소성재료역학 (metal plasticity) chapter 12: yield function 8... · 2019. 9. 5. · 446.631a...
TRANSCRIPT
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446.631A
소성재료역학(Metal Plasticity)
Chapter 12: Yield Function
Myoung-Gyu Lee
Office: Eng building 33-309
Tel. 02-880-1711
TA: Chanyang Kim (30-522)
mailto:[email protected]
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Three-dimensional plasticity
1-D constitutive law Stresses and strains in 3-D
General state : multiple components existTensionCompressionBending….
ε
σ
σxx σyy
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Three-dimensional plasticity
Stress and Strain tensorTensor : mathematical notation of physical quantities
Stress : symmetric 2nd order tensor
• 0 th order Tensor : scalar value – energy, etc• 1st order Tensor : vector - force, displacement, velocity, etc• 2nd order Tensor : linear transformation from vector to the other vector
- stress, strain, etc.
xx yx zx
xy yy zy
xz yz zz
σ
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Three-dimensional plasticity
1-D : point 2-D : line 3-D : surface
I
II
( ,0,0)ST Y
2 or 2(2 , ,0)PS PLS K K
( , ,0)BB B B
3 or 3( , ,0)PS PLS K K
ε
σ
For isotropic case,
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Basic features of the yield surface
Concept of material coordinates
(or materially embedded coordinates)
𝑥′
𝑦′ 𝑦
𝑥
p
Global coordinates system
(or laboratory coordinates system)
𝑥
𝑦
Material coordinates system
• Since the constitutive law describes material properties, components of
vector or tensor quantities are defined with respect to material coordinates
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Basic features of the yield surface
Convexity of yield surface
(a) (b)
Convex Non-convex
• The yield surface is considered to be convex
• In other words, yield surface should be bulged out
• Or, any straight line connecting two points located inside the surface stays
inside the surface
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Basic features of the yield surface
• For the simplicity, consider a 2-D imaginary yield surface
( ) ( , ) xx yyf f constant C
• Size of yield function f(σ) is defined by constant C
• For the isotropic case, yield function can be assumed as a circle
• For the anisotropic case, ellipse can be an yield function
2 2 1/2
1
2 2 2 2
2
( ) ( ) c
( ) ( ) c
xx yy
xx yy
f
f
1
2 2 21 1
1
2 2 22 2
2 2 2
3
2 2 2
4
( ) ( ) ( ( ) )
( ) ( ) (( ) )
( ) ( ( ) )
( ) (( ) )
yy
xx
xxyy
yy
xx
xxyy
af a
b
bf b
a
af a
b
bf b
a
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Basic features of the yield surface
n-th order homogeneous function
( ) ( )nf f x x Bold : vector or tensor
Two properties of n-th order homogeneous function
i) (n-1)-th order homogeneous function
or
ii)
f
x
( ) ( )i ij
i ij
f f fx or x nf
x x
x x
x
1 1 1
1 1
1 1 1
( )and ( )
( )
n n nn n
n n n
nx n x nxf
ny n y ny
g g gxx
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Basic features of the yield surface
Proof (1)
( ) ( ) nf fx x
( ) ( ) ( ) ( )( )
( ) ( )
( x )( x )
x
f x f f
fwhere
g
g
x x xI x
x x x x
Left hand side
Right hand side
( )( )n n
f
g
xx
x
1( ) ( ) ng gx x
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Basic features of the yield surface
Proof (2)
( ) ( ) nf fx x
( ) ( ) ( ) ( )( )
( ) ( )
f x f f
g
x x xx x x
x x
Left hand side
Right hand side
1
( )( )
n
nf
n f
xx
( )( )
fnf
xx x
x
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Basic features of the yield surface
• Linear transformation of isotropic yield surface into anisotropic yield
surface – preserve the convexity
/ 0
0 /
xx xx
yy yy
c a
c b
• Effective stress or equivalent stress –
the yield function of the first order homogeneous function
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Basic features of the yield surface
Expansion, translation, shape change of yield surface
Expansion Translation Shape change(distortion)
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Appendix
Principal stress and invariants
Coordinates transformation Principal
axis
Generalcoordinates
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Appendix
Principal values and directions of symmetric tensor
= Eigenvalues and eigenvectors
( ) 0
,
det 0
ij ij ior n
for the non trivial solution
σn n σ I n 0
σ I
Where λ : principal values (or eigenvalues) of tensorn : principal directions(or eigenvectors) of tensor
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Appendix
Principal values & vectors and Invariants
= Do not change with any coordinates system
3 2 2
1 2 3
1 2 3
1
2 2
2
3
det 0,charactoristicequation is
0
where , , areinvariants of tensor
( )
1( ) ( )
2
det( )
from
I I I
I I I
I trace
I trace trace
I
σ I
σ
σ σ
σ
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Yield function - IsotropyIsotropic generalization
1 2 3
( )
( , , , , , )
( , , )
= ( , , )
ij
I II III I II III
I II III
f
f
f as a symmetric function
f I I I
n n n
General case
Isotropic case
Denote with invariants
1 2 3
where , , :
, , :
, , : the threeinvariants of
I II III
I II III
pricipal stresses
principal directions
I I I
n n n
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Yield function - Incompressibility
Hydrostatic & deviatoric stresses
• Decomposition of the stress into two components: the hydrostatic
and deviatoric components
11 22 33
1 where
3
1( )
3
:deviatric stress
ij ij kk ij kkS
trace
S I
S
11 22 33
12 1311 22 33
22 33 11
21 23
11 22 33
33 11 22
31 32
11 22 33
2
0 03
2 1
0 03 3
2
3 0 0
ij
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Yield function - Incompressibility
Deviatoric strains
Similarly,1
( )3
: ( )
: ( )
( ) 0 ( )
p p p
p
p
p p
kk
d d trace d
d plastic strain increment
d deviatoric plastic strain increment
trace d de for crystaline materials
e I
e
e
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Yield function - IncompressibilityHydrostatic & deviatoric stresses - example
III 33,
I 11,
II 22,
P
O
H
HL(Hydrostatic Line) (1, 1, 1)
H
S
Deviatoric plane(Octahedral plane) (1, 1, 1)
11 12 13 11 12 13
21 22 23 21 22 23
31 32 33 31 32 33
23 23 3211 11
22 22 31 31 13
33 33 12 12 21
1 0 0
0 1 0
0 0 1
1
1 with
1
S S S
S S S A
S S S
S SS
S A S S
S S S
, , S HNow from the figure
T
1 11 1
1 13 3
1 1
H
1 1
1 13
1 1
ii A
1
3A trace [111]H
11 22 33 11
11 22 33 22
11 22 33 33
21
23
2
S
S
S
S H
T
11 22 33
1
0 1 0
1
SS S S
[111]S
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Yield function - Incompressibility
Yield surface for incompressible case
• For crystal materials, plastic deformation is incompressible and
the hydrostatic stress does not affect the plastic deformation
since the plastic deformation is incurred by shear stress.
0
( ) is independent of
( ) ( , ) ( )
p
kk kk
p p
ij ij
ij kk
ij ij kk ij
d for arbitrary
dW S de
f f
f f f S f f S
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Isotropic & Incompressible yield surface
1 2 3
2 3
( )
( )
( , , , , , )
= ( , , ) as a symmetric function
= ( , , )
= ( , )
ij
ij
S S S
I II III I II III
I II III
f
f S
f S S S n n n
f S S S
f J J J
f J J
General case
Isotropic case
Denote with invariants
incompressible case
Since J1 = 0
1 2 3
1
2 2
2
3
where , , areinvariantsof deviatoric tensor
( ) 0
1( ) ( )
2
det( )
J J J
J trace
J trace trace
J
S
S S
S
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Incompressibility
π-diagram
I II
III
A
BB
A
I( )Pd II( )
Pd
III( )Pd
O
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Incompressibility
π-diagram
A way to find the deviatoric stress component: S1, S2 and S3 (with the condition
Sii=0):3,III 3,III( )S
2,II 2,II( )S1,I 1,I( )S
(2,1,0)
'(3,2,1)
(1,0, 1)SThey all share the same position on the
deviatoric plane (therefore, in the
diagram), but with different
hydrostatic component
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Von Mises isotropic yield function
2 2 2 2
2 3 2
1 1 1( ) ( ) ( , ) ( ) .
2 2 2 ij ij I II IIIf f f J J J S S S S S ConstS S
(or J2 plasticity)
From above, yield function can be defined like in below
( ) ( ) ( ) ij ijf S S c S
Where 𝜎 : equivalent(or effective) stress
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Reference stress state
( ) ( ) ( ) ij ijf S S cS
How can we define the size of yield function c? From reference state
I
II
( ,0,0)ST Y
2 or 2(2 , ,0)PS PLS K K
( , ,0)BB B B
3 or 3( , ,0)PS PLS K K
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Reference stress state
I II
III
2: ( , , )
3 3 3
Y Y YS
Y
: ( ,0,0)Y
I II
III
B
B
2: ( , , )
3 3 3
B B BS
: ( , ,0)B B
I II
III
K
: ( , ,0)S K K
: ( , ,0)K K
I II
III
: ( ,0, )S K K
K
: (2 , ,0)K K
Simple tension Pure shear(PS2)
Pure shear(PS3) Balanced biaxial
I
II
( ,0,0)ST Y
2 or 2(2 , ,0)PS PLS K K
( , ,0)BB B B
3 or 3( , ,0)PS PLS K K
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Reference stress state
( ) ij ijf S S
Reference state : simple tension case
For the reference state to calibrate the yield criterion is the simple tension,
1
3
0 0 2 3 0 0 3 0 0
0 0 0 0 3 0 0 3 0
0 0 0 0 0 3 0 0 3
( yield stress of the simple tension)
ij ij kk ijS
Y Y Y
Y Y
Y Y
f Y
2 2 24 1 1
9 9 9
3
2
f Y Y Y Y
3
2
ij ijS S Y
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Reference stress state
( ) ij ijf S S
Reference state : pure shear case
For the reference state to calibrate the yield criterion is the pure shear,
1
3
0 0 0 0 0 0 0
0 0 0 0 0 0 0
0 0 0 0 0 0 0 0 0
( yield stress of the pure shear)
ij ij kk ijS
K K
K K
f K
2 2
1
2
f K K K
1 1
2 3ij ijS S K Y
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Reference stress state
( ) ij ijf S S
Reference state : balanced biaxial case
For the reference state to calibrate the yield criterion is the balanced biaxial,
1
3
0 0 3 0 0 2 3 0 0
0 0 0 3 0 0 2 3 0
0 0 0 0 0 2 3 0 0 2 3
( yield stress of balanced biaxial tension)
ij ij kk ijS
B B B
B B B
B B
f B
2 2 21 1 4
9 9 9
3
2
f B B B B
3
32
ij ijS S B Y K
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Von Mises yield criterion
2 22 2 2 2
11 22 22 33 33 11 12 23 31
1 6 6 62
Y
22 2 2 2 2 2
11 22 33 12 23 31 11 22 33
2 2 2 2 2
11 22 22 33 33 11 12 23
( )=
3 =
2
3 3 1 1 ( )( )2 2 3 3
3 1 2 3
3 2 2 2 1 32
1 6 6
2
ij ij
ij ij
ij ij ij kk ij ij pp ij
ij ij kk pp
f f f S
f S S
f S S
2316
In summary,
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Tresca isotropic yield function
(or maximum shear criterion)
max min max min( ) ( ) ( , , )2 2
I II III
S Sf f S S S KS
2
2
2
I II I II
II III II III
I III I III
S S K
S S K
S S K
3 2 2 2 4 6
2 3 2 2
1 27 9 3J - J - 0
16 64 16 2 or K J K J K
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Tresca yield function
max min max min
2 2
S Sf A A
Different reference state cases
I II
III
Y
2: ( , , )
3 3 3
Y Y YS
: ( ,0,0)Y
I II
III
B
B
2: ( , , )
3 3 3
B B BS
: ( , ,0)B B
I II
III
K
: ( , ,0)S K K
: ( , ,0)K K
I II
III
: ( ,0, )S K K
K
: (2 , ,0)K K
Pure shear(PS3) Pure shear(PS2)
Simple tension Balanced biaxial
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Tresca yield functionReference state : pure shear case
For the reference state to calibrate the yield criterion is the pure shear,
max min max min
2 2
S Sf A A
max min .2
f A
0 0 0 0
0 0 0 0
0 0 0 0 0 0
K K
K K
( yield stress of the pure shear)K
( )
2
1
K Kf A K
A
max min 2 2
YK
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Tresca yield functionReference state : simple tension case
For the reference state to calibrate the yield criterion is the simple tension,
max min max min
2 2
S Sf A A
0 0
0 0 0
0 0 0
Y
0
2
2
Yf A Y
A
max min ( )Y
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Tresca yield functionReference state : balanced biaxial
max min max min
2 2
S Sf A A
max min 2
f A B
0 0
0 0
0 0 0
B
B
0
2
2
Bf A B
A
max min B
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Drucker isotropic yield function
26 3 63
2 3 2 3 2 3
2
( ) ( ) ( , ) ( , ) (1 )J
f f f J J J J J KJ
S
• Incompressible, isotropic, and symmetric for tension and compression,
• If ξ=0 von Mises yield criterion
• So, Drucker yield criterion is extension of von Mises yield criterion, which
modifies the shape of yield surface from the von Mises yield surface by
material constant ξ
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Drucker isotropic yield function2
6 3 632 3 2 3 2 3
2
( ) ( ) ( , ) ( , ) (1 )J
f f f J J J J J KJ
S
• 𝐽32/𝐽2
2 from 𝛼 = −1(pure shear) to 𝛼 = 0(simple tension)
22
2
3
3
22
3
332
2
13
2 2 1 127
2 2 1 1
27 1
I
I
J
J
J
J
• Let 𝜎1, 𝜎2, 0 → 𝜎1 1, 𝛼, 0where 𝛼 = 𝜎2/𝜎1 (−1 ≤ 𝛼 ≤ 0)
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Drucker isotropic yield function
26 3 63
2 3 2 3 2 3
2
( ) ( ) ( , ) ( , ) (1 )J
f f f J J J J J KJ
S
22
2
3
3
22
3
332
2
13
2 2 1 127
2 2 1 1
27 1
I
I
J
J
J
J
1
62
32
32
2 2 1 1( , ) 3 1 1
27 1I K
• Principal stress σI can be derived as follows
( 0, ) ( )I Y B • Since and , ( 1, )I K
6 6 62 2
27 4 27 4
27 27K Y B
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Drucker isotropic yield function
( , )I • By normalizing with which is von Mises yield function case, ( , 0)I
11
2 62 63
3 32
2
2 2 1 1( , )1 1
( , 0) 27 1
I
I
J
J
• From convexity condition, 27 9
8 4
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Drucker isotropic yield function
• From previously driven equations, Drucker isotropic yield function can be plotted
In plane stress condition In π diagram
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Non-quadratic isotropic yield functiongeneralized from von Mises yield function
1
2 2 2 2
I II II III III I S S S S S S
Von Mises yield function
generalization
1
I II II III III I
M M M MS S S S S S
Hosford non-quadratic isotropic yield function
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Non-quadratic isotropic yield functiongeneralized from von Mises yield function
1
I II II III III I
M M M MS S S S S S
Hosford non-quadratic isotropic yield function in plane stress condition
Case 1 : 1 ≤ M ≤ 2 Case 2 : 2 ≤ M ≤ ∞
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Hill 1948 quadratic anisotropic yield function
2 2 2 2
2 2 2
( ) F( ) G( ) H( )
2L 2M 2N
yy zz zz xx xx yy
yz zx xy
f
• Anisotropic expansion of von Mises yield criterion• This will be further discussed in Chapter 14
Von Mises
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Drucker-Prager compressibleisotropic yield function
Deviatoric plane
oII
III
I
Hydrostatic Line (1, 1, 1)
oII
III
I
Hydrostatic Line (1, 1, 1)
Deviatoric plane
1 2 3 1 2 3 2 1( , , ) ( , , ) 2 +I I I I J I J I
• Drucker-Prager yield function can be utilized for Soil, Concrete, or other hydrostatic stress dependent materials
Case 1 : β>0 Case 2 : β
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Drucker-Prager compressibleisotropic yield function• Variation of Drucker-Prager yield criterion
2 12 +J I
Double cone shape
Deviatoric plane
o
III
I
Hydrostatic Line (1, 1, 1)
II
Ellipsoid shape
2
2 12 +J I
Deviatoric plane
o
III
I
Hydrostatic Line (1, 1, 1)
II