2014_ce5320 dsp_iv_lab_tests.pdf

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CE 5320 Soil Dynamics (2014) CE 5320 Soil Dynamics (2014) D i S il P i Dynamic Soil Properties- Lab Tests Lab Tests Prof. A. Boominathan Department of Civil Engineering IIT M d IIT Madras [email protected] Prof. Boominathan, IIT Madras

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  • CE 5320 Soil Dynamics (2014)CE 5320 Soil Dynamics (2014)

    D i S il P iDynamic Soil Properties-Lab TestsLab Tests

    Prof. A. BoominathanDepartment of Civil Engineering

    IIT M dIIT [email protected]

    Prof. Boominathan, IIT Madras

  • Laboratory measurement of dynamic soil propertiescan be used to supplement or confirm the results ofcan be used to supplement or confirm the results offield measurements.

    Lab tests are necessary Lab tests are necessary to establish values of damping and modulus of

    strains at larger than these that can be attained ingthe field

    to measure the properties of materials that do notp pexist in the field, such as soils to be compacted.

    Two types of loading: Dynamic loads. Cyclic but slow enough that inertial effects do noty g

    occur.

  • Laboratory TestsLaboratory TestsLaboratory TestsLaboratory Tests

    Low strain element testsLow strain element tests Low strain element testsLow strain element tests Resonant column testResonant column test Bender element testBender element test Bender element testBender element test

    High strain element testsHigh strain element testsC li i i l C li i i l Cyclic triaxial testCyclic triaxial test

    Cyclic direct simple shear testCyclic direct simple shear test Cyclic torsion shear testCyclic torsion shear test

    Prof. Boominathan, IIT Madras

  • Resonant Column Test

    This testing technique applies cyclic

    force to a soil specimen at various

    frequencies.

    A cylindrical test specimen (solid or

    hallow) is excited harmonically in

    torsional or axial loading .

    Fig. shows the soil specimen is fixed

    at the bottom and and is subjected to

    torsition at the toptorsition at the top.

    The resonant (natural) frequency of

    the soil element can be obtainedthe soil element can be obtained

  • For example, when there is no top mass, the natural period of soil

    column, Tn, in torsional shear is given by

    T 4H/VTn = 4H/VsWhen the resonance or the maximum response occurs at the

    l di i d f ( h f f ) i h /1loading period of (or the frequency of ) in the test

    this experimental value and the theoretical value are equated.

    nn/1

    Hence,

    2)/4(,/4/,/4 THGandTHGVVH )/4(,/4/,/4 nnssn THGandTHGVVH

    By equating the theoretical and experimental resonant frequencies, the shear modulus G is obtainedshear modulus, G, is obtained.

  • Interpretation of resonant column test The dynamic response of a specimen to this force is measured in terms of velocity and /or acceleration.

    While a precise measurement of small displacement (deformation) is difficult, velocity and acceleration at a high gfrequency are large enough to be measured.

    By varying the loading frequency, the variation of amplification in amplitude ofamplification in amplitude of response is plotted against the frequency. Damping from Free or

    Forced vibration test data.

  • Lf2 )FLf(4G r2

    Prof. Boominathan, IIT Madras

  • Typical results of R.C tests on Clay

    Prof. Boominathan, IIT Madras

  • Limitations of Resonant Column Test

    The number of loading cycles that a soil specimen experiences during tests is p p gsignificantly greater than that in real earthquakes.qThe obtained modulus and damping corresponds to those of many cycles.corresponds to those of many cycles.

    R.C. tests on water saturated specimens under large strain amplitudes cause under large strain amplitudes cause liquefaction (high frequency shaking makes free drainage of pore water impossible) free drainage of pore water impossible)

  • BENDER ELEMENT TEST

    Bender elements are constructed by bonding two piezoelectrical materialspiezoelectrical materials together in such a way that a voltage applied to their faces causes to expand while the other contracts causing the entire element to bend .

    Si il l l t l di t b Similarly , a lateral disturbance of the bender element will produce a voltage , so that the bender elements can be used be de e e e ts ca be usedas both s-wave transmitters and receivers

    Positive voltage causes element to bend one way way. Negative voltage causes it to bend the other.

  • Shearwavepropagationthroughalaboratorysoilsamplep p g g y p

  • Measurement of wave propagation velocity by bender elements

    By measuring the time

    required for the wave to travelrequired for the wave to travel

    from the source to the receiver,

    and knowing the distanceand knowing the distance

    between each, the shear wave

    velocity of the specimen can bey p

    measured nondestructively.

    the maximum shear modulus

    Gmax (with < 10-6)

    Gmax = 2sVmax sV

  • Prof. Boominathan, IIT Madras

  • Measurement of Vs in the lab Bender Element Test

    LocationDepth

    (m)Soil

    description (soilclassificati

    Gs NMC (%)

    Atterberg limits (%)

    LL PL PI(on)

    LL PL PI

    Tondiarpet 10.00 Soft clay 2.7 60 77 28 49

    Siruseri 2 25 Stiff clay 2 7 34 85 26 59

    Size of specimen: 50 x 100 mm2

    Siruseri 2.25 Stiff clay 2.7 34 85 26 59

    Waveform: sinusoidal Frequency: 5000 Hz Input voltage amplitude: 20 Vpp S/N ratio: 4 db Estimation of travel time: peak

    to peak

    14

  • Comparison of Field and Lab Test Results (Tondiarpet)

    Vs = 120 m/s

    V fili f b d l Wave trace

    Vs profiling from bender element test

    15

    Measured VMeasured Vss is about 20 % and 14 % lower than the field MASW for soft is about 20 % and 14 % lower than the field MASW for soft

    and stiff clay respectively.and stiff clay respectively.

  • Gmax for Kalpakkam sand from Bender element test Bender element test

    (Jaya et al., 2008)

    140

    120

    130

    140

    Dr = 20 %D = 50 %

    90

    100

    110Dr = 50 %

    Dr = 65 % Dr = 85 %

    Pa)

    70

    80

    90

    Gm

    ax (M

    P

    40

    50

    60

    0 20 40 60 80 100 120 140 160 180 200 22030

    Effective Confining Stress (kPa)Prof. Boominathan, IIT Madras

  • Th li t i i l t t d i ll d ib d i The cyclic triaxial test procedures is well described in ASTM D 3999:

    In the triaxial test, a cylindrical specimen is placed between In the triaxial test, a cylindrical specimen is placed between top and bottom loading platens and surrounded by a thin rubber membrane. Th i i bj d di l ll The specimen is subjected to a radial stress usually applied pneumatically and an axial stress.

    The difference between the axial stress is called the The difference between the axial stress is called the deviator stress.

    The deviator stress is applied cyclically either under stress controlled conditions or under strain controlled conditions.

    Frequency range of modern cyclic triaxial apparatus - 0.1 to 10 Hzto 10 Hz.

  • Simulation of earthquake loading in cyclic triaxial apparatusapparatus

    Shear deformations are resulting from propagatedresulting from propagated waves

    Ishihara (1996)Seed and Lee (1966)Prof. Boominathan, IIT Madras

  • CYCLIC TRIAXIAL TEST SETUP

  • Test ProcedureTest Procedure Sample Preparation Size: Diameter 50/70/100 mm Air pluviation, water pluviation and moist tamping

    techniquestechniques Saturation Degree of saturation (B > 0.96)g ( )Consolidation Saturated sand specimens are consolidated to the required

    ff ti i t i teffective isotropic stresses.Cyclic deformation Sine wave with a frequency of 0 1-10 Hz Sine wave with a frequency of 0.1-10 Hz. During cyclic loading the cell pressure is kept constant. The cell pressure, axial load, axial deformation and pore p , , p

    water pressure are monitored using a built-in data acquisition system. Prof. Boominathan, IIT Madras

  • A t i l h t i l i th t t i l t bt i d f th li A typical hysteresis loop in the stressstrain plot obtained from the cyclictriaxial test.

    Modulus is determined from the slope of the line joining the end points ofth lthe loop.

    Damping characteristics can be calculated from the area of the hysterisiscurve which represents the energy dissipated during the strain cycle. Thedamping ratio is proportional to the ratio of the loop to the area of thedamping ratio, is proportional to the ratio of the loop to the area of the

    triangle OAB

    1 4

    area of hysteresis looparea of triangle OAB

  • Typical Stress- Strain Loops from Cyclic Triaxial Tests

    1 cycle

    d1 d2 1 2E ( ) /( )

    W

    d110

    d

    s

    W4 W

    G = E/2(1+)1

    2

    G = E/2(1+)d2

    At 1.5% (200 kPa)Deviator Stress Axial Strain

    ( )

  • Shear modulus and Damping f l kk dcurves for Kalpakkam sand

    60

    40

    50

    (MPa

    )

    20

    30

    '0'0

    200kPa

    100kPa

    mod

    ulus

    (

    10

    20

    Shea

    r m

    0.01 0.1 1 100

    Shear strain (%)

    Jaya et.al, (2008)Prof. Boominathan, IIT Madras

  • Anumberoffieldtestsmeasurelowstrainproperties,

    particularly wave propagation velocities Among theseparticularlywavepropagationvelocities.Amongthese

    testsSeismiccrosshole,MASW,andSeismicrefractionare

    widelyused.

    OtherfieldtestssuchasSPT,BVT,andCPLTmeasurethe

    propertiesatrelativelyhigherstrainlevels.

    Shear modulus G is commonly obtained from laboratory ShearmodulusGiscommonlyobtainedfromlaboratory

    testssuchasresonantcolumn,benderelementandcyclic

    i i ltriaxialtests.

    Prof. Boominathan, IIT Madras

  • Prof. Boominathan, IIT Madras