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Draft4.3 Strain Decomposition 25Given x1= X1, x2=−3X3, x3= 2X2, find the deformation gradient F, the right stretch tensor U, the rotation tensor R, and the left stretch tensor V.. 4.6 Lag

Trang 1

Draft4.3 Strain Decomposition 25

Given x1= X1, x2=−3X3, x3= 2X2, find the deformation gradient F, the right stretch tensor U, the rotation tensor R, and the left stretch tensor V.

Solution:

From Eq 4.25

F =

∂x1

∂X1

∂x1

∂X2

∂x1

∂X3

∂x2

∂X1

∂x2

∂X2

∂x2

∂X3

∂x3

∂X1

∂x3

∂X2

∂x3

∂X3

 =

 10 00 −30

0 2 0

From Eq 4.126

U2= FTF =

 10 00 02

0 −3 0

 10 00 −30

0 2 0

 =

 10 04 00

0 0 9

thus

U =

 10 02 00

0 0 3

From Eq 4.127

R = FU−1=

 10 00 −30

0 2 0

 10 01 0

0 0 13

 =

 10 00 −10

0 1 0

Finally, from Eq 4.128

V = FRT =

 10 00 −30

0 2 0

 10 00 01

0 −1 0

 =

 10 03 00

0 0 2

Example 4-11: Polar Decomposition II

For the following deformation: x1= λ1X1, x2=−λ3X3, and x3= λ2X2, find the rotation tensor

Solution:

[F] =

λ01 00 −λ03

0 λ2 0

=

λ01 00 λ02

0 −λ3 0

λ01 00 −λ03

0 λ2 0

 =

λ

0 λ2 0

0 0 λ2

[U] =

λ01 λ02 00

0 0 λ3

[R] = [F][U]−1=

λ01 00 −λ03

0 λ2 0

1

0 λ12 0

0 0 λ13

 =

 10 00 −10

0 1 0

 (4.139)

Thus we note that R corresponds to a 90o rotation about the e1 axis

Trang 2

Example 4-12: Polar Decomposition III

Trang 3

Draft4.3 Strain Decomposition 27

Polar Decomposition Using Mathematica

Given x1=X1+2X2, x2=X2, x3=X3, a) Obtain C, b) the principal values of C and the corresponding directions, c) the

matrix U and U-1 with respect to the principal directions, d) Obtain the matrix U and U-1 with respect to the e i bas

obtain the matrix R with respect to the e i basis

Determine the F matrix

In[1]:= F= 881, 2, 0<, 80, 1, 0<, 80, 0, 1<<

Out[1]=

i k

jjjj jjj

1 2 0

0 1 0

0 0 1

y {

zzzz zzz

Solve for C

In[2]:= CST= Transpose@FD F

Out[2]=

i k

jjjj jjj

1 2 0

2 5 0

0 0 1

y {

zzzz zzz

Determine Eigenvalues and Eigenvectors

In[3]:= N@Eigenvalues@CSTDD

Out[3]= 81., 0.171573, 5.82843<

In[4]:= 8v1, v2, v3< = N@Eigenvectors@CSTD, 4D

Out[4]=

i k

jjjj jjj

0 0 1

-2.414 1 0 0.4142 1 0

y {

zzzz zzz

In[5]:= << LinearAlgebra‘Orthogonalization‘

In[6]:= vnormalized= GramSchmidt@8v3, −v2, v1<D

Out[6]=

i k

jjjj jjj

0.382683 0.92388 0 0.92388 -0.382683 0

y {

zzzz zzz

In[7]:= CSTeigen= Chop@N@vnormalized CST vnormalized, 4DD

Out[7]=

i k

jjjj jjj

5.828 0 0

0 0.1716 0

y {

zzzz zzz

Determine U with respect to the principal directions

In[8]:= Ueigen= N@Sqrt@CSTeigenD, 4D

Out[8]=

i k

jjjj jjj

2.414 0 0

0 0.4142 0

y {

zzzz zzz

In[9]:= Ueigenminus1= Inverse@UeigenD

Out[9]=

i k

jjjj jjj

0.414214 0 0

0 2.41421 0

0 0 1

y {

zzzz zzz

Determine U and U- 1with respect to the ei basis

In[10]:= U_e= N@vnormalized Ueigen vnormalized, 3D

Out[10]=

i k

jjjj jjj

0.707 0.707 0

0.707 2.12 0

0 0 1

y {

zzzz zzz

In[11]:= U_einverse= N@Inverse@%D, 3D

Out[11]=

i k

jjjj jjj

2.12 -0.707 0

-0.707 0.707 0

0 0 1

y {

zzzz zzz

Determine R with respect to the ei basis

In[12]:= R= N@F %, 3D

Out[12]=

i k

jjjj jjj

0.707 0.707 0

-0.707 0.707 0

0 0 1

y {

zzzz zzz

m−polar.nb

Trang 4

4.4 Summary and Discussion

92 From the above, we deduce the following observations:

1 If both the displacement gradients and the displacements themselves are small, then ∂u i

∂X j ≈ ∂u i

∂x j and

thus the Eulerian and the Lagrangian infinitesimal strain tensors may be taken as equal E ij = E ij ∗

2 If the displacement gradients are small, but the displacements are large, we should use the Eulerian infinitesimal representation

3 If the displacements gradients are large, but the displacements are small, use the Lagrangian finite strain representation

4 If both the displacement gradients and the displacements are large, use the Eulerian finite strain representation

4.5 Compatibility Equation

93 If ε ij = 12(u i,j + u j,i) then we have six differential equations (in 3D the strain tensor has a total

of 9 terms, but due to symmetry, there are 6 independent ones) for determining (upon integration)

three unknowns displacements u i Hence the system is overdetermined, and there must be some linear relations between the strains

94 It can be shown (through appropriate successive differentiation of the strain expression) that the compatibility relation for strain reduces to:

2ε ik

∂x j ∂x j +

2ε jj

∂x i ∂x k − ∂2ε jk

∂x i ∂x j − ∂2ε ij

∂x j ∂x k = 0 or x×L×∇x= 0 (4.140)

There are 81 equations in all, but only six are distinct

2ε11

2ε22

2ε12

∂x1∂x2 (4.141-a)

2ε22

2ε33

2ε23

∂x2∂x3 (4.141-b)

2ε33

2ε11

2ε31

∂x3∂x1 (4.141-c)

∂x1



− ∂ε23

∂ε31

∂ε12

∂x3



2ε11

∂x2∂x3 (4.141-d)

∂x2



∂ε23

∂ε12

∂x3



2ε22

∂x3∂x1 (4.141-e)

∂x3



∂ε23

∂ε31

∂x3



2ε33

∂x1∂x2 (4.141-f)

In 2D, this results in (by setting i = 2, j = 1 and l = 2):

2ε11

2ε22

2γ12

Trang 5

Draft4.5 Compatibility Equation 29

I , i

3 3

2

I , i

2

I , i

1 1

2 2

X , x

u

P

P

0 t=0

t=t

X

O

U

o

x

X , x

X , x

x2 ,

X3, x3

2

X

X1

O

x1 ,

u

x

t=0

+d

X X

X

+d

d

d x

t=t

X

u u

Q

0

Q

P P

0

Position Vector x = x(X, t) X = X(x, t)

GRADIENTS

Deformation F = xX≡ ∂x i

∂x j

H = F−1

Displacement ∂u i

∂X j = ∂x i

∂x j = δ ij − ∂X i

∂x j or

J = uX = F− I K≡ u∇x = I− H

TENSOR

Deformation B −1 ij =∂X k

∂x i

∂X k

∂X i

∂x k

∂X j or

B−1 =x X·X∇x = Hc ·H C =X x·x∇X = Fc ·F

C−1= B−1 STRAINS

Finite Strain E ij = 12



∂x k

∂X i

∂x k

∂X j − δ ij



or E ij ∗ =12



δ ij − ∂X k

∂x i

∂X k

∂x j

 or

E = 12(X x·x∇X

Fc ·F

Hc ·H

)

2



∂u i

∂X j + ∂u j

∂X i+ ∂u k

∂X i

∂u k

∂X j



or E ij ∗ =1

2



∂u i

∂x j +∂u j

∂x i − ∂u k

∂x i

∂u k

∂x j

 or

E = 12(uX+X u +X u·u∇X)

J+Jc+Jc ·J

E= 12(ux+x u− ∇x u·u∇x)

K+Kc −K c ·K

Small E ij = 12



∂u i

∂X j + ∂u j

∂X i



E ij ∗ =12



∂u i

∂x j +∂u j

∂x i



Deformation E = 12(uX+X u) = 12(J + Jc) E= 12(ux+x u) = 12(K + Kc)

ROTATION TENSORS

Small [12



∂u i

∂X j +∂u j

∂X i

 +12



∂u i

∂X j − ∂u j

∂X i



]dX j

#

1 2



∂u i

∂x j +∂u j

∂x i

 +12



∂u i

∂x j − ∂u j

∂x i

$

dx j

deformation [1

2(uX+X u)

E

+1

2(uX− ∇X u)

W

]·dX [1

2(ux+x u)

E

+1

2(ux− ∇x u)

]·dx

Finite Strain F = R·U = V·R

STRESS TENSORS

First T0= (det F)T%

F−1&T Second T = (det F)˜ %

F−1&

T%

F−1&T

Table 4.1: Summary of Major Equations

Trang 6

95 When he compatibility equation is written in term of the stresses, it yields:

2σ11

2σ22

∂x2 − ν ∂2σ11

∂x2 = 2 (1 + ν) ∂

2σ21

∂x1∂x2 (4.143)

Example 4-13: Strain Compatibility

For the following strain field 

X2

X2+X2

X1

2(X2+X2) 0

X1

does there exist a single-valued continuous displacement field?

Solution:

(X2+ X2)2 = X

2− X2

(X2+ X2)2 (4.145-a)

2∂E12

(X2+ X2)− X1(2X1)

(X2+ X2)2 = X

2− X2

(X2+ X2)2 (4.145-b)

1

⇒ ∂2E11

2E22

2E12

(4.145-d) Actually, it can be easily verified that the unique displacement field is given by

u1= arctanX2

X1; u2= 0; u3= 0 (4.146)

to which we could add the rigid body displacement field (if any)

4.6 Lagrangian Stresses; Piola Kirchoff Stress Tensors

96 In Sect 2.2 the discussion of stress applied to the deformed configuration dA (using spatial coordiantes

x), that is the one where equilibrium must hold The deformed configuration being the natural one in

which to characterize stress Hence we had

(note the use of T instead of σ) Hence the Cauchy stress tensor was really defined in the Eulerian

space

97 However, there are certain advantages in referring all quantities back to the undeformed configuration (Lagrangian) of the body because often that configuration has geometric features and symmetries that are lost through the deformation

98 Hence, if we were to define the strain in material coordinates (in terms of X), we need also to express the stress as a function of the material point X in material coordinates.

Trang 7

Draft4.6 Lagrangian Stresses; Piola Kirchoff Stress Tensors 31

99 The first Piola-Kirchoff stress tensor T0 is defined in the undeformed geometry in such a way that it

results in the same total force as the traction in the deformed configuration (where Cauchy’s stress

tensor was defined) Thus, we define

where t0 is a pseudo-stress vector in that being based on the undeformed area, it does not describe the actual intensity of the force, however it has the same direction as Cauchy’s stress vector t.

100 The first Piola-Kirchoff stress tensor (also known as Lagrangian Stress Tensor) is thus the linear transformation T0 such that

and for which

df = t0dA0= tdA ⇒ t0= dA

using Eq 4.147-b and 4.149 the preceding equation becomes

T0n0= dA

dA0Tn = T

dA

and using Eq 4.36 dAn = dA0(det F)%

F−1&T

n0 we obtain

T0n0= T(det F)%

F−1&T

the above equation is true for all n0, therefore

T0 = (det F)T%

F−1&T

(4.153)

(det F) T0F

T or T ij = 1

(det F)(T0)im F jm (4.154)

101 The first Piola-Kirchoff stress tensor is not symmetric in general, and is not energitically correct.

That is multiplying this stress tensor with the Green-Lagrange tensor will not be equal to the product

of the Cauchy stress tensor multiplied by the deformation strain tensor

102 To determine the corresponding stress vector, we solve for T0 first, then for dA0 and n0 from

dA0n0=det F1 FT n (assuming unit area dA), and finally t0= T0n0

103 The second Piola-Kirchoff stress tensor, ˜T is formulated differently Instead of the actual force df

on dA, it gives the force d˜ f related to the force df in the same way that a material vector dX at X is

related by the deformation to the corresponding spatial vector dx at x Thus, if we let

and

where d˜f is the pseudo differential force which transforms, under the deformation gradient F, the

(actual) differential force df at the deformed position (note similarity with dx = FdX) Thus, the

pseudo vector t is in general in a differnt direction than that of the Cauchy stress vector t.

104 The second Piola-Kirchoff stress tensor is a linear transformation ˜T such that

˜

Trang 8

df = F ˜ Tn0dA0 (4.157)

we also have from Eq 4.148 and 4.149

and comparing the last two equations we note that

˜

which gives the relationship between the first Piola-Kirchoff stress tensor T0 and the second Piola-Kirchoff stress tensor ˜T.

105 Finally the relation between the second Piola-Kirchoff stress tensor and the Cauchy stress tensor can

be obtained from the preceding equation and Eq 4.153

˜

T = (det F)%

F−1&

T%

F−1&T

(4.160)

and we note that this second Piola-Kirchoff stress tensor is always symmetric (if the Cauchy stress tensor

is symmetric) It can also be shown that it is energitically correct

106 To determine the corresponding stress vector, we solve for ˜T first, then for dA0and n0from dA0n0=

1

det F FT n (assuming unit area dA), and finally ˜t = ˜ Tn0

Example 4-14: Piola-Kirchoff Stress Tensors

4.7 Hydrostatic and Deviatoric Strain

85 The lagrangian and Eulerian linear strain tensors can each be split into spherical and deviator

tensor as was the case for the stresses Hence, if we define

1

3e =

1

then the components of the strain deviator E are given by

E ij  = E ij −1

3eδ ij or E

= E1

We note that E measures the change in shape of an element, while the spherical or hydrostatic strain

1

Trang 9

Draft4.7 Hydrostatic and Deviatoric Strain 33

Piola−Kirchoff Stress Tensors

The deformed configuration of a body is described by x1=X1ê 2, x2=−X2/2, x3=4X3 ; If the Cauchy stress tensor is

given by

i k

jjjj jjjj

100 0 0 0

0 0

0 0 0 y {

zzzz zzzz MPa; What are the corresponding first and second Piola−Kirchoff stress tensors, and calculate the

respective stress tensors on the e3 plane in the deformed state.

‡ F tensor

CST= 880, 0, 0<, 80, 0, 0<, 80, 0, 100<<

880, 0, 0<, 80, 0, 0<, 80, 0, 100<<

F= 881 ê 2, 0, 0<, 80, 0, −1 ê 2<, 80, 4, 0<<

99 ÄÄÄÄÄ1

2, 0, 0=, 90, 0, - ÄÄÄÄÄ1

2 =,80, 4, 0<=

982, 0, 0<, 90, 0, ÄÄÄÄÄ1

4 =,80, -2, 0<=

‡ First Piola−Kirchoff Stress Tensor

880, 0, 0<, 80, 0, 0<, 80, 25, 0<<

i k

j j

y {

z z

‡ Second Piola−Kirchoff Stress Tensor

980, 0, 0<, 90, ÄÄÄÄÄÄÄÄ25

4 , 0=, 80, 0, 0<=

i k

j j

0 ÄÄÄÄÄÄ254 0

y {

z z

‡ Cuchy stress vector

Can be obtained from t=CST n

i k

j j

0 0 100 y {

z z

‡ Pseudo−Stress vector associated with the First Piola−Kirchoff stress tensor

For a unit area in the deformed state in the e3direction, its undeformed area dA0n0is given by dA0n0 = ÄÄÄÄÄÄÄÄÄÄÄÄÄÄÄF det F T n

detF= Det@FD

1

n= 80, 0, 1<

80, 0, 1<

i k

j j

0 4 0 y {

z z

Thus n0=e2and using t0=T0 n0 we obtain

i k

j j

0 0 25 y {

z z

We note that this vector is in the same direction as the Cauchy stress vector, its magnitude is one fourth of that of the

Cauchy stress vector, because the undeformed area is 4 times that of the deformed area

‡ Pseudo−Stress vector associated with the Second Piola−Kirchoff stress

tensor

i k

j j

0 25 ÄÄÄÄÄÄ4 0 y {

z z

We see that this pseudo stress vector is in a different direction from that of the Cauchy stress vector (and we note that

the tensor F transforms e2into e3 ).

Trang 10

εI

ε ε

2

Figure 4.8: Mohr Circle for Strain

4.8 Principal Strains, Strain Invariants, Mohr Circle

86 Determination of the principal strains (E(3)< E(2)< E(1), strain invariants and the Mohr circle for strain parallel the one for stresses (Sect 2.3) and will not be repeated here

where the symbols I E , II E and III E denote the following scalar expressions in the strain components:

I E = E11+ E22+ E33= E ii = tr E (4.164)

II E = −(E11E22+ E22E33+ E33E11) + E232 + E312 + E122 (4.165)

= 1

2(E ij E ij − E ii E jj) = 1

2E ij E ij −1

2I

2

= 1

2(E : E− I2

III E = detE =1

6e ijk e pqr E ip E jq E kr (4.168)

87 In terms of the principal strains, those invariants can be simplified into

I E = E(1)+ E(2)+ E(3) (4.169)

II E = −(E(1)E(2)+ E(2)E(3)+ E(3)E(1)) (4.170)

III E = E(1)E(2)E(3) (4.171)

88 The Mohr circle uses the Engineering shear strain definition of Eq 4.91, Fig 4.8

Example 4-15: Strain Invariants & Principal Strains

Trang 11

Draft4.8 Principal Strains, Strain Invariants, Mohr Circle 35

Determine the planes of principal strains for the following strain tensor

 1

3 0

3 0 0

Solution:

The strain invariants are given by

The principal strains by

 1− λ

0 0 1− λ

= (1− λ)

'

13 2

( '

13 2

(

(4.174-b)

13

The eigenvectors for E(1)= 1+213 give the principal directions n(1):

11+

13 2

3 1+

13

13 2

n(1)1

n(1)2

n(1)3

=



11+

13 2



n(1)1 +

3n(1)2

3n(1)1 1+

13 2



n(1)2



11+

13 2



n(1)3

=

0 0 0

 (4.175) which gives

13

2

3 n

(1)

n(1)·n(1) =

'

1 + 2

13 + 13

12 + 1

( 

n(1)2

2

= 1⇒ n1

2= 0.8; (4.176-c)

For the second eigenvector λ(2)= 1:

 1− 1

0 0 1− 1

n(2)1

n(2)2

n(2)3

=

3n(2)2

3n(2)1 − n(2)

2

0

=

0 0 0

which gives (with the requirement that n(2)·n(2) = 1)

Trang 12

n(3)= n(1)×n(2) = det







e1 e2 e3

0.8 0.6 0





= 0.6e1− 0.8e2 (4.179) Therefore

a j i =

n(1)

n(2)

n(3)

=

0.80 0.60 01

and this results can be checked via

[a][E][a]T =

0.80 0.60 01

 1

3 0

3 0 0

0.8 0.6 00 −0.8 0.6

 =

2.30 01 00

0 0 −1.3

 (4.181)

Example 4-16: Mohr’s Circle

Construct the Mohr’s circle for the following plane strain case:

 00 05 03

0

3 3

Solution:

1 2 1

60o 2 B

D

E

F

ε

ε s

n

2 3

We note that since E(1) = 0 is a principal value for plane strain, ttwo of the circles are drawn as shown

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