane:

    o Stateofstress( and)

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Directionofplane

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    Plane b

    maxc

    xx

    xyxy

    Plane a

    aMinor principal

    plane (3, 0)Major principal

    plane (1, 0)xy

    xy

    1

    b

    y

    Pole

    23

    mind

    Knowingthelocationofthepole,determinethedirectionof:

    1, ,

    o Minorprincipalplane(2,withhorizontal,clockwise)

    o

    Plane

    with

    maximum

    shear

    stress

    ( ,

    with

    horizontal,

    clockwise)

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Planewithminimumshearstress(4,withhorizontal,anticlockwise)

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    estateo stresson2perpen cu ar

    laneswithinasoilelementisshownin2 t/m2

    theoppositefigure.DrawMohrscircle, 1.5 t/m2

    anddetermine:

    5 t/m25 t/m

    .

    whichtheyact. 2

    ii.Maximum

    shear

    stress

    and

    the

    Soil Element

    .

    iii.Thestateofstressonaplaneinclined

    Dr.Asmaa Moddather PBWN302 Fall2012

    20o anticlockwisewithhorizontal.

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    22 t/m

    2

    2Plane b

    , .

    Stresses on plane b: (+2, +1.5) t/m25 t/m2

    5 t/m2

    Plane a

    2 t/m2Note: horizontal

    and

    vertical

    axes

    MUST

    be

    drawn

    withthesamescale 2

    b Pole

    o (t/m2)

    a

    Dr.Asmaa Moddather PBWN302 Fall2012

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    t/m2

    max

    b3 Pole

    o 1

    3

    2

    (t/m2)

    a

    i.Principle stresses ( = 0):

    1: Major principle stress = 5.62 t/m2, 1 = 68

    o clockwise, with horizontal

    3: Minor principle stress =1.37 t/m2, 2 = 158

    o clockwise, with horizontal

    Dr.Asmaa Moddather PBWN302 Fall2012

    Maximum shear stress: max = 2.12 t/m2, 3 = 23

    o anticlockwise, with horizontal

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    t/m2

    b20

    Pole

    (t/m2)

    (1.39, 0.18)

    (t/m2)

    a

    iii.

    State of stress at plane inclined 20o anticlockwise with horizontal:

    = 1.39 t/m

    2

    Dr.Asmaa Moddather PBWN302 Fall2012

    = 0.18 t/m2

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    o Frictionandinterlockingbetweensoilparticles Friction

    componento Interparticleattractionforces(duetoelectrochemicaleffects)

    Cohesioncomponent

    function of the effective normal stress () acting on plane of

    failure: ''' tancS +=

    where, c and are the shear strength parameters

    c: effective cohesion

    Dr.Asmaa Moddather PBWN302 Fall2012

    : effective angle of shearing resistance

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    Mohr-Coulomb shear strength

    failure envelope

    c

    '''

    f tancS +==

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Shear strength

    failure envelope

    (f, f)

    c

    Elastic equilibrium

    ast c equ r um

    Dr.Asmaa Moddather PBWN302 Fall2012

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    ,

    between particles ():

    v.loose

    versus

    v.

    dense

    o Gradation:

    poor ygra e versuswe gra e

    small large

    o

    Particle

    shape:roundedversusangular

    small large

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Particlesurface

    roughness

    (as

    roughness

    increases,increases)

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    orcoarsegra ne so :

    o

    ranges

    rom

    27o

    to

    45o

    dry wet

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    Forfine

    rained

    soils,

    S

    de ends

    on

    friction

    and

    interlockin

    o Stresshistor overconsolidation ratio :

    betweenparticles()aswellascohesion(c):

    asOCR

    increases,

    S

    increases

    ,

    floculated hashigherS

    :

    asdisturbanceincreases,Sdecreases

    o Soi permea i ity water rainage :

    Shearstrength

    of

    soil

    loaded

    under

    drained

    conditions(slowly)isdifferentfromthat

    c

    loadedunderundrained conditions(quickly)

    Drainedshearstrengthversusundrained shear

    stren th

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    Shear strength parameters for a particular soil are

    determined by means of laboratory tests on specimens

    sampled from insitu soil.

    Great care is required in sampling, storage, and handling

    o samp es pr or o es ng, espec a y n case o

    undisturbed samples where it is necessary to preserve the

    in

    situ structure and water content of soil.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Shearboxapparatus.

    ProvingringShearbox

    Vertica isp acement ia gage

    Motor,applieshorizontal

    Dr.Asmaa Moddather PBWN302 Fall2012

    Weightstoapplynormalload

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    Dr.Asmaa Moddather PBWN302 Fall2012

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    s a ev ce use to measure orce. t cons sts

    of an elastic ring of known diameter with a

    measuring device located in the center of the

    r ng t at measures ts e ect on.

    ,

    by which we convert the readings of the

    measuring device (deflection) into force.

    Force = proving ring reading x calibration

    constant.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    c e m a co s ear oxappara us:

    oa ngp a e

    Samplemaybecircularorsquare

    ~

    2

    Dr.Asmaa Moddather PBWN302 Fall2012

    Boxissplitinto2halves

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    1. ssem e eappara us samp e,porouss ones, erpaperneeded),shearboxparts)andfillshearboxwithwaterifneeded.

    2. pp y

    norma

    orce

    on

    top

    o

    s ear

    ox

    1 .3. Shearforceisappliedtospecimenbymovingonehalfofthebox

    relativetotheothertocausefailureinthesoilspecimen.Shearingforceismeasuredbyprovingringorloadcell.

    Pictureofsampleafterfailure

    4. ert ca v an or zonta h sp acementsaremon tore duringthetest.

    Dr.Asmaa Moddather PBWN302 Fall2012

    5. Repeatsteps

    2,

    3,

    and

    4

    for

    different

    normal

    forces

    (N2,N3).

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    1. Foreach

    test,

    calculate:

    Normalstress()=normalforce/areaofsample

    Shearstress()=shearforce/areaofsample

    2. Plot:

    Peak

    ress,

    Densesand

    shearstrength

    Densesandec

    imen,

    v

    nsion

    Shearst

    f heightofsp

    Expa

    ion Sheardisplacement,h

    sandf

    ==constantLoosesand

    Chang

    ein

    Com

    pres

    Loosesandandnormallyconsolidatedclayresultinsimilar(h andvh

    Sheardisplacement,h

    Dr.Asmaa Moddather PBWN302 Fall2012

    Densesandandoverconsolidated clayresultinsimilar(h andvhrelationships)

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    3. or es 1,ge 1 an max1=f1.

    Fortest2,get2 andmax2=f2.

    , 3 max3= f3.

    4. Plot:

    Test (2)

    Test (3)

    (3, f3)

    Test (1)

    (1,f1)

    , ote: or zonta an vert ca

    axesMUST

    be

    drawn

    with

    the

    samescale

    c

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    1. enera y, rec s ear es s are con uc e on ry san , sa ura e san ,

    and saturated clay.

    2. For sands, soil has high permeability, water drains instantaneously

    ur ng e es , u = 0 ur ng s ear ng, ere ore, = roug ou

    the test.

    3. For clays, to maintain = throughout the test (similar to sands), the

    es s con uc e s ow y so excess pore wa er pressure u can ra n

    during shearing.

    4. Measured shear strength parameters: c, called drained/effective

    Dr.Asmaa Moddather PBWN302 Fall2012

    s ear strengt parameters.

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    oreac es ,we now an f on a urep ane,w c s or zon a .

    (,f) Pole

    cMinor principal

    plane (3, 0)Major principalplane (1, 0)

    Dr.Asmaa Moddather PBWN302 Fall2012

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    s ear ox test carr e out on a s ty c ay so , gave t e

    followin results:

    235.6176.6117.758.9Verticalload(N)

    8..1..2Provin

    rin

    dial

    au ereadin

    mm

    If the shear box area is 36 cm2 and the proving ring

    ,

    and the angle of shearing resistance.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    xamp examp e

    235.6176.6117.758.9Verticalload(kg)

    8.97.15.33.2rov ngr ng a gaugerea ng

    (mm)

    132.75105.7578.75

    =3.2x15

    Horizontalforce, H

    (kg) =47.25

    =6.544.913.27

    .

    =1.64 (kg/cm2)

    3.692.942.19=47.25/36

    =

    (kg/cm2)

    Dr.Asmaa Moddather PBWN302 Fall2012

    .

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    xamp examp e4.00

    3.50

    2.50

    .

    (kg/cm

    2)

    1.50

    2.00

    arStress,

    1.00Sh

    0.00

    .

    0.00 0. 0 1.00 1. 0 2.00 2. 0 .00 . 0 .00 . 0 .00 . 0 6.00 6. 0 .00

    c

    Normalstress, (kg/cm2)c = 0.60 kg/cm2

    Dr.Asmaa Moddather PBWN302 Fall2012

    = 25o

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    1. Simple

    2. Not expensive

    Disadvantages:

    . ,weakest plane (might overestimate strength).

    . , ,

    are adjusted such that u = 0..

    specimen is not uniform (stress concentration at corners).

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Provingring

    Test

    specimen

    Dialgageforvertical

    displacementTriaxialcell

    Triaxialcell

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Filterpaper

    Rubbermembrane

    OringsTop/bottom

    Dr.Asmaa Moddather PBWN302 Fall2012

    Porousstones

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    Verticalload

    Transparentcylinder

    Orings

    Confiningpressure

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Dr.Asmaa Moddather PBWN302 Fall2012

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    Air is released SamplePlacement

    Open valve

    Air release valve

    Top drainage

    Loading ram

    Transparent cylinder

    Porous stone

    Specimen

    Porous stone

    Membrane

    Open valve

    Dr.Asmaa Moddather PBWN302 Fall2012

    All around

    Pressure supply

    o om ra nage

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    SamplePlacement:

    1. Trim

    sample

    to

    required

    dimensions

    (h/d

    ~ 2).

    2. P acesamp eon ottom i terpaperan porousstone.

    3. ace

    op

    er

    paper,

    porous

    s one,

    an

    oa ng

    cap.

    . .

    6. Lowerloadin bar usttorestonloadin ca .

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    oa ng ages:

    o Sta eI

    l in confinin ressure( )

    Openvalve

    Open/closedvalve

    Dr.Asmaa Moddather PBWN302 Fall2012

    aroun

    Pressuresupply

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    Applyingaxialload(N)

    Deviatorstress

    (d)

    oa ng ages:

    o Sta eII

    l in confinin ressure( )

    Openvalve

    Open/closedvalve

    Dr.Asmaa Moddather PBWN302 Fall2012

    aroun

    Pressuresupply

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    o Stage1:

    Apply

    confining

    pressure

    (c)

    = cell

    pressure.o Sta e2:

    Increaseaxialload(N)uptofailure.Axialload/areaofspecimen

    iscalled

    deviator

    stress

    .

    c c+df

    cc cc

    +

    Dr.Asmaa Moddather PBWN302 Fall2012

    Stage(1) Stage(2)

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    ra nage con ons ur ng s ages 1 an 2 are se accor ng orequired type of test.

    c c + df

    cc cc

    Valve (open/closed) Valve (open/closed)

    c

    c + df

    Valve opened

    Valve closed

    Valve opened

    Valve closed

    Dr.Asmaa Moddather PBWN302 Fall2012

    Consolidated, C

    Unconsolidated, U

    Drained, D

    Undrained, U

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    c c +df

    cc cc

    Valve (open/closed) Valve (open/closed)

    Stage (1)

    cStage (2)

    c + df

    Consolidated, C Unconsolidated, U Drained, D Undrained, U

    Stage 1 Stage 2 Test Type

    -

    C U Consolidated-Undrained (CU)

    U U Unconsolidated-Undrained UU

    Dr.Asmaa Moddather PBWN302 Fall2012

    U D Unconsolidated-Drained (UD) ever one

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    c c df

    cc cc

    c

    c+df

    Note:

    Stage 2

    c 3

    c

    +df

    =1Stage 1

    Minor principal plane Major principal plane

    Dr.Asmaa Moddather PBWN302 Fall2012

    Pole(c, 0) (c+df, 0)

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    c c + df

    cc cc

    Valve (open) Valve (open)

    Stage (1)

    cStage (2)

    c + df

    Consolidated, C Drained, D

    = =

    c c + df1 =

    1 =

    3 = 3

    3 = 3

    Dr.Asmaa Moddather PBWN302 Fall2012

    1 1 1 1

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    StressstrainRelationships:

    s,d

    OCC

    OCCecimen,

    V

    nsion

    e

    viatorStre

    NCC

    df

    v

    olumeofs

    Expa

    sion Axial Strain, v

    D

    NCCChangein

    Compres

    Axial Strain, v

    d v V v

    relationships)

    Dr.Asmaa Moddather PBWN302 Fall2012

    oosesan

    an

    norma y

    conso a e

    c ay

    resu

    n

    s m ar

    d

    van

    Vv

    relationships)

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    Mohr circle at failure

    dStage I

    tage

    1fdf3

    1

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    1f(2) 3(2)1f(1)3(1)c=0

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    OCC NCC

    pc

    c1

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    c c + df

    cc cc

    Valve (open) Valve (closed)

    Stage (1)

    cStage (2)

    c + df

    Consolidated, C Undrained, U

    = =3 c c

    c c + df1 =

    1 =u =

    3 = 3

    u = va ue measure uring test

    3 = 3 - u

    Dr.Asmaa Moddather PBWN302 Fall2012

    1 = 1 1 = 1 - u

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    StressstrainRelationships:

    s,d OCC

    OCCressure

    ,u

    ve

    e

    viatorStre

    NCC

    df

    p

    orewater

    Axial Strain, v

    D

    NCCChangein

    +ve

    Axial Strain, v

    Dense sand and overconsolidated cla result in similar ( and u

    relationships)

    Dr.Asmaa Moddather PBWN302 Fall2012

    v v

    relationships)

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    u = +ve =

    1 = 1u decreases

    Same diameter

    Mohr circle at failure

    Mohr circle at failure

    (Total stresses, measured)

    ective stresses, ca cu ate

    'c=0

    Dr.Asmaa Moddather PBWN302 Fall2012

    u u

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    = -c c, ,

    3 = 3u increases

    1 = 1u increases

    o Ifc>pc, soil behaves as NCC, u = +ve

    3 = 3u decreases

    =

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    Overconsolidated Cla (OCC)

    Mohr circle at failure

    Mohr circle at failure

    OCC

    ect ve stresses, ca cu ate(Total stresses, measured)

    2

    c1

    pc

    u1 u2

    Dr.Asmaa Moddather PBWN302 Fall2012

    3 4u=-veu=+ve

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    Drainage conditions during stages 1 and 2 are set according to

    re uired t e of test.

    c

    c

    + df

    cc cc

    Valve (open/closed) Valve (open/closed)

    c

    c + df

    Valve opened

    Draina e allowed

    Valve closed

    Draina e not allowed

    Valve opened

    Draina e allowed

    Valve closed

    Draina e not allowed

    Dr.Asmaa Moddather PBWN302 Fall2012

    Consolidated, C Unconsolidated, U Drained, D Undrained, U

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    c c + df

    cc cc

    Valve (closed) Valve (closed)

    Stage (1)

    cStage (2)

    c + df

    Unconsolidated, U Undrained, U

    = =

    c c + df1 =

    1 =d . . dc . . c

    Measured u during shearing = uc + ud +ve (NCC), -ve (OCC)

    Dr.Asmaa Moddather PBWN302 Fall20123 = 3 - u 1 = 1 - u

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    One effective stress circle to all

    total stress circles calculatedSame diameter

    Mohr circle at failure

    Total stresses measured

    u= 0

    1

    '3 1(1)3(1)

    cu

    3(2) 1(2)

    u(1) (-ve)

    u(2) (+ve)c =undrained shearstren th

    Note: increasingc doesntresultinanyincreasein3

    Dr.Asmaa Moddather PBWN302 Fall2012

    Sinceall

    3

    prior

    to

    shearing

    is

    the

    same

    in

    all

    samples,

    the

    strength

    of

    the

    sampleswhenshearedwillbethesame.

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    Loadingframe

    Provingring

    (measuresaxialdisplacement)

    Sample

    SpecialcaseofUUtest

    o c =0

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Verysimple

    and

    quick

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    amp e acemen :

    . ~ .

    . .

    as drying will alter samples characteristics considerably.

    3. Lower loading piston until it contacts specimen.

    4. Begin the test, continue until load values decrease or until20 strain is reac e .

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Ao A

    Bulging

    H

    Ho H

    ConstantV =

    HAAH oo

    testbeforeafter test

    =

    AAHA oooo

    ooo

    ===

    =

    %

    AA o=

    Dr.Asmaa Moddather PBWN302 Fall2012

    )(1)HH(1H)(H

    o

    o 100

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    Readings:Load(F),verticaldisplacement(H)

    Data

    Reduction: a o

    o where: Ho =initialsampleheight

    o Stress: =F/Ac

    c o a

    Ao =initial

    x

    sectional

    area

    of

    the

    sample

    DataPlotting:

    Dr.Asmaa Moddather PBWN302 Fall2012

    o Plotstress

    () versus

    axial

    strain

    (a)

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    Stress,

    qu

    Strain, (%)

    a,f

    qu =unconfinedstrength

    Dr.Asmaa Moddather PBWN302 Fall2012

    cu =undrained shear

    strength

    =

    qu/2

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    qu

    c

    = 0 c = 0

    u = 0

    cu

    qu0.0

    u

    3

    1

    =

    = qu

    0

    qu =unconfinedstrength

    Dr.Asmaa Moddather PBWN302 Fall2012

    cu =undrained shear

    strength

    =

    qu/2

    UnconsolidatedUnconsolidatedUndrainedUndrained (UU Test(UU Test

    versusUnconfinedCompressionTestversusUnconfinedCompressionTest

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    pp

    One effective stress circle to all

    total stress circles (calculated)Same diameter

    Mohr circle at failure(Total stresses, measured)

    c = 3 = 0

    u= 0

    1 '3 1(1)3(1)

    u

    3(2) 1(2)

    u(UC)u(UU1)

    u(UU2)

    =

    Dr.Asmaa Moddather PBWN302 Fall2012

    u

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    ra ne

    s ear

    s reng

    parame ers:

    o c' OCC

    o : NCC,sand

    Theseparametersareobtainedfrom:

    o CDTest

    o Usedtodesignstructuresforlongtermcondition Drained.

    Dr.Asmaa Moddather PBWN302 Fall2012

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    Undrained shearstrengthparameters:

    o cu, u=0 ,

    eseparametersareo ta ne rom:

    o

    es

    Dr.Asmaa Moddather PBWN302 Fall2012

    Undrained.

    xamp examp e 11

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    The following results were obtained at failure in a series of

    .

    i. Determine the shear strength parameters of this soil.

    ii. If a specimen is subjected to a confining pressure of 150 kPa

    , .

    on n ngpressure

    (kN/m2)

    ev a ors ress

    (kN/m2)Test

    1003501

    210102

    Dr.Asmaa Moddather PBWN302 Fall2012

    xamp examp e 11

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    1= c+df3= cc

    2

    df2

    Test

    4501001003501

    6202102104102

    ' .

    c'=119kN/m2

    620c'

    '=12o

    450100 210

    Note: sincec>0,thisclayis

    Dr.Asmaa Moddather PBWN302 Fall2012

    OCC,and

    pc >210kN/m2

    xamp examp e 11

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    ii. If a specimen is subjected to a confining pressure of 150 kPa and a

    deviator stress of 200 kPa would it fail? Comment.

    350150

    c

    Elastic equilibrium

    Dr.Asmaa Moddather PBWN302 Fall2012

    xamp examp e 22

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    Aclayspecimenfailedatunconfinedstrengthvalueof400kN/m2

    when lacedinanunconfinedtesta aratuswhatwouldbethe

    undrained shearstrength

    for

    the

    tested

    specimen?

    u =0

    Undrained Shearstrength:

    0.0

    400

    u

    cu =

    qu/2

    =

    400/2

    =

    200

    kN/m2

    Dr.Asmaa Moddather PBWN302 Fall2012

    xamp examp e 33

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    ,

    (sampleheight=10.4cm,samplediameter=4.2cm),Findtheunconfined

    strengthandtheundrained shearstrengthforthetestedsample.(Ao =13.85

    cm2,Ho =10.4cm).

    1112171613940Load(kg)

    0.3500.3000.1110.0 00.0530.0340.0130.0

    3.3652.8851.0670.7690.5100.327=0.013x100/10.40.0 =H/Ho (%)

    =0.125

    14.3414.2714.0013.9613.9213.9013.85A

    (cm2

    )0.125

    13.85=A

    =13.87

    100

    )100

    (%)(1

    =

    Dr.Asmaa Moddather PBWN302 Fall20120.770.841.211.150.930.65

    =0.290Stress(kg/cm2) 87.13

    4.0=

    xamp examp e 33

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    1.20

    1.40

    qu

    1.00

    (kg/cm

    2)

    0.60

    .

    ialStress,

    0.20

    .Ax

    0.00

    0.00 0.50 1.00 1.50 2.00 2.50 3.00 3.50 4.00

    Axial Strain, a (%)

    Unconfinedstrength:qu =1.21kg/cm2

    Dr.Asmaa Moddather PBWN302 Fall2012

    Un raine S earstrengt :

    cu =

    qu/2

    =

    0.61

    g/cm

    2