ElasticitySummary.pdf

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CVEN4304 Structural Analysis & Finite Elements CVEN9820 Computational Structural Mechanics Summary of Elasticity Theory Chongmin Song School of Civil and Environmental Engineering University of New South Wales 1

Transcript of ElasticitySummary.pdf

  • CVEN4304 Structural Analysis & Finite ElementsCVEN9820 Computational Structural Mechanics

    Summary of Elasticity Theory

    Chongmin Song

    School of Civil and Environmental EngineeringUniversity of New South Wales

    1

  • Course Materials

    Lecture notes

    Section 3.1 of Cook

    Appendix C of Logan

    2

  • Strain-Displacement Relationship (Plane Strain)

    Displacements in x-, y -directions: {u} = [ u v ]TStrains ({} = []{u})

    xyxy

    {}

    =

    uxvy

    uy

    +vx

    =

    x0

    0

    y

    y

    x

    []

    {uv

    } {u}

    3

  • Stress State and Equilibrium Equations

    Equilibrium in plane strain and in plane stress

    x tdy xy tdx+(x +x ,x dx)tdy +(xy + xy ,y dy)tdx+Fx tdxdy = 0xx

    +xyy

    + Fx = 0

    xyx

    +yy

    + Fy = 0

    In matrix form: []T{}+ {F} = 0

    x0

    y

    0

    y

    x

    []T

    xyxy

    {}

    +

    {FxFy

    } {F}

    = 0

    Note that the differential operator [] is the same as instrain-displacement relationship.

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  • Stress-Strain Relationship: Normal stresses andstrains

    xx

    y

    y

    z

    z

    Hookes law (E : Youngs modulus)

    x =xE

    y =yE

    z =zE

    Poissons effect (: Poissons ratio)

    y = xE x = yE

    x = zE

    z = xE z = yE

    y = zE5

  • Stress-Strain Relationship: Normal stresses andstrains

    Superposition

    x =xE y

    E z

    E

    y = xE +yE z

    E

    z = xE yE+zE

    Conversely

    x =E

    (1+ )(1 2) ((1 )x + y + z)

    y =E

    (1+ )(1 2) (x + (1 )y + z)

    y =E

    (1+ )(1 2) (x + y + (1 )z)

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  • Stress-Strain Relationship: Shear stresses and strains

    Hookes law (G : shear modulus)

    =

    G

    In stress components:

    xy =xyG

    ; yz =yzG

    ; xz =xzG

    or conversely

    xy = Gxy ; yz = Gyz ; xz = Gxz

    Shear modulus is not independent of E and

    G =E

    2(1+ )

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  • Stress-Strain Relationship (3D)

    In matrix form ({} = [E ]{} with elasticity (constitutive) matrix [E ])

    xyzxyyzxz

    =

    2G1 2

    1 0 0 0 1 0 0 0 1 0 0 00 0 0 122 0 00 0 0 0 122 00 0 0 0 0 122

    xyzxyyzxz

    Conversely ({} = [E ]1{})

    xyzxyyzxz

    =

    1E

    1 0 0 0 1 0 0 0 1 0 0 00 0 0 2(1+ ) 0 00 0 0 0 2(1+ ) 00 0 0 0 0 2(1+ )

    xyzxyyzxz

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  • Plane Strain Condition

    One dimension (z) is much larger than the other two (x and y )

    In-plane forces do not vary along the largest dimension z.

    Dam Pipeline

    z

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  • Plane Strain Condition

    No displacement occurs along the largest dimension z

    w = 0; z = wz

    = 0

    Inplane displacements u and v are independent of z

    u = u(x , y)v = v(x , y)

    ; xz =

    uz

    +wx

    = 0

    yz=vz

    +wy

    = 010

  • Plane Strain Condition: Stress-Strain Relationship

    Considering z = yz = zx = 0

    xyzxy00

    =

    2G1 2

    1 0 0 0 1 0 0 0 1 0 0 00 0 0 122 0 00 0 0 0 122 00 0 0 0 0 122

    xy0xy00

    Elasticity matrix for plane strain condition:

    [E ] =2G

    1 2

    1 0 1 00 0

    1 22

    Normal stress along the largest dimension z

    z = xE yE+zE

    = 0; z = (x + y )

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  • Plane Stress Condition

    One dimension (z) is much smaller than the other two (x and y )

    zz = yz = xz = 0

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  • Plane Stress Condition: Stress-Strain Relationship

    xyzxy00

    =

    1E

    1 0 0 0 1 0 0 0 1 0 0 0

    0 0 0 2(1+ ) 0 00 0 0 0 2(1+ ) 00 0 0 0 0 2(1+ )

    xy0xy00

    Elasticity matrix for plane stress condition ({} = [E ]{}):

    [E ]1 = 1E

    1 0 1 00 0 2(1+ )

    ; [E ] = E1 2

    1 0 1 00 0 12

    Normal strain along the largest dimension z

    z = E (x + y )

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  • Boundary Conditions

    Enforced displacements

    u = u; v = v ; w = w

    For example, fixed boundary:

    u = v = w = 0

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  • Boundary Conditions

    Prescribed tractions

    Unit outward normal (l, m) onboundary.

    Equilibrium on boundary AB withlength ds

    Boundary conditions

    x = lx +mxyy = lxy +my

    Written in matrix form{xy

    }=

    [l 0 m0 m l

    ]

    [L]T

    xyxy

    = [L]T{}15

  • Boundary Conditions

    Similarity with differential operator in equations of equilibrium

    [L] =

    l 00 mm l

    ; compare with [] =

    x0

    0

    y

    y

    x

    [L] is in the same form as [] with l , m replacing

    x,

    y.

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  • Pure Bending of a Beam

    Displacement solution

    u = Cxyv = 0.5C(x2 + y2)

    Note that planes remain planes(u varies linearly in y and u = 0at neutral axis y = 0)

    Strains

    x =ux

    = Cy

    y =vy

    = Cy

    xy =vx

    +uy

    = Cx Cx = 017

  • Pure Bending of a Beam (conted)

    Stresses (Plane stress condition)

    x =E

    1 2 (x + y ) =E

    1 2 (Cy + C2y)

    = CEy (Linear variation over cross section)y =

    E1 2 (y + x ) =

    E1 2 (Cy Cy)

    = 0

    xy = Gxy = 0

    Equilibrium (body force Fx = Fy = 0)

    xx

    +xyy

    = 0+ 0 = 0

    xyx

    +yy

    = 0+ 0 = 0

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  • Pure Bending of a Beam (conted)

    Boundary conditions

    Left side: outward normal (1, 0)x = lx +mxy = CEyy = lxy +my = 0

    Right side: outward normal (1, 0)

    x = lx +mxy = CEyy = lxy +my = 0

    x

    y

    hn=(1,0)n=(-1,0)

    Bending moment (b: thickness of beam)

    M =12(CE h

    2

    ) h

    2(

    23h2

    ) b 2 = CE bh

    3

    12

    Constant C for a applied bending moment M

    C =MEI

    (I : Moment of inertia)

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  • Common Civil Engineering Problems

    Mathematical model in form of

    []T {}+ {F} = 0; {} = [E ]{}; {} = []{u}; {} = [L]T {}

    Quantity Solid mechanics Heat conduction Seepage flow

    Function Displacements {u} Temperature T Hydraulic head hField gradient Strains: {T} = []T {h} = []h

    {} = []{u} where [] =[

    x

    y

    z

    ]TConstitutive law Elasticity [E ] Conductivity [] Permeability []

    Induced field Stresses: Fluxes: Velocities:

    {} = [E ]{} {f} = []{T} {v} = []{h}Surface load Tractions: Normal flux: Normal velocity:

    {} = [L]T {} fn = [L]T {f} vn = [L]T {v}Internal load Body forces: {F} Source: Q Source QEquilibrium []T {}+ {F} = 0 []T {T} Q = 0 []T {h} Q = 0

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