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    Geotechnical and Geoenvironmental Aspect of Waste

    and their Util ization in I nf rastructure Project

    Modeling Techniques in Geotechnical

    Engineering

    V. A. Sawant

    Associate Professor

    Department of Civil Engineering

    IIT Roorkee

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    PHYSICAL MODELING

    NUMERICAL MODELING

    STATISTICAL ANALYSIS- DEVELOPMENT OFEMPIRICAL RELATIONSHIPS

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    PHYSICAL MODELING

    CENTRIFUGE MODELING

    NUMERICAL MODELING

    RELIABILITY BASED ANALYSIS

    ARTIFICIAL NEURAL NETWORKS

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    Physical Modeling

    Studies on scaled models are resorted to in engineering

    disciplines in order to understand the behaviour of thereal full-scale structures called prototypes.

    A physical model involves a real object subjected to

    forces or displacements and physical quantities such as

    resulting responses are measured.

    From the physical measurements made on the model,

    the corresponding quantities are predicted for the

    prototype.

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    Scaled models in GE seriously lack similitude

    because stress levels in the model do not matchthose in the prototype.

    There are two major factors which need to be

    considered in modeling of GE structures Theseare :

    Body force due to gravity which is often the

    actuating force and

    Soil properties such as strength and stiffness

    which are highly stress dependent.

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    CENTRIFUGE MODELINGWhen studies are undertaken to understand the

    behavior of real structures through scaled models, it isfound impossible to simulate the body forces in the

    normal 1 g field.

    It has been realized that this deficiency can beovercome with the use of centrifuge technique in which

    models are subjected to predetermined, high

    acceleration levels to produce similarity conditions

    satisfactorily in most situations.

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    Centrifuge modeling is now firmly established as a

    dependable research tool that can provide solutions to

    many of the intractable problems in GE.Some of the important problems relating to earth dams

    tunnels, offshore foundations, geo-environmenta

    problems, problems of nuclear waste disposal, seismicstudies of earth structures and foundations can be

    tackled using centrifuge modeling.

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    Two systems are said to behave similarly when

    corresponding physical quantities are related by

    equations of the type Rm=Rpwhere Rm and Rp are same physical quantity pertaining

    to the model and the prototype

    is the proportionality constant.Different physical quantities may be related by

    different proportionality constants. The linearity of the

    relationship is a necessity.

    When two systems behave similarly :

    knowledge of the behaviour of one will enable us to

    determine what the behaviour of the other must be.

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    Modeling of clay slope

    Consider the stability of a

    clay slope shown in Figure

    having a slope angle i under

    undrained conditions.

    An estimate of the

    maximum stable height maybe based on the slip circle

    method of analysis.

    Based on Taylor's stabilitychart the maximum stable

    height of slope Hc for i =

    60 can be estimated.

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    Suppose if this estimate is to be verified, how

    could one proceed to carry out a scaled model

    study by reducing the linear dimension by afactor, say of 50 %.

    If experiments are envisaged in 1-g field it

    becomes necessary to produce a model material

    having a value of cu/=0.02 for the value of theprototype material.

    It is indeed almost impossible to produce a

    material corresponding to this value of cu/.

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    Table 3 Scaling Laws

    Quantity Prototype Model

    Length n 1

    Area n2

    1Volume n3 1

    Velocity 1 1

    Acceleration 1 n

    Mass n3 1

    Force n2 1

    Energy n3 1Stress 1 1

    Strain 1 1

    Mass density 1 1

    Energy density 1 1

    Time (dynamic) n 1

    Time (diffusion) n2 1Time (creep) 1 1

    Frequency 1 n

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    ANNs are a data driven artificial intelligence approach

    that attempts to mimic, cognition capability of humanbrain.

    ANNs learn by examples of data inputs and outputs

    presented to them so that the subtle functionalrelationships among the data are captured, even if the

    underlying relationships are unknown or the physical

    meaning is difficult to explain.

    This is in contrast to most traditional empirical andstatistical methods, which need prior knowledge about

    the nature of the relationships among the data.

    ARTIFICIAL NEURAL NETWORKS

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    The input from each PE in the previous layer xi is multiplied by

    an adjustable connection weight wji. At each PE, the weighted

    input signals are summed and a threshold value j is added.

    This combined input Ij is then passed through a nonlineartransfer function f(Ij) to produce the output of the PE yj . The

    output of one PE provides the input to the PEs in the next layer.

    The propagation of information in an ANN starts at the input

    layer, where the input data are presented. The network adjustsits weights on the presentation of a training data set and uses a

    learning rule to find a set of weights that will produce the

    input/output mapping that has the smallest possible error. This

    process is called learning or training.Once the training phase of the model has been successfully

    accomplished, the performance of the trained model needs to

    be validated using an independent testing set.

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    Figure 2 Main steps in ANN model development

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    Liquefaction during earthquakes is one of the very dangerous

    ground failure phenomena that can cause a large amount of

    damage to most civil engineering structures. Although theliquefaction mechanism is well known, the prediction of

    liquefaction potential is very complex. This fact has attracted many

    researchers to investigate the applicability of ANNs for predicting

    liquefaction. Hanna et al (2007) reported evaluation of liquefaction

    potential of soil deposits using artificial neural networks. The

    prediction capabilities of the ANN model was compared to a set of

    data that were not used during model training and testing. The

    validation data was randomly selected from both Kocaeli and Chi-

    Chi earthquakes, and corresponds to approximately 12 percent of

    the data set collected. The results are presented in graphical form

    in Figure 3. The results produced by the proposed ANN model

    compare well with the field data.

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    Figure 3 Network performance on soil liquefaction potential (Hanna et al 2007)

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    NUMERICAL MODELINGMathematical and computational techniques have been developed for

    design, analysis, and prediction of the behavior of soil and rock, as well

    as structural elements in contact with the soil, when subjected tovarious internally or externally applied boundary conditions.

    Models are not meant to be an exact representation of reality, but

    rather to mimic the essential characteristics of the elements of the

    prototype as necessary for design or prediction.

    Status in Basic and Applied Engineering Research

    Numerical modeling is the subject of many basic and applied research

    efforts in civil engineering. Such efforts often involve the use of FDM,

    FEM, BEM, and DEM in conjunction with sophisticated nonlinear

    elastic, elastoplastic, viscoplastic, crystal plasticity, and

    micromechanical constitutive models. Constitutive models have

    increased rapidly in sophistication in recent decades.

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    Subgrade Reaction Approach

    Elastic Continuum Approach

    Finite Element Analysis

    Analysis of Pile (LLP)

    S i l i l FEM

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    In the SAFE approach, variations of loading anddisplacements in the direction of revolution are

    expressed in the form of Fourier series.

    Displacements in the plane forming solid ofrevolution are expressed using shape functions, as

    employed in 2-D FE formulation.

    Semi-analytical FEM

    L

    n

    n

    L

    n

    n

    L

    n

    n

    L

    n

    n

    L

    n

    n

    L

    n

    n

    nwnww

    nvnvv

    nunuu

    10

    01

    10

    sincos

    cossin

    sincos

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    Semi-analytical FEM

    Pile & soil media 8 node continuum element

    Interface between pile and soil 6 node interface

    element

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    Eight Noded Element

    84

    112

    1

    62

    112

    1

    7,5,3,1

    1)1)(1(4

    1

    2

    2

    andifor

    N

    andifor

    N

    ifor

    N

    ii

    ii

    iiiii

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    Stress strain relationship is given as,

    DD

    z

    r

    rz

    z

    r

    z

    r

    rz

    z

    r

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    215.000000

    0215.00000

    00215.0000

    0001

    0001

    0001

    )1)(21(

    ED

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    Element stiffness matrix, [K]e, is given by

    Load vector, {F}, for uniformly distributed load,

    qz, acting on the element can be obtained as,

    1

    1

    1

    1

    2 ddrJBDBkT

    e

    2

    0

    1

    1

    0

    sin

    cos

    ddrNqaFT

    e

    Stiffness matrix of and interface element

    V S

    f

    T

    f dsBDBk

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    Geometry and Material

    Properties

    Pile E=0.3605108 kPa

    = 0.15

    Soil Es=4267 kPa

    Load 1000 kN

    Dia (m) 0.4, 0.6, 0.8, 1.0

    L/D Ratio 10, 15, 20, 25

    z/D

    r/D

    Finite Element Mesh

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    Deflection Curves for different Dia & L/D ratio

    Z/L

    Non-dimensional Displacement

    0.4-25

    0.6-25

    0.8-25

    1.0-25

    0.4-20

    0.4-15

    0.4-10

    M/HT

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    Z/L

    M/HT

    25 20

    15 10

    Bending Moment along the length of pile

    Depth of max. moment 0.33, 0.3, 0.25, 0.2 (L/D 10, 15, 20, 25)

    i l ( )

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    Top-Displacement (mm)

    L/D Dia 0.4 Dia 0.6 Dia 0.8 Dia 1.0

    10 186.660 123.025 91.435 72.582

    15 159.468 105.436 78.557 62.489

    20 155.309 102.769 76.618 60.977

    25 155.131 102.658 76.538 60.916

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    Pile Top Displacement (mm)

    Top-Displacement(m

    m)

    L/D

    0.4 0.6

    0.8 1

    EI

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    Non-dimensional Top-Displacement

    L/D Dia 0.4 Dia 0.6 Dia 0.8 Dia 1.0

    10 0.50831 0.50253 0.49799 0.49413

    15 0.43426 0.43068 0.42785 0.42542

    20 0.42293 0.41979 0.41729 0.41513

    25 0.42245 0.41933 0.41685 0.41471

    3TH

    EI

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    Non-dimensional Pile Top Displacement

    Non-DimensionalDisplacement

    L/D

    0.4 0.6

    0.8 1

    M M t (kN )

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    Max. Moment (kNm)

    L/D Dia 0.4 Dia 0.6 Dia 0.8 Dia 1.0

    10 566.465 848.613 1129.925 1410.425

    15 707.483 1057.121 1404.825 1750.825

    20 731.766 1092.167 1450.161 1806.061

    25 733.780 1095.050 1453.869 1810.558

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    Maximum Moment in Pile (kNm)

    Max.

    Moment(kNm)

    L/D

    0.4 0.6

    0.8 1

    M

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    Non-dimensional Max-Moment

    L/D Dia 0.4 Dia 0.6 Dia 0.8 Dia 1.0

    10 0.22190 0.22162 0.22131 0.22100

    15 0.27714 0.27607 0.27516 0.27434

    20 0.28665 0.28522 0.28404 0.28300

    25 0.28744 0.28598 0.28476 0.28370

    TH

    MM max

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    Non-dimensional Max. Moment in Pile

    Non-D

    imensionalMaxM

    oment

    L/D

    0.4 0.6

    0.8 1

    Observations

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    1. Top Displacement (absolute and non-dimensional) is

    decreasing with increase in pile diameter and L/D ratio.

    However after L/D=20 it approaches a constant value(0.42 in non-dimensional).

    2. Absolute Max. Moment in Pile is increasing with

    increase in pile diameter and L/D ratio. However after

    L/D=20 it approaches a constant value.

    3. Non-dimensional Max. Moment in Pile is decreasing

    with increase in pile diameter, but increasing with L/D

    ratio (0.22 to 0.28). However after L/D=20 it approaches

    a constant value (0.287).

    4. Depth of max. moment decreases with L/D ratio from

    0.33 (for L/D=10) to 0.2(for L/D=25).

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    3-D F ini te Element Analysis

    Pile, pile cap and soil aredescretized using 20 nodeisoparametric continuumelements

    Interface between the pileand soil is modeled using 16node isoparametric surfaceelement.

    The analysis, further, takesinto consideration theinteraction between the pile

    cap and underlying soil,generally the most neglectedparameter in the analysis ofpile group.

    ddVVBDBK

    dddJBDBK

    f

    T

    fe

    T

    e

    1

    1

    1

    1_

    1

    1

    1

    1

    1

    1

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    Pile was hollow circular with diameter of 1.6. However, for the sake of convenience, the

    hollow circular section of pile is converted into an equivalent solid circular section of 1.6

    An equivalent modulus of elasticity of sand

    modulus was approximately computed from the relation E= Jz Terzaghi (1943)

    where z is the depth from surface and J is the dimensionless parameter. Lateral load of

    magnitude 2.75 lb

    Table 1 : Properties of Pile Soil

    Pile Soil

    Mild Steel Medium Dense sand

    Ep =43520 lb.inch2 Density =120 lb/cft

    = 0.20 = 0.25

    J = 350

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    0

    4

    8

    12

    16

    20

    24

    -0.002 0.000 0.002 0.004 0.006 0.008 0.010 0.012 0.014 0.016

    Depth(inch)

    Displacement (inch)

    Figure 2 Comparioson of Top Displacement of Pile

    FEM Expt

    Figure 3 Comparison of Bending Moment distribution in Pile

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    Figure 3 Comparison of Bending Moment distribution in Pile

    0

    4

    8

    12

    16

    20

    24

    -0.5 0.5 1.5 2.5 3.5 4.5 5.5

    Depth(i

    n)

    Moment (lb-in)

    FEM

    Expt

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    From the Figure 2 and Figure 3, quite a good

    agreement is seen in the results obtained by FEMand experiment.

    Variation obtained in displacement between either

    result is in the range of 4-10 % and that in moment

    in is in the range of 3- 8%.This indicates close agreement in the results.

    Displacement (m)

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    D

    epth(m)

    FirstSecond

    Third

    Spacing 3D

    Depth(m)

    Moment (kNm)

    First

    Second

    Third

    Spacing 3D

    Granular Pile (GP)

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    In this section, a single GP whose modulus of

    deformation increases with depth is analyzed.

    If (z, ) are vertical and shear stress on anyelement, then from the equilibrium of vertical

    forces on the elementdzd

    d z 4

    ZEZE 10

    Assuming the modulus of deformation E(Z) of the GP

    to increase linearly with depth as

    where is the rate of increase of the modulus with the

    normalized depth Z=z/LStress strain relation for the GP

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    d

    wWand

    Ed

    Lkwhere

    WZdWd

    ZdWdZ

    Ed

    wk

    zd

    wd

    Lzd

    wdZ

    dwk

    zdwdLE

    zdwdZE

    zd

    wdZEZE

    s

    s

    s

    zz

    0

    2

    2

    2

    0

    2

    2

    02

    2

    0

    0

    4

    01

    04

    1

    4/1

    1.

    Boundary conditions

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    Boundary conditions

    At top of GP z=Z=0 24

    d

    Pz

    At tip z=L, Z=1,

    W=0, if GP is resting on rigid stratumw = z/kt, for deformable stratum

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    01

    1

    01

    1

    1

    22

    2

    2

    2

    W

    W

    Zd

    Wd

    Zd

    WdZ

    W

    W

    Zd

    Wd

    Zd

    WdZ

    dkwhere

    W

    Wdk

    m

    sisi

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    ZnW

    WnZnWnZnW

    nZWith

    WW

    ZWW

    ZWWWZ

    i

    iii

    i

    iiiiii

    121

    5.015.01

    1

    012

    21

    2

    2

    1

    2

    1

    2

    211

    211

    Consolidation

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    222

    22

    2

    2

    2

    2

    2

    ,,1,,2,,1

    ,1,,,2,1,

    2

    ,1,,1,11

    ,,,,

    1

    z

    tjiutjiutjiu

    z

    u

    r

    tjiutjiutjiu

    r

    u

    r

    tjiutjiu

    rr

    u

    r

    t

    tjiuttjiu

    t

    u

    formDifferenceFinite

    z

    uC

    r

    u

    rr

    uC

    t

    u

    j

    vZvR

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    22

    ,,1,,2,,1

    ,1,,1,2

    ,1,,,2,1,,,,,

    z

    Ctand

    r

    Ctwhere

    tjiutjiutjiu

    tjiutjiurr

    tjiutjiutjiutjiuttjiu

    vZZ

    vRR

    Z

    jR

    R

    00;0;02

    r

    urat

    z

    uHzatudrAt e

    Boundary conditions

    Reliability

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    Reliability is the probability of an system performing its

    required function adequately for a specified period of

    time under stated conditions.It is the purpose of reliability-based design to produce

    an engineered system whose failure would be an event

    of very low probability.

    Probabilities of failure are the most significant indexesof reliability.

    Being objective, they admit directly to comparisons of

    the risk of failure of different systems under varying

    operating conditions.

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    Slope section for the Illustrative example``1

    Central factor of safety of the slope using mean values of

    the uncertain parameters is 1.243

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    Table 1 Soil data for Illustrative Example

    Soil Parameter Mean Value COV (%)

    Cohesion, c' (kN/m2) 18.00 22.22

    Friction Angle, 30.00 10.00

    Unit Weight, (kN/m3

    )19.50 3.00

    Pore Pressure Ratio, ru0.35 50.00

    First Order Second Moment (FOSM) Method

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    First Order Second Moment (FOSM) Method

    FOSM estimates the uncertainty on the FS as a function of the

    variances of the random input variables.

    , cohesion, and pore pressure u.

    It uses Taylor series expansion to estimate the local uncertainty of

    the FS

    If Y is a function of several random variables,

    Y=g(X1, X2, ........, Xn)

    One can obtain the mean and variance of Y, using Taylor

    series expansion, as follows

    n

    i

    n

    jji

    ji

    n XXCVXX

    gXXgYE

    1 1

    2

    21 ,2

    1,.......,,X

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    in

    i i

    n

    ii

    i

    n

    n

    i

    n

    ijji

    jii

    n

    i i

    XVX

    gYVandXV

    X

    gXXgYE

    XXCVX

    g

    X

    g

    XVX

    g

    YV

    2

    112

    2

    21

    1

    1 1

    2

    1

    2

    1,.......,,X

    ,2

    Rosenblueth's Point Estimate Method (RPEM)

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    PEM, suggested by Rosenblueth (1975) and modified by Li

    (1992) is widely used.

    The versatility of the RPEM is that, it can be used even when

    the functional relationships are not given as an explicit

    equation. This independence from the type of distribution or

    correlations among the basic variables is an advantage.

    In RPEM, the original probability density function (PDF) ofthe random variable X is approximated by assuming that the

    entire probability mass of X is concentrated at two points x-

    and x+.

    Calculations are made at two points and Rosenblueth uses the

    following notations

    X- = -z- and X+ = -z+

    xgpxgpYErrr

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    1;

    2

    11

    2

    1

    1

    2

    zzzwhere

    ppandzz

    zp

    1

    1 1121

    2,........,,

    N

    i

    N

    ijN

    ij

    ji

    N

    iiiN

    pp

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    Table 2 Results of reliability Analysis by RPEM and FOSM

    (c',') = 0 (c',') = 0.50 (c', ') = 0.25

    RPEM FOSM RPEM FOSM RPEM FOSM

    E[FS] 1.242 1.243 1.238 1.243 1.243 1.243

    [FS] 0.303 0.291 0.282 0.275 0.315 0.3

    () 0.798 0.835 0.843 0.884 0.771 0.811PrFS 1.0 0.2124 0.2018 0.1996 0.1883 0.2203 0.2086