Stress,Strain & Elasticity

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    Stress, Strain, & Elasticity

    Mostly from Dieter

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    Nine quantities are required to define the

    state of stress at a point.

    Moment balance shows; tij = tji

    Six independent quantities

    zxyzxyzyx ,,,,,

    zyzzx

    yzyxy

    zxxyx

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    Plane Stress

    2-D state of stress

    Approached when one dimension of the

    body is relatively small (example: thin

    Plane stress when s3 = 0

    Only three stresses are required

    xyyx and ,,

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    2/122

    2/122

    4

    2/2cos

    4

    2sin

    xyyx

    yx

    xyyx

    xy

    Orientation

    2/1

    22

    2min

    1max

    22

    xy

    yxyx

    2

    21max

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    State of stress in 3-D

    If , triaxialstate of stress

    0321

    ,

    If , hydrostatic state of stress

    321

    321

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    Invariants

    2223

    2222

    1

    2 xyzzxyyzxzxyzxyzyx

    zxyzxyxzzyyx

    zyx

    I

    I

    I

    The sum of normal stresses for any orientation

    in the coordinate system is equal to the sum of the

    normal stresses for any other orientation

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    Stress Tensor

    Stress is a second-rank tensor quantity Vector is a first-rank tensor quantity

    jiji SaS '

    ' aaa

    A scalar, which remains unchanged with transformation ofaxes, is a zero-rank tensor

    No. components =3n n tensor-rank

    3

    2

    333231

    232221'3

    '2

    S

    S

    aaa

    aaa

    S

    S

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    Kronecker delta, dij

    A second-rank unit isotropic tensor

    001

    If we multiply a tensor of nth rank with dij,

    the product tensor will have (n-2)th rank

    jiij

    0

    100

    010

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    Components of a stress tensor, sij

    Stress is asymmetric tensor

    First invariant of the stress tensor,I1

    I1

    is a scalar

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    Second Invariant,I2, is the sum of principalminors

    Third Invariant,I3, is the determinant of the

    matrix. The three invariants are given by the roots

    of the following equation.

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    2

    2

    2

    0

    02

    yx

    xy

    xy

    yx

    yx

    yx

    yxy

    xyx

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    Hydrostatic stress is given by

    Decomposition of the stress tensor:

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    J1, J2, and J3 are the principal values of thedeviatoric stress tensor.

    J1 is the sum of the diagonal terms:

    J2 is the sum of the principal minors:

    0)()()(1 mzmymxJ

    222

    J3 is the determinant of the deviatoric stress matrix.

    )(66 222

    2

    xzyzxy

    yxxzyJ

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    Displacement, ui

    Q(x,y,z) to Q(x+u, y+v, z+w)

    u =f(u, v, w)

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    1-D Strain

    AB

    ABBA

    L

    Lex

    ''

    x

    u

    dx

    dxdxx

    udx

    u = exx

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    Generalization to 3-D

    For 1-D, u = exx

    Generalizezeyexeu

    jiji

    zzzyxz

    yzyyyx

    xeu

    zeyexew

    zeyexev

    eij= ui/xj

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    Displacement Tensor

    Produces both shear strain and rigid body rotation

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    Is eij a satisfactory measure of the strain?

    If yes, eij=0 when there is no distortion

    Consider a rigid body rotation

    0

    0

    ije

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    Decomposition

    eij needs to be decomposed into shear strain andrigid-body rotation

    Any second-rank tensor can be decomposed into

    a symmetric and an anti-symmetric tensor.

    jiijijjiijij

    ijijij

    eeandee

    e

    2

    1

    2

    1

    Strain Tensor Rotation Tensor

    Generalized Displacement Relation: jijjiji xxu

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    Principal Strains

    Similar in concept to principal stresses Can identify, principal axes along which there

    are no shear strains or rotations, only pureextension or contraction.

    ,coincide with the principal stress axes

    Definition of principal strain axes: Three

    mutually perpendicular directions in the bodywhich remain mutually perpendicular duringdeformation.

    Remain unchanged if and only ifvij =0

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    Dilatation, D

    Volume change or dilatation

    Note D is the first invariant of the strain tensor

    1'

    1)1)(1)(1(

    321

    321

    sfor

    Mean Strain, em = D/3

    Strain deviator, eij, is the part of the strain tensor

    that represents shape change at constant volume

    ijijmijj

    3

    '

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    Engineering Shear Strains

    Shear Strain, g = a/h = tanq ~ q

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    Simple Shear

    +Rotation

    =

    Pure Shear

    xy

    yxxy

    yxxyxy ee

    2

    Tensor shear strains

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    Elasticity (for isotropic solids) Equations that relate stresses to strains are

    known as Constitutive Equations

    Hookes law: sx=Eex

    Poissons Relation:

    E

    xxzy

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    zxzxyzzyxyxy GGG ;;Need only two elastic constants, E and n

    )1(2 GShear Modulus,

    ijkkijij EE

    1

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    Other Elastic Constants

    Bulk Modulus,

    pK m

    E

    Compressibility, b = 1/K

    Lams Constant,

    )21(3

    )21(

    2

    G

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    Inversion

    ijkkijijEE

    1

    ijijmijj

    3

    '

    ijij

    1

    ijij G 2kkii K 3

    Distortion:

    Dilatation:

    )1(2 G

    pK m

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    Plane Stress (s3=0):

    1222

    2121

    1

    1

    E

    E

    1 ane tra n e3= :

    213 E

    122

    2

    212

    1

    )1(11

    )1(11

    E

    E

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    Strain Energy

    Elastic strain energy, U= energy spent by theexternal forces in deforming an elastic body

    dU=0.5P du = 0.5(sxA)(exdx) = 0.5(sxex)Adx

    22

    Strain Energy/vol.,222

    0 xxE

    U

    ijijzxzxyzyzxyxy

    zzyyxxU

    2

    1

    2

    10

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    zxzx

    yzzy

    xyxy

    G

    G

    G

    222

    2220

    21

    2

    zxyzxy

    xzzyyxzyx

    G

    EEU

    ijij

    U

    0

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    Atomistic Aspects(from Ashby and Jones)

    E is influenced by two factors(a) the interatomic bonds spring constant

    (b) the packing of atoms no. of springs

    Different types of Bonds Primary: Metallic, ionic, and covalent

    Strong

    Secondary: van der Waals and HydrogenWeak

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    Ionic Bondni

    r

    B

    r

    qUrU

    0

    2

    4

    )(

    Attractive

    part

    Repulsive

    part

    q-chargee0-permitivity

    of vacuum

    n~12Lacks Directionality

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    Covalent Bond )()( nmr

    B

    rrU

    nm

    Hi hl

    directional

    Metallic bond is

    similar

    Interatomic

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    Interatomic

    Forces

    drdUF,Force

    0rrF for small displacements

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    2

    2

    dr

    Ud

    dr

    dF

    S

    Stiffness,

    When stretching is small, S is a constant

    0

    2

    2

    0

    rrdr

    UdS

    Spring Constantof the Bond

    00 rrSF

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    00 rrNS

    0rr

    n

    No. of bonds/area,2

    0/1 rN

    00

    r

    SE

    n

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    Generalized Hookes Law

    Fourth-rank tensors (81 components)

    klijklij

    klijklijC

    S

    Sijkl Compliance TensorCijkl Stiffness Tensor

    (from Nye: Physical Properties of Crystals)

    Symmetry: sij = sji and eij = eji

    ijlkijkllkijlkklijkl

    lkijlkijklijklij

    SSSS

    SS

    Reduces the no. independent

    components from 81 to 36

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    Contracted Notation

    345

    426

    561

    332313

    232212

    131211

    11

    345

    426

    561

    332313

    232212

    131211

    2

    1

    2

    12

    1

    2

    122

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    565554535251

    464544434241

    363534333231

    262524232221

    161514131211

    CCCCCC

    CCCCCC

    CCCCCC

    CCCCCC

    CCCCCC

    Energy consideration Cmn=Cnm

    Reduces the no. of independent constants to 21

    Possible to reduce no. of independent constants

    further by considering crystal symmetry

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    nmnm S

    Tensor notation 11 22 33 23, 32 31, 13 12, 21

    Matrix notation 1 2 3 4 5 6

    S = S when m and n are 1 2 or 32Sijkl = Smn when eitherm orn is 4, 5, or 6

    4Sijkl = Smn when both m and n are 4, 5, or 6

    S1111 = S112S1123 = S144S2323 = S44

    Possible to reduce no of

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    Example

    Measures extension in Ox3 direction when the

    S34 in orthorhombic crystal

    Possible to reduce no. of

    independent constants further by

    considering crystal symmetry

    crysta s s eare a out t e x1 rect on

    Operate a diad axis parallel to Ox2 direction

    Crystal remains unaltered because of symmetry So does extension parallel to Ox3, now under

    reverse forces

    Implies that S34 has to be necessarily equal to zero

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    Cubic Crystals

    Let Ox, Oy, and Ozbe parallel to [100],

    [010] and [001], respectively.

    Rotate by 90. The crystal will look the

    same.

    665544

    312312

    CCC

    CCC

    Remaining constants

    vanish

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    12111211

    1212

    12111211

    121111

    2

    2

    SSSS

    SC

    SSSS

    SS

    C

    4444

    1

    SC

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    Isotropic Solids

    Form of the matrix can be obtained from thecubic matrix by requiring that the components

    should be unaltered by a 45 rotation

    GSSS

    11441211

    12112 SSX

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    CompositesIsostrain AnalysisCompatibility:

    EEEm

    m

    f

    f

    c

    c

    mfc

    fAAfAA

    PPP

    EA

    P

    EAEA

    P

    cmcf

    mfc

    mm

    m

    ff

    f

    cc

    c

    1/;/

    mfcEffEE )1(

    Rule-of-Mixtures

    I A l i

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    Isostress Ananlysis

    mfc

    mfc

    ff

    ff

    )1(

    )1(

    fm

    mfc

    EffE

    EEE

    )1(

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    Upper and Lower Bounds