DERIVATION OF STRAIN GRADIENT LENGTH VIA...
Transcript of DERIVATION OF STRAIN GRADIENT LENGTH VIA...
University of Thessaly Dept. of Civil Engineering
ICCESMM11
DERIVATION OF STRAIN GRADIENT LENGTH VIA HOMOGENIZATION OF HETEROGENEOUS
ELASTIC MATERIALS
A.Triantafyllou1,2 , A.E. Giannakopoulos2
1 Laboratory of Reinforced Concrete Technology and Structures2 Laboratory for Strength of Materials and Micromechanics
University of Thessaly Dept. of Civil Engineering
ICCESMM11
Introduction (1/2)
Gradient elasticity theories include an intrinsic length (ℓ) parameter and this allows these theories to capture the size effect that has been shown experimentally to exist in heterogeneous materials.
Constraint couple stress elasticity (or Cosserat theory)
Simplified dipolar elasticity theory (or grade-two theory)
gradient of rotations
gradient of the strains
In both theories the internal length is associated with the microstructure of the material (e.g. grain size, particle size, etc.).
University of Thessaly Dept. of Civil Engineering
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Introduction (2/2)
A typical composite material consists of a matrix and inclusions.
The aim of homogenization is to replace the composite material with an equivalent material of uniform macroscopic properties.
When gradient theories are considered, an additional material parameter, the internal length, is added. Nevertheless, the same strategy of homogenization can be used, only this time, to yield an estimate for this new parameter.
University of Thessaly Dept. of Civil Engineering
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Aim
Heterogeneous Cauchy material
Homogeneous gradient material
Estimate the characteristic length as function of the inclusion radius, volume fraction and elastic constants
University of Thessaly Dept. of Civil Engineering
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Plain Strain Classic Elasticity Solutions (1/3)
0
))(21(1
)()(2
1 222222
=
−−+−
−=
θ
νµ
u
rpbqar
pqabab
u mm
r
0
1)(
1)(
22
22
222
22
22
22
222
22
=−−
+−
−−=
−−
+−
−=
θ
θθ
σ
σ
σ
r
rr
ab
pbqa
rab
abqp
ab
pbqa
rab
abqp
drrU rrrr
b
cl )( θθθθα
εσεσπ += ∫
Circular ring subjected to normal uniform external and internal pressures
0rrr
r ur
u=
∂∂
br =at
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Classic Elasticity Solutions (2/3)
Rigid 0)( == arur
Void 0=q
Elastic
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Classic Elasticity Solutions (3/3)
Rigid
Void
Elastic
),,,()21)(1(2
)21()1(
122
22
22
1l
ll
lb
cfpcc
bpc
U mmmmm
mm
cl νµπννµ
ννπ×××=
−++
−−
−
=
),,,()1(2
)21(
222
222
2l
ll
lb
cfpc
cb
pU mm
m
m
cl νµπµ
νπ×××=
−
−+
=
[ ]),,,,,(
)21()21()1(
)1)(21(2
_322
2
2222
_3l
l
ll b
cfpccc
pb
cU iimmi
miim
mii
icl νµνµπνµνµ
ννπµ×××=
−++−−
−−
=
[ ][ ]
),,,,,(
)21(1)(21()21)(21()1(2)21()21(
)21()21()1(2
)1(
_322
222
2
222
_3
ll
ll
bcfp
ccc
ccc
pcb
U
iimmm
mmimimimim
miimm
mcl
νµνµπ
ννµννµµννµ
νµνµµ
π
×××=
−+−+−−−+−+−
×−++−−
−
=
University of Thessaly Dept. of Civil Engineering
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Gradient Solutions (1/3)
The elastic strain energy density function W that incorporates strain gradient effects is (for in-plane isotropy):
−
++−
+= )21
(21
),( 2ikkijjijkijkijijijijW κκ
νν
κκεεν
νεεµκε l
−
+=∂∂
= ijijijij
ij
Wδε
νν
εµε
τ21
2
−
+=∂∂
= jkippijkijk
ijk
Wδκ
νν
κµκ
λ21
2 2l
The stress and double stress quantities τ and λ are defined as follows:
( )drrU rrrrrrrrrr
b
agr θθθθθθθθθθ κλκλετετπ +++= ∫
The elastic energy of the gradient solution is: ijkijk x∂∂= /εκ
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Gradient Solutions (2/3)
−
−−
+
−−
−−±=4
26
213212261
2)21()21(
22)(
r
crI
rI
rc
rK
rK
rc
r
ccrPr
l
ll
l
ll
lνννν
−−
−+
−+
−−=ll
lll
lr
Ir
Icr
Kr
KcrRr 213212 )21()1()21()1()( νννν
qaPr −=)(
0)( =aRr
pbPr −=)(
0)( =bRr
The dynamic boundary conditions required by the principal of virtual work, are:
,
,
Boundary Conditions
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Gradient Solutions (3/3)
pbPr −=)(
,
,
Boundary Conditions for compact disc
0rrr
r ur
u=
∂∂
−
+
−
+
−
×+−=
llll
ll
bI
bI
bI
bI
bIb
upbc rrr
21220
0
3
22)21(
]2)21[(2
ννν
µν
[ ]
−
+
−
+
−
×+−
−
+
−=
llll
ll
llll
bI
bI
bI
bI
bIb
upb
Ib
Ib
I
crrr
21220
0212
7
22)21(
]2)21(24
ννν
µννν
028 == cc
Solution for the four constants involved in the annulus problem
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Summary
,
,
The energy of the heterogeneous material and the energy of the gradient homogeneous material were determined for the same boundary conditions.
Heterogeneous Cauchy material
Homogeneous
gradient material
grcl UU =
By equating the energies, we can derive an estimation of the internal length of the gradient material as a function of the inclusion radius α, the composition ratio c and the elastic constants of matrix and inclusion
University of Thessaly Dept. of Civil Engineering
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Classic effective material properties (1/2)
,
,
The Generalized Self Consistency Method has been shown to give good estimates not only for the case of dilute composition (c 0)but also for the limiting case of full packing of the inclusion phase (c 1).
In addition to the physical consistency of the results, it should be noted that the Generalized Self Consistent method is the only complete exact, closed form solution.
We will assume that these estimates for μ and v hold also for the gradient theory.
University of Thessaly Dept. of Civil Engineering
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Effective material properties (2/2)
,
,
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
5.0
0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100%
Composition, c
Sh
ear
mo
du
li r
atio
, μ
/μm
15/
10/
5/
5.2/
2/
5.1/
=
=
=
=
=
=
mi
mi
mi
mi
mi
mi
µµ
µµ
µµ
µµ
µµ
µµ
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Estimate of the internal length (1/5)
,
,
Assumption of a heterogeneous material with elastic properties, μm, νm, μi ,νi and composition c.
Estimation of effective in-plane elastic properties, μ and ν, corresponding to each problem (Christensen model)
Estimation of internal length based on solving grcl UU =
University of Thessaly Dept. of Civil Engineering
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Estimate of the internal length: Rigid Inclusions (3/5)
,
,
0
1
2
3
4
5
6
7
8
0.1% 1.0% 10.0% 100.0%
Composition, c
Gra
die
nt
inte
rnal
len
gth
to
in
clu
sio
n r
adiu
s ra
tio
, ℓ/α
25.0
20.0
15.0
10.0
=
=
=
=
m
m
m
m
ν
ν
ν
ν
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Estimate of the internal length: Elastic Inclusions (4/5)
,
,
0
1
2
3
4
5
6
7
0.1% 1.0% 10.0% 100.0%
Composition, c
Gra
die
nt
inte
rnal
len
gth
to
in
clu
sio
n r
adiu
s ra
tio
, ℓ/α
∞→
=
=
=
=
=
mi
mi
mi
mi
mi
mi
µµ
µµ
µµ
µµ
µµ
µµ
/
15/
10/
5/
5.2/
2/
Poisson ratio of the matrix and inclusion is 0.2 and 0.25 respectfully
University of Thessaly Dept. of Civil Engineering
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Estimate of the internal length: Porous materials (5/5)
,
,
The normalized internal length (b/ℓ) estimate for this case is of the order 10-8, for the majority of c values. It is also noted that for some values of c, the estimate of b/ℓ becomes negative. These results can not be acceptable since they lack physical justification. In other words, there can be no prediction for the internal length for the case of porous materials or generally when the inclusions are less stiff than the matrix.
University of Thessaly Dept. of Civil Engineering
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Conclusions
,
,
The homogenization of a heterogeneous Cauchy-elastic material was performed and the internal length parameter used in strain gradient theory was estimated. Specifically:
1. The maximum estimates were found when inclusions much stiffer than the matrix were considered.
2. The analysis was limited to the 2D case of fiber reinforced composites. The internal length was found to be between 0.5 and 7 times the inclusion radius, for small values of c, depending on the inclusion to matrix shear modulus ratio.
3. The internal length decreases rather rapidly as the composition is increased and is approximately zero for .
4. No prediction was possible for inclusions less stiff than the matrix and for the extreme case which corresponds to porous materials. The opposite has been found by Bigoni using Cosserat theory.
%70>c
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Remarks (1/2)
,
,
1. Lower bound results in the estimate of the internal length parameter
Energy optimization based on stress boundary conditions represent an upper bound estimate for the value of the estimated parameter, whereas estimates based on displacement boundary conditions represent a lower bound.
The lower bound estimate for this case is simply ℓ=0
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Remarks (2/2)
,
,
2. An important finding regarding the case of spherical particles
When the same methodology is applied to the case of spherical inclusions, one finds that the estimate of the internal length parameter when demanding equality of the two energies is always the trivial solution of b/ℓ=0.
In other words, the elastic energy of the homogeneous gradient material is always greater than the elastic energy of the heterogeneous Cauchy material and the difference between the two increases monotonically. The reason for this failure is that we have used spherically symmetric solutions for comparison fields.