Lecture1(Stress Strain MohrCircle FEM)
Transcript of Lecture1(Stress Strain MohrCircle FEM)
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Lecture 1
Stress and Small (Infinitesimal) Strain
Finite Element Method
Mohr Circles
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zz zy zx
yz yy yx
xz xy xx
Representation of 9 stress components in a
Cartesian Coordinate
If the body is in equilibrium, then there is only
6 independent stress components
zx xz zx
yz zy yz
xy yx xy
zz yz xz
yz yy xy
xz xy xx
Stress
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If there is no shear stress on a surface, then the traction vector (think of it as a force vector) must
be parallel to the unit normal vector .
T n̂
multiplier scalar aiswherennT T ˆˆ Rearranging this equation
matrixidentityanis I wheren I 0ˆ
From linear algebra, the condition for the existence of a unique solution is 0det I If we expand the determinant of this equation, we find the characteristic equation (an eigenvalue problem)
0322
1
3 I I I
0ˆ
ˆˆ
3
2
1
n
n
n
zz yz xz
yz yy xy
xz xy xx
If we substitute each of to replace , we can solve for the corresponding eigenvectors321 ,, 321 ˆ,ˆ,ˆ nnn
1ˆˆˆ2
3
2
2
2
1 nnn
zx yz xy z y xT ,,,,,
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4
400
065
058
zz yz xz
yz yy xy
xz xy xx
022 xy yy xx p yy xx p
MPa
MPa
MPa
xy yy xx yy xx
4
90.15684
168
2
1
10.125684
168
2
1
5684168
21
4
1
2
1
3
2
1
22
2
2
1
22
1
2
1
22
2,1
2
1
22
2,1
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1 If we substitute
0ˆ
ˆˆ
1
1
1
1
1
1
z
y
x
zz yz xz
yz yy xy
xz xy xx
n
nn
2221
2221
2221
ˆ
ˆ
ˆ
C B A
C n
C B A
Bn
C B A
An
z
y
x
1
1
zz yz
yz yy A
1
zz zx
yz xy B
yz zx
yy xy
C
1
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6
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Y x A General Equation Constituting an Eigenvalue ProblemIf = eigenvalues, then this equation becomes:
x x A This equation is known as eigenvector equation and it can be represented by the
following homogeneous equations:
rseigenvectoasknownarefor solution10
01e.g.matrixidentity
0
x
I
x I A
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thereforezero,notissince x
0
.
....
.
.
21
22221
11211
nnnn
n
n
A A A
A A A
A A A
I A
This equation is known as the characteristic equation:
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81
24 A
0
81
24
03012
01x284
2
or
551.3
449.8
arerootsor seigenvalueThe
2
1
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To determine the eigenvectors, substitute the eigenvalues into the equation:
08124
2
1
2
1
x
x
which gives an eigenvector corresponding to eigenvalue 1 of 8.449:
0449.881
2449.84
2
1
x
x
1
45.0
2
1
x
x
and an eigenvector corresponding to the second eigenvalue 2 of 3.551:
0551.381
2551.34
2
1
x
x
225.0
1
2
1
x
x
The matrix A is said to be positive-definite, as both its roots are positive.
For nth order matrix, it would involve polynomial of the nth degree
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First Invariant (independent of coordinate system) of Stress Tensor
Second Invariant of Stress Tensor
Third Invariant of Stress Tensor
z y x I 1
222222222
1
2
1 zx yz xy z y x z y x I
222
3 2 xy z xz y yz x zx yz xy z y x I
Second Invariant of Deviatoric Stress Tensor
22222222222226
1
2
1 zx yz xy z x z y y x zx yz xy z y x sss J
Third Invariant of Deviatoric Stress Tensor
1
222
3
3
1
2
I swhere
ssssss J
ii
xy z xz y yz x zx yz xy z y x
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300
00
001 I
m
m
m
m
Deviator Stress
Hydrostatic Stress
m zz yz xz
yzm yy xy
xz xym xx
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Stress Vector zx yz xy z y x
T ,,,,,
Deviatoric Stress Vector3
1
mI s
Vector Equivalent of the
Kronecker Delta 0,0,0,1,1,1T m
Displacement Vector u
Strain Vector zx yz xy z y x
T ,,,,,
Deviatoric Strain Vector
3volme
Octahedral Normal Stress31 I oct
Octahedral Shear Stress2
3
2 J oct
Volumetric Strain z y xvol
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0
0
0
Z z y x
Y
z y x
X z y x
zz yz zx
yz yy xy
zx xy xx
Differential Equation of Equilibrium in Cartesian Coordinate
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Small Strain
zz zy zx
yz yy yx
xz xy xx
z z z
y y y
x x x
z
u
y
u
x
u
z
u
y
u
x
u
z
u
y
u
x
u
u
Representation of 9 strain components in a
Cartesian Coordinate
For symmetry reasons, then there is only 6
independent strain components
z
x
x
z xz zx
y
z
z
y zy yz
x
y
y
x yx xy
uu
uu
uu
2
1
21
2
1
Shear Strain
Normal Strain
Compatibility of Strain to ensure
that a single valued displacement
can be found from integrating the
strain
z x z x
z y y z
y x x y
xz xx zz
yz zz yy
xy yy xx
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
y z x z z y x
x y z y y x z
z x y x x z y
zx yz xy zz
yz xy zx yy
xy zx yz xx
22
2
22
22
2
22
22
2
22
xy xy 2
1
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Deviator Strain
3
3
3
v zz yz zx
yzv yy xy
zx xyv
xx
dev
zz yy xxv Volumetric Strain
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Stress-Strain Relationship
DElasticity Matrix
zx
yz
xy
zz
yy
xx
zx
yz
xy
zz
yy
xx
E
)1(2
)21(00000
0)1(2
)21(0000
00
)1(2
)21(000
0001)1()1(
000)1(
1)1(
000)1()1(
1
)21)(1(
)1(
)1(2
E G
Young’s ModulusShear Modulus
Poisson’s ratio
Lame’s Constant
)21)(1()21(
2
E G
Isotropic Material
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Transverse Isotropic Material E.g., Shale
zx
yz
xy
zz
yy
xx
zx
yz
xy
zz
yy
xx
G
E G
E
E
E
E
2
1
2
1
1
2
122
21
21
1
00000
00000
00)1(2000
0000001
0001
1 isotropyof planethetonormalProperties
isotropyof planetheinProperties
2
1
E
E
zx
yz
xy
zz
yy
xx
zx
yz
xy
zz
yy
xx
nm
nm
nn
nnn
nnnnn
n
E
)21)(1(00000
0)21)(1(0000
00)21(2
1000
000)1(
000)1()1(
000)1()()1(
)21)(1(
2
211
2
211
2
21
2
1
12
22
2
12
22
21
2
2
2
211
2
m E
G
n E
E
2
2
2
1
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Plane Stress Problem: Thin Plate Plane Strain Problem: Tunnel, Retaining Wall
000
0
0
yy yx
xy xx
000
0
0
yy yx
xy xx
yy xx xx xxG
2
1
G
xy
xy2
yy xx yy yyG
2
1
yy xx zz
xy
y
x
xy
yy
xx
G
E E
E E
100
01
01
xy
yy
xx
xy
yy
xx E
2100
01
01
1 2
xy
yy
xx
xy
yy
xx E
2
2100
01
01
211
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Principal Stress Space and Yield Criterion
3
1cos 0 All principal stresses are the same (isotropic stress)
Principal stresses are not the same (general condition)
E F D
nnn ˆ,ˆ,ˆThree orthogonal Unit vector along the stress path plane
1
1
1
3
1 ̂Dn
1
1
0
2
1 ̂E n
1
1
2
6
1ˆF n
planeon planeon Along diagonal
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The components of stresses in the D, E and F directions are given by
the inner products of stresses with the three unit vectors:
p D 33
1321
322
1 E
32126
1 F
Mean stress31 I p
qF E 3
2
3
22
1
133221
2
3
22
21
2
122 By Pythagorean Theorem,
Or the deviatoric stress q is
2
1
2
2
1
2
12
13
2
32
2
21
2
1
133221
2
3
22
21
3
)()()(2
1
I I q
q
q
Lode Angle
23
321
3
2tan
E
F
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Yield Criterion for Metal (Tresca in 1864)
)(31 metal for failureat stresstensileT
T F E 223 31
Yield Criterion for Metal (Von Mises in 1913)
Equation of a circle
stressYield AxialY
Y
2
13
2
32
2
21
22
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Mohr Coulomb Yield Criterion (1773)
cos2
131
sin2
1
2
13131
cos2sin1sin1 31 c
321 For
planetheat Looking
F D 3
2
3
11
F E D 6
1
2
1
3
12
F E D 6
1
2
1
3
13
Irregular Hexagonal Shape
321 For sin22cos62sin3sin13 DF E c
The size of the yield surface depends upon
pstressmeanand D
Perspective View
Triaxial CompressionTest
Triaxial Extension
Test
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Normally, Mohr-Coulomb Yield Criterion is expressedin 3-D stress space as:
0cos3
sinsincos
3
sin21
c J I F
=Lode Angle
6
2
333sin
2
3
2
3 with
J
J
Lode Angle
23
321
3
2tan
E
F
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Drucker-Prager Yield Criterion (1952)
Difficult representation
in Sharp Corner
1. Modify Von Mises Yield Criterion so that
sin3
cos6
sin3
sin6
c pq
Normally, Drucker-Prager Yield Criterion is
expressed in 3-D stress space as:
012 k I J F
k
relates to frictional component of shearing resistance
relates to cohesion component of shearing resistance
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2. Modify Mohr Coulomb Yield Criterion by Lade and Duncan (1975) for cohesionless soil (c=0)
constantmaterialais3
321 where p
32222)1(2)3(2)(3
DF E F F E D
3
3
2
2
)sin3(
sin16
)sin3(
sin12
1
where
3. Modify Mohr Coulomb Yield Criterion by Matsuoka and Nakai (1974) for cohesionless soil (c=0)
constantmaterialais)( 133221321 where p
0)()1(23)31(226222323 F E D DF E F
32
32
sinsinsin99
)sinsinsin1(3
where
0
3
21
K F
I
I I
Normally, Matsuoka and Nakai Yield Criterion
is expressed in 3-D stress space as:
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d r d r r r 111 )()(
1sideonForceRadial
d r d r r r 333 )()(
3sideonForceRadial
)2
()()2
sin()()(
2sideonForce Normal
2312
d dr
d r r
)
2
()()
2
sin()()(
4sideonForce Normal
4314
d dr
d r r
dr
r 2)(
4sideonForceShear
dr r 4)(2sideonForceShear
Concept of Stress and Strain in
Plasticity
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direction)tangential(involumeunit per componentforce body
direction)radial(involumeunit per componentforce body
S
R
directionradialinforceEquation of Equilibrium
02
)(2
)()()(
42
4231
dr Rrd dr
d dr
d dr d r d r
r r
r r
Divide both sides by drd
0)()(
2
1)()( 4242
31
Rr
d dr
r r r r r r
r
r r
)(
Area gets smaller
to the limit
d
r
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Divide the equation by r
0)()(2
1)()( 4242
31
Rr d dr
r r r r r r
01
Rr r r
r r r
0
Rr d
r
r r r r r
r
r
r
r
r
r
r
r
)()(
r r
r
r
Expand by product rule
Similarly the equation of equilibrium in the tangential direction
021
S r r r
r r
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01 R
r r r r r r
021
S
r r r
r r
Differential equation of equilibrium in Polar Coordinate
0 X
y x xy x
Differential equation of equilibrium in Cartesian Coordinate
0
Y
x y
xy y
Make use of Airy stress function to find the elastic stress distribution of a circular hole in an
infinite medium under isotropic stress condition
o
i
P
P
PressureExternal
PressureInternal
Differential equation of equilibrium in Cartesian Coordinate
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0
X y x
xy x
q q
0
Y x y
xy y
For no horizontal acceleration, X=0 Body force is simply the weight of the body g
0
y x
xy x 0
g
x y
xy y
Also need the Compatibility Equations in terms of Stresses
x
u x
Components of Strain
y
v y
x
v
y
u xy
Differentiate twice w.r.t. yDifferentiate twice w.r.t. x Differentiate w.r.t. x and then y
y x x y
xy y x
2
2
2
2
2
Arrive the Compatibility Equation in terms of Strain
Use Hook’s Law to transform into Compatibility Equation in terms of Stress
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p y q
)(1 y x x E
)(1 x y y E
xy xy xy
E G )1(21
y x x y
xy x y y x
2
2
2
2
2
)1(2)()(
Substitute into the compatibility equation, we get:
0
y x
xy x
0
g
x y
xy y
Next, to differentiate the equilibrium equation
Differentiate w.r.t. x
Differentiate w.r.t. y and then add the
two equations and it becomes:
2
2
2
22
2 y x y x
y x xy
For Plane Stress Condition:
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The Compatibility Equation in terms of Stresses is obtained by substituting
back into
y x x y
xy x y y x
2
2
2
2
2
)1(2
)()(
2
2
2
22
2 y x y x
y x xy
)1()()(
2
2
2
2
x y
x y y x )(2
2
2
2
y x
y x
)1(2
2
2
2
2
2
2
2
x x y y
x y y x)(
2
2
2
2
y x
y x
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
2
y x y x x x y y
y x y x x y y x
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02
2
2
2
2
2
2
2
y x x y
y x y x
02
2
2
2
y x y x
The Compatibility Equation in terms of StressesFor Plane Stress Condition:
The Compatibility Equation in terms of Stresses for Plane Stress Condition
including body forces are similarly derived and given as follows:
y
Y
x
X
y x y x 12
2
2
2
F Pl S i C di i
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For Plane Strain Condition:
y x x E 111 2
xy xy xy E G
)1(21
x y y E
111 2
02
2
2
2
y x y x
The Compatibility Equation in terms of StressesFor Plane Stress Condition also the same for
Plane Strain Condition
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The Compatibility Equation in terms of Stresses for any general case with
body forces are similarly derived as follows:
y
Y
x
X
y x y x
1
12
2
2
2
The usual method of solving both the equilibrium and compatibilityequations is to introduce a new stress function (introduced byAiry in 1862, that is why call Airy Stress Function)
0
y x
xy x
0
g x y
xy y
For the equilibrium equations
to be satisfied, it has been shown that the new stress function must also satisfy the following expressions for the stress
components:
gy x
y
2
2
gy y
x
2
2
y x xy
2
S b tit t th i 22 2
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Substitute these expressions
into the Compatibility equation
gy x
y
2
2
gy y
x
2
2
y x xy
2
02
2
2
2
y x y x
The stress function must also satisfy the following expressions:
024
4
22
4
4
4
y y x x
If this stress function can be satisfied, then the equilibriumequation and compatibility equation will also be satisfied .
Thus, the solution of many 2D problems (including body
forces) can be derived by finding a solution which satisfy thestress function incorporating the boundary conditions.
Th t f ti ( ith t b d f ) i l di t
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The stress function (without body force) in polar coordinatesmust also satisfy the following expressions for the stress
components:
2
2
2
11
r r r
r 2
2
r
r r r r r r
111 2
2
The Compatibility Equation in terms of Stresses in polar coordinates is:
01111
2
2
22
2
2
2
22
2
r r r r r r r r
St Di t ib ti S t i l b t A i
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Stress Distribution Symmetrical about an Axis
The Compatibility Equation in terms of Stresses in polar coordinates, when the Stress Function depends on r only, is:
01111
2
2
22
2
2
2
22
2
r r r r r r r r
011211
32
2
23
3
4
4
2
2
2
2
dr
d
r dr
d
r dr
d
r dr
d
dr
d
r dr
d
dr
d
r dr
d
Which is an ordinary differential equation, which can be reduced to a linear differential equation with constant
coefficients by introducing a new variable t such that
The solution has four constants of integration, which must be determined from the boundary conditions.
t er
Assume the stress function to be in the form as:
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Assume the stress function to be in the form as:
The corresponding stress function without body force is obtained:
DCr r Br r A 22
loglog
C r Br
A
r r r 2)log21(
12
2
2
r
0 r
2
2
2
11
r r r r
C r B
r
A2)log23(
2
r r r
1
0 BFor The solution becomeswhich may be used to represent the stress
distribution in a hollow cylinder subjected to
uniform pressure on the inner and outer surfaces
C r
Ar 22 C r
A 22
Apply the boundary conditions: pp
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Apply the boundary conditions: obr r iar r p p
C r
Ar 22
ir pC
a
A 2
2
or pC
b
A 2
2
From which,
22
22
ab
p pba A io
22
22
2ab
b pa pC oi
C r
Ar 22 C r
A2
2 and substitute back into the equation
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22
22
222
22 1
ab
a pa p
r ab
p pba oiior
22
22
222
22 1
ab
a pa p
r ab
p pba oiio
To find the radial displacement, use r uor
r u
r E For Plane Stress Condition
112 234 dddd
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0112
32234
dr
d
r dr
d
r dr
d
r dr
d check
DCr r Br r A 22 loglog
DCr r A 2log
Cr r
Adr
d 2
1
C
r A
dr
d 2
122
2
33
3 12
r A
dr
d
44
4 16
r A
dr
d
4
16
r A
3
12
2
r A
r )2
1(
122 C r
Ar
0)21
(1
3 Cr
r A
r
416r
A 414 r A C r r
A 211 24 0121 24 r C
r A
4
16
r
A 01
64
r
A
Derivation of Elasto-Plastic Solution to compute radial crown displacement of a tunnel under plane
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Derivation of Elasto Plastic Solution to compute radial crown displacement of a tunnel under plane
strain, homogeneous, isotropic stress condition for c’ and ’ material
er
i p o pa
o p
2
r hi h i th di l
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r
r p p er oorr e
which is the radial
stress in the elastic
zone
2
1
r
r p
E r
u er o
r
e
which is the elastic radial displacement
For the stresses in the plastic zone, needs to use the Mohr-Coulomb failure criterion
r
r
r N
sin1
sin1
12
)1(
2)1(
r
r
r
r
r
N
N c
N
N c
pa
r r r i
N
rr
which is the radial stresses
in the plastic zone
r r r r i N
rr cc pa
r r
cotcot
)1(
which is the radial stressesin the plastic zone
sin1
i1
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cossin1
sin1
sin1cossin1
c p
c p
or
or
e
e
which is the radial stress at
the elastic-plastic boundary
Plastic radius1
cot
cotcos)sin1(ln
r r r i
r r o
N
c p
cc p
e aer
cos)sin1( c p p oicrit which is the critical internal
support pressure
Concept of Stress and Strain in Finite Element Formulation
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Plasticity is concerned with predicting the maximum loading which can be
applied to a body without causing:
•Excessive Yield
•Flow
•Fracture
Plasticity Rule is based on 3 assumptions:
1. The yield criterion (F), represented by a surface in the stress space,
at which plastic deformation may develop
2. The hardening law (h being a hardening parameter), that governs the
possible changes in shape, size and position of the yield surface with
an increase in plastic strains
3. The plastic flow rule governing the increment of the plastic strains
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For elasto-plastic materials undergoing infinitesimal deformation,
Total strain increment = Elastic strain increment + Plastic strain increment
plel d d d The elastic strain component can be represented using the generalized Hooke's law:
D = Elastic Constitutive Modulus
Plastic strains are irreversible
plel
d d D Dd d
1st assumption in Plasticity Rule:
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The yield criterion (F), represented by a surface in the stress space, at
which plastic deformation may develop
plhF F ,
h is the vector of the hardening parameters governing the changes of the yield surface with
increasing plastic strains
If F < 0 , material is elastic (stress state within the yield surface)
If F = 0, material is in plastic equilibrium (stress state fulfills the yield criterion or stress
state at the yield surface)
F > 0 Not Admissible (stress state cannot be outside the yield surface)
2nd and 3rd assumptions in Plasticity Rule:
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2. The hardening law (h being a hardening parameter), that governs the
possible changes in shape, size and position of the yield surface withan increase in plastic strains
3. The plastic flow rule governing the increment of the plastic strains
Plastic Flow Rule states that during the plastic strain increment along theyield surface, the plastic strain increment is proportional to the
gradient of the Plastic Potential
Plastic Potential plhQQ ,
Plastic Multiplier Increment d
Q
d d pl
This means that the vector representing the plastic strain increment is directed as the
outward normal vector at the point that corresponds to the current stress state.
In the superimposed space of stresses and strains:
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• The flow rule is called Associated Flow Rule if the yield surface is coincided
with the plastic potential
• The flow rule is called Non-Associated Flow Rule if the yield surface is not
coincided with the plastic potential
Associated Flow Rule Non-Associated Flow Rule
Forming of Elasto-Plastic Constitutive Matrix for Finite Element Analysis
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During plastic strain increment, if the stress points remain on the yield surface, then the
following consistency condition is assumed:
0
pl pl
T T
d h
h
F d
F dF
By substituting the equations relating stress increment to total strain increment and the flow rule,
the following equation is obtained:
0
pl pl
T T
d h
h
F d
F dF
plel d d D Dd d
Q
d d pl
0
d Qh
h
F Q D
F Dd
F pl
T T T
Re-arranging this equation so that the plastic multiplier is a function of the total
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strain as follows:
pe
T
H H
Dd F
d
Q D
F H
T
ewhere
Qh
h
F H
pl
T
p
= so called Hardening Modulus
Finally, substitute the equation describing the plastic multiplier into stress versus strain equation,
the elasto-plastic constitutive matrix governing the incremental direct stress versus strain
relationship in the non-linear range is given below:
d Dd ep
T FQ
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pe
ep
H H
DF Q
D D
D
The matrix is symmetrical if F=Q (Associated Flow Rule)
For Strain Hardening Material, H p>0
For Perfectly Plastic Material, H p=0
For Strain Softening Material, H p < 0
Finite Element Method
I th FEM l i d fi i ti i di ti d i t i l
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• In the FEM, a complex region defining a continuum is discretized into simplegeometric shapes called elements.
• The properties and the governing relationships are assumed over these elementsand expressed mathematically in terms of unknown values at specific points in theelements called nodes.
• An assembly process is used to link the individual elements to the given system.When the effects of loads and boundary conditions are considered, a set of linear ornonlinear algebraic equations is usually obtained.
• Solution of these equations gives the approximate behavior of the continuum orsystem.
• The continuum has an infinite number of degrees-of-freedom (DOF), while the
discretized model has a finite number of DOF. This is the origin of the name, finite
element method.
Examples of Perfectly Plastic Material
k i ld C i i
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Drucker-Prager Yield Criterion
012 k I J F
k
relates to frictional component of shearing resistance
relates to cohesion component of shearing resistance
Mohr-Coulomb Yield Criterion
0cos3
sinsincos
3
sin21
c J I F
=Lode Angle
6
2
333sin
2
3
2
3 with
J
J
Von Mises Yield Criterion
Tresca Yield Criterion
For the particular case of a triaxial compression test, 2=3, the
i b
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equation becomes:
cos2sin3131 c
Discontinuities in the yieldsurface gradient in Mohr-
Coulomb Material : Numerical
difficulties
Matsuoka and Nakai Yield Criterion eliminates
this drawback
0
3
21
K F
I I I
Stress-Strain Constitutive Relationship
For Elastic and Isotropic Material expressed Strain in terms
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For Elastic and Isotropic Material expressed Strain in terms
of Stress (plane stress case)
0
0
0
100
01
01
xy
y
x
xy
y
x
xy
y
x
G
E E
E E
12
'
'
0
E
ModulusShear GratiosPoisson
ModulussYoung E
straininitial
0
1 E
Stress-Strain Constitutive Relationship
For Elastic and Isotropic Material expressed Stress in terms of Strains
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For Elastic and Isotropic Material expressed Stress in terms of Strains
(plane stress case)
0
0
0
2
2100
01
01
1 xy
y
x
xy
y
x
xy
y
x E
0 E stressinitial0 For Elastic and Isotropic Material expressed Stress in terms of Strains
(plane strain case)
0
0
0
2
2100
01
01
211 xy
y
x
xy
y
x
xy
y
x E
Strain and Displacement Relationships (for small strains and small rotations)
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x
v
y
u
y
v
x
u xy y x
,,
v
u
x y
y
x
xy
y
x
0
0
Du or
In Matrix Form
Equilibrium Equations (in elastic theory, stresses must satisfy the following
equilibrium equations)
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0
x
xy x f y x
0
y
y xy f y x
forcesbodyare f and f x x
Boundary Conditions
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The boundary S of the body can be divided
into two parts:
Su (displacement condition) and
St (traction condition) and is described as:
uS onvalueknownvvalueknownu vu _ _
,
t y x S onvalueknown yt valueknown xt t t _ _
,
All types of loads (distributed surface loads, body forces, concentrated
forces and moments) are converted to point forces acting at the nodes
General Formulation of the Finite Element Stiffness Matrix
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Displacement (u, v) inside a plane element are interpolated from nodal
displacement (ui, vi) using shape functions Ni as follows:
d
.
.
....00
...00
2
2
1
1
21
21 N uor v
u
v
u
N N
N N
v
u
vector nt displacemenodal
vector nt displacemeu
matrix functionshape N
d
From the strain-displacement relationship, the strain vector is:
BDND dd
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matrixnt displacemestraintheis
DN Bwhere
Bor DN Du
d ,d
The strain energy stored in an element is:
vol
xy xy y y x x
vol
T dV dV U 2
1
2
1
volT
vol
T dV E dV E U 21
21
kd d 2
1
d d 2
1 T
vol
T T
EBdV BU
The Element Stiffness Matrix k is:
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volT
EBdV Bk
Given the material property E, the behavior of k depends on the B
matrix only, which in turn depends on the shape functions N.
Thus the quality of the finite element analysis is also determined by
the choice of the shape functions.
Constant Strain Triangle (CST)
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Using the strain-displacement relationship, the strain within the element is
related to the displacement at the nodes:
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69
Other types of elements
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Assemble Global Stiffness Matrix
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matrixnt displacemestraintheis
DN Bwhere
Bor DN Du
d ,d vol
T EBdV Bk
d
.
.
....00
...00
2
2
1
1
21
21 N uor v
u
v
u
N N
N N
v
u
Du
Stress Calculation
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0
0
0
2
2100
0101
211 xy
y
x
xy
y
x
xy
y
x E
d EB E
xy
y
x
xy
y
x
For linear elastic material, solution is direct and converge at each load step
For non-linear elastic material and material behaves as elasto-plastic, iterative
method is required because the stiffness matrix is non-symmetrical
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vol
epT BdV E Bk
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Mohr-Coulomb Yield Criterion (Elasto-Plastic Model)
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For non-associated flow rule,
replace internal friction angle bydilution angle
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Sandip Shah,
Ph.D. Thesis,
Department of
Civil
Engineering,
University ofToronto
For Hoek- Brown Yield Criterion (Elasto-Plastic Model)
Carranza-Torresa C and Fairhurst C 1999 The elasto-plastic response
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Carranza-Torresa, C. and Fairhurst, C. 1999. The elasto-plastic response
of underground excavations in rock masses that satisfy the Hoek-Brown
failure criterion. International Journal of Rock Mechanics and Mining
Sciences, vol. 36, pp. 777-809.
Mohr Circles
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