micromorphic crystal plasticity - sorbonne-universite.fr

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Micromorphic Crystal Plasticity Samuel Forest, Nicolas Cordero, Ana¨ ıs Gaubert * , Esteban Busso Mines ParisTech / CNRS Centre des Mat´ eriaux/UMR 7633 BP 87, 91003 Evry, France [email protected] * ONERA, 29, Av. de la Division Leclerc, F–92322 Chˆ atillon, France

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Page 1: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Micromorphic Crystal Plasticity

Samuel Forest, Nicolas Cordero, Anaıs Gaubert∗, Esteban Busso

Mines ParisTech / CNRSCentre des Materiaux/UMR 7633

BP 87, 91003 Evry, [email protected]

∗ ONERA, 29, Av. de la Division Leclerc, F–92322 Chatillon, France

Page 2: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 3: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 4: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 5: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Enhancing classical continuum mechanicsWithin the framework of generalized continuum mechanics, weintroduce additional degrees of freedom

DOF = u , χ∼

p

where χ∼

p is a generally non compatible plastic microdeformationtensor.In a first gradient theory, only the first gradients of the DOFintervene in the model

GRAD = F∼ := 1∼ + u ⊗∇X , K∼ := Curl χ∼

p

In the context of crystal plasticity, only the curl part of the plasticmicrodeformation is considered, instead of its full gradient.The following definition of the Curl operator is adopted:

K∼ := Curl χ∼

p :=∂χ∼

p

∂Xk× e k , Kij := εjkl

∂χpik

∂Xl

The “microcurl” model 5/54

Page 6: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Method of virtual powerThe method of virtual power is used to derive the balance andboundary conditions, following [Germain, 1973].

• Power density of internal forces; it is a linear form withrespect to the velocity fields and their Eulerian gradients:

p(i) = σ∼ : (u ⊗∇x) + s∼ : ˙χ∼

p+ M∼ : curl ˙χ

p, ∀x ∈ V

where the conjugate quantities are the Cauchy stress tensorσ∼ , which is symmetric for objectivity reasons, the microstresstensor, s∼, and the generalized couple stress tensor M∼ . Thecurl of the microdeformation rate is defined as

curl ˙χ∼

p:= εjkl

∂ ˙χpik

∂xle i ⊗ e j = K∼ · F∼

−1

The “microcurl” model 6/54

Page 7: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Method of virtual powerThe method of virtual power is used to derive the balance andboundary conditions, following [Germain, 1973].

• Power density of contact forces;

p(c) = t · u + m∼ : ˙χ∼

p, ∀x ∈ ∂V

where t is the usual simple traction vector and m∼ the doubletraction tensor.

The “microcurl” model 7/54

Page 8: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Method of virtual powerThe method of virtual power is used to derive the balance andboundary conditions, following [Germain, 1973].

• Application of the principle of virtual power, in the absenceof volume forces and in the static case, for brevity:

−∫

Dp(i) dV +

∫∂D

p(c) dS = 0

for all virtual fields u , ˙χ∼

p, and any subdomain D ⊂ V .

The “microcurl” model 8/54

Page 9: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Method of virtual powerThe method of virtual power is used to derive the balance andboundary conditions, following [Germain, 1973].

• Application of the principle of virtual power, in the absenceof volume forces and in the static case, for brevity:

−∫

Dp(i) dV +

∫∂D

p(c) dS = 0

for all virtual fields u , ˙χ∼

p, and any subdomain D ⊂ V .

• By application of Gauss divergence theorem, assumingsufficient regularity of the fields, this statement expands into:∫

V

∂σij

∂xjui dV +

∫V

(εkjl

∂Mik

∂xl− sij

)˙χpij dV

+

∫∂V

(ti − σijnj) ui dS+

∫∂V

(mik − εjklMijnl) ˙χpik dS = 0, ∀ui ,∀ ˙χp

ij

The “microcurl” model 9/54

Page 10: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Method of virtual power

This leads to the two field equations of balance of momentum andgeneralized balance of moment of momentum:

div σ∼ = 0, curlM∼ + s∼ = 0, ∀x ∈ V

and two boundary conditions

t = σ∼ · n , m∼ = M∼ · ε∼· n , ∀x ∈ ∂V

the index notation of the latter relation being mij = Mikεkjlnl .

The “microcurl” model 10/54

Page 11: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 12: Micromorphic Crystal Plasticity - sorbonne-universite.fr

State variables

• The deformation gradient is decomposed into elastic and plastic parts inthe form F∼ = E∼ · P∼

• The elastic strain is defined as E∼e := 1

2(E∼

T · E∼ − 1∼)

The “microcurl” model 12/54

Page 13: Micromorphic Crystal Plasticity - sorbonne-universite.fr

State variables

• The deformation gradient is decomposed into elastic and plastic parts inthe form F∼ = E∼ · P∼

• The elastic strain is defined as E∼e := 1

2(E∼

T · E∼ − 1∼)

• The microdeformation is linked to the plastic deformation via theintroduction of a relative deformation measure defined as

e∼p := P∼

−1 · χ∼

p − 1∼

It measures the departure of the microdeformation from the plasticdeformation, which is associated with a cost in the free energy potential.When e∼

p ≡ 0, the microdeformation coincides with plastic deformation.

The “microcurl” model 13/54

Page 14: Micromorphic Crystal Plasticity - sorbonne-universite.fr

State variables

• The deformation gradient is decomposed into elastic and plastic parts inthe form F∼ = E∼ · P∼

• The elastic strain is defined as E∼e := 1

2(E∼

T · E∼ − 1∼)

• The microdeformation is linked to the plastic deformation via theintroduction of a relative deformation measure defined as

e∼p := P∼

−1 · χ∼

p − 1∼

It measures the departure of the microdeformation from the plasticdeformation, which is associated with a cost in the free energy potential.When e∼

p ≡ 0, the microdeformation coincides with plastic deformation.

• The state variables are assumed to be the elastic strain, the relativedeformation, the curl of microdeformation and some internal variables, α:

STATE := E∼e , e∼

p, K∼, αThe specific Helmholtz free energy density, ψ, is a function of thesevariables. In this simple version of the model, the curl ofmicrodeformation is assumed to contribute entirely to the stored energy.

The “microcurl” model 14/54

Page 15: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Entropy principleThe dissipation rate density is the difference:

D := p(i) − ρψ ≥ 0

which must be positive according to the second principle of thermodynamics.

When the previous strain measures are introduced, the power density of

internal forces takes the following form:

p(i) = σ∼ : E∼ · E∼−1 + σ∼ : E∼ · P∼ · P∼

−1 · E∼−1

+ s∼ : (P∼ · e∼p + P∼ · e∼

p) + M∼ : K∼ · F∼−1

ρiΠ∼

e : E∼e+ρ

ρiΠ∼

M : P∼ · P∼−1

+ s∼ : (P∼ · e∼p + P∼ · e∼

p) + M∼ : K∼ · F∼−1

where Π∼e is the second Piola–Kirchhoff stress tensor with respect to the

intermediate configuration and Π∼M is the Mandel stress tensor:

Π∼e := JeE∼

−1 · σ∼ · E∼−T , Π∼

M := JeE∼T · σ∼ · E∼

−T = E∼T · E∼ ·Π∼

e

The “microcurl” model 15/54

Page 16: Micromorphic Crystal Plasticity - sorbonne-universite.fr

State lawsOn the other hand,

ρψ = ρ∂ψ

∂E∼e : E∼

e+ ρ

∂ψ

∂e∼p

: e∼p + ρ

∂ψ

∂K∼: K∼ + ρ

∂ψ

∂αα

We compute

JeD = (Π∼e − ρi

∂ψ

∂E∼e ) : E∼

e+ (JeP∼

T · s∼− ρi∂ψ

∂e∼p) : e∼

p

+ (JeM∼ · F∼−T − ρi

∂ψ

∂K∼) : K∼

+ (Π∼M + Jes∼ · χ∼

pT ) : P∼ · P∼−1 − ρi

∂ψ

∂αα ≥ 0

Assuming that the processes associated with E∼e, e∼

p and K∼ arenon–dissipative, the state laws are obtained:

Π∼e = ρi

∂ψ

∂E∼e , s∼ = J−1

e P∼−T · ρi

∂ψ

∂e∼p, M∼ = J−1

e ρi∂ψ

∂K∼· F∼

T

The “microcurl” model 16/54

Page 17: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Evolution lawsThe residual dissipation rate is

JeD = (Π∼M + Jes∼ · χ∼

pT ) : P∼ · P∼−1 − Rα ≥ 0, with R := ρi

∂ψ

∂αAt this stage, a dissipation potential, function of stress measures,Ω(S∼ ,R), is introduced in order to formulate the evolutionequations for plastic flow and internal variables:

P∼ · P∼−1 =

∂Ω

∂S∼, with S∼ := Π∼

M + Jes∼ · χ∼pT

α = −∂Ω

∂Rwhere R is the thermodynamic force associated with the internalvariable α, and S∼ is the effective stress conjugate to plastic strainrate, the driving force for plastic flow.

The “microcurl” model 17/54

Page 18: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 19: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Application to crystal plasticityIn the case of crystal plasticity, a generalized Schmid law is adopted for each

slip system s in the form:

f s(S∼ , τsc ) = |S∼ : N∼

s | − τ sc ≥ 0, with N∼

s = l s ⊗ n s

for activation of slip system s with slip direction, l s , and normal to the slip

plane, n s . We call N∼s the orientation tensor. The critical resolved shear stress

is τ sc which may be a function of R in the presence of isotropic hardening.

The “microcurl” model 19/54

Page 20: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Application to crystal plasticityIn the case of crystal plasticity, a generalized Schmid law is adopted for each

slip system s in the form:

f s(S∼ , τsc ) = |S∼ : N∼

s | − τ sc ≥ 0, with N∼

s = l s ⊗ n s

for activation of slip system s with slip direction, l s , and normal to the slipplane, n s . We call N∼

s the orientation tensor. The critical resolved shear stressis τ s

c which may be a function of R in the presence of isotropic hardening.

The generalized resolved shear stress can be decomposed into two

contributions:

S∼ : N∼s = τ s−x s , with τ s = Π∼

M : N∼s and x s = −s∼·χ∼

pT : N∼s

The usual resolved shear stress is τ s whereas x s can be interpreted as aninternal stress or back–stress leading to kinematic hardening. [Steinmann, 1996]

The back–stress component is induced by the microstress s∼ or, equivalently, by

the curl of the generalized couple stress tensor, M∼ , via the balance equation

x s = curlM∼ · χ∼

pT : N∼s

The “microcurl” model 20/54

Page 21: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Application to crystal plasticity

In the case of crystal plasticity, a generalized Schmid law isadopted for each slip system s in the form:

f s(S∼ , τsc ) = |S∼ : N∼

s | − τ sc ≥ 0, with N∼

s = l s ⊗ n s

for activation of slip system s with slip direction, l s , and normal tothe slip plane, n s . The critical resolved shear stress is τ s

c whichmay be a function of R in the presence of isotropic hardening. Thekinematics of plastic slip follows from the choice of a dissipationpotential, Ω(f s), that depends on the stress variables through theyield function itself, f s :

F∼p·F∼

p−1 =N∑

s=1

∂Ω

∂f s

∂f s

∂S∼=

N∑s=1

γs N∼s , with γs =

∂Ω

∂f ssign(S∼ : N∼

s)

The “microcurl” model 21/54

Page 22: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 23: Micromorphic Crystal Plasticity - sorbonne-universite.fr

From micromorphic to strain gradient plasticity

If the following internal constraint is enforced:

e∼p ≡ 0 ⇐⇒ χ

∼p ≡ P∼

the curl part of the plastic microdeformation is directly related tothe dislocation density densor:

K∼ := Curl χ∼

p ≡ CurlP∼ = Jα∼ · F∼−T

The microcurl theory reduces to strain gradient plasticity accordingto [Gurtin, 2002].

As a result the microcurl model incorporates, as wanted, adependence of material behaviour on the dislocation density tensor.

The “microcurl” model 23/54

Page 24: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 25: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Small deformation microcurl modelWhen deformations and rotations remain sufficiently small, theprevious equations can be linearized as follows:

F∼ = 1∼ + H∼ = 1∼ + H∼e + H∼

p, H∼e = ε∼

e + ωe , H∼p = ε∼

p + ωp

where ε∼e ,ω∼

e (resp. ε∼p,ω∼

p) are practically equal to the symmetricand skew–symmetric parts of E∼ − 1∼ (resp. P∼ − 1∼).When microdeformation is small, the relative deformation islinearized as

e∼p = (1∼ + H∼

p)−1 · (1∼ + χ∼

p)− 1∼ ' χ∼

p −H∼p, with χ

∼p = χ

∼p − 1∼

The “microcurl” model 25/54

Page 26: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Small deformation microcurl modelWhen deformations and rotations remain sufficiently small, theprevious equations can be linearized as follows:

F∼ = 1∼ + H∼ = 1∼ + H∼e + H∼

p, H∼e = ε∼

e + ωe , H∼p = ε∼

p + ωp

where ε∼e ,ω∼

e (resp. ε∼p,ω∼

p) are practically equal to the symmetricand skew–symmetric parts of E∼ − 1∼ (resp. P∼ − 1∼).When microdeformation is small, the relative deformation islinearized as

e∼p = (1∼ + H∼

p)−1 · (1∼ + χ∼

p)− 1∼ ' χ∼

p −H∼p, with χ

∼p = χ

∼p − 1∼

When linearized, the state laws become:

σ∼ = ρ∂ψ

∂ε∼e, s∼ = ρ

∂ψ

∂e∼p, M∼ = ρ

∂ψ

∂K∼The evolution equations read then:

ε∼p =

∂Ω

∂(σ∼ + s∼), α = −∂Ω

∂R

The “microcurl” model 26/54

Page 27: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Small deformation microcurl modelWe adopt the most simple case of a quadratic free energypotential:

ρψ(ε∼e , e∼

p,K∼ ) =1

2ε∼

e : C≈

: ε∼e +

1

2Hχe∼

p : e∼p +

1

2AK∼ : K∼

The usual four–rank tensor of elastic moduli is denoted by C≈. The

higher order moduli have been limited to only two additionalparameters: Hχ (unit MPa) and A (unit MPa.mm2). It followsthat:

σ∼ = C≈

: ε∼e , s∼ = Hχe∼

p, M∼ = AK∼

Large values of Hχ ensure that e∼p remains small so that χ

∼p remains

close to H∼p and K∼ is close to the dislocation density tensor:

curlχ∼

p ≡ curlH∼p = α∼

The “microcurl” model 27/54

Page 28: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Small deformation microcurl modelWe adopt the most simple case of a quadratic free energypotential:

ρψ(ε∼e , e∼

p,K∼ ) =1

2ε∼

e : C≈

: ε∼e +

1

2Hχe∼

p : e∼p +

1

2AK∼ : K∼

The usual four–rank tensor of elastic moduli is denoted by C≈. The

higher order moduli have been limited to only two additionalparameters: Hχ (unit MPa) and A (unit MPa.mm2). It followsthat:

σ∼ = C≈

: ε∼e , s∼ = Hχe∼

p, M∼ = AK∼

The yield condition for each slip system becomes:

f s = |τ s − x s | − τ sc

with

x s = −s∼ : P∼s = (curlM∼ ) : P∼

s = A(curl curlχ∼

p) : N∼s

The “microcurl” model 28/54

Page 29: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 30: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 31: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

γ

h 2h 2

γ

l

1

2

O

n

s

(s) (h+)(h−)

The microstructure is composed of a hard elastic phase (h) and asoft elasto–plastic phase (s) where one slip system with slipdirection normal to the interface between (h) and (s) is considered.A mean simple glide γ is applied in the crystal slip direction of thephase (s). We consider displacement and microdeformation fieldsof the form:

u1 = γx2, u2(x1), u3 = 0, χp12(x1), χp

21(x1)

within the context of small deformation theory.

Size effect in a two–phase single crystal laminate 31/54

Page 32: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

u1 = γx2, u2(x1), u3 = 0, χp12(x1), χp

21(x1)ˆH∼

˜=

24 0 γ 0u2,1 0 00 0 0

35 ˆH∼

p˜=

24 0 γ 00 0 00 0 0

35 ˆH∼

e˜=

24 0 γ − γ 0u2,1 0 00 0 0

35hχ∼

pi

=

24 0 χp12(x1) 0

χp21(x1) 0 00 0 0

35 hcurl χ

pi

=

24 0 0 −χp12,1

0 0 00 0 0

35

Size effect in a two–phase single crystal laminate 32/54

Page 33: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

u1 = γx2, u2(x1), u3 = 0, χp12(x1), χp

21(x1)

ˆH∼

˜=

24 0 γ 0u2,1 0 00 0 0

35 ˆH∼

p˜=

24 0 γ 00 0 00 0 0

35 ˆH∼

e˜=

24 0 γ − γ 0u2,1 0 00 0 0

35hχ∼

pi

=

24 0 χp12(x1) 0

χp21(x1) 0 00 0 0

35 hcurl χ

pi

=

24 0 0 −χp12,1

0 0 00 0 0

35The resulting stress tensors are:

ˆσ∼

˜= µ

24 0 γ − γ + u2,1 0γ − γ + u2,1 0 0

0 0 0

35 ˆs∼˜

= −Hχ

24 0 γ − χp12 0

−χp21 0 0

0 0 0

35ˆM∼

˜=

24 0 0 −Aχp12,1

0 0 00 0 0

35 ˆcurlM∼

˜=

24 0 −Aχp12,11 0

0 0 00 0 0

35These forms of matrices are valid for both phases, except that γ ≡ 0 in the hardelastic phase. Each phase possesses its own material parameters, Hχ and A, theshear modulus, µ, being assumed for simplicity to be identical in both phases.

Size effect in a two–phase single crystal laminate 33/54

Page 34: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

The balance equation, s∼= −curlM∼ , gives χp21 = 0 and the plastic slip:

γ = χp12 −

A

Hχχp

12,11

In the soft phase, the plasticity criterion stipulates that

σ12 + s12 = τc + Hγcum

where H is a linear hardening modulus considered in this phase.We obtain the second order differential equation for the microdeformationvariable in the soft phase, χps

12,

1

ωs2χps

12,11 − χps12 =

τc − σ12

H, with ωs =

sHs

χH

As`Hs

χ + H´

where 1/ωs is the characteristic length of the soft phase for this boundary valueproblem.

Size effect in a two–phase single crystal laminate 34/54

Page 35: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 36: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

The force stress balance equation requires σ12 to be uniform. It follows that thenon–homogeneous part of the differential equation is constant and then thehyperbolic profile of χps

12 takes the form:

χps12 = C s cosh (ωsx) + D

where C s and D are constants to be determined. Symmetry conditions(χps

12(−s/2) = χps12(s/2)) have been taken into account.

In the elastic phase, where the plastic slip vanishes, an hyperbolic profile of themicrodeformation variable, χph

12 , is also obtained:

χph12 = C h cosh

„ωh

„x ± s + h

2

««, with ωh =

sHh

χ

Ah

where, again, C h is a constant to be determined and symmetry conditions havebeen taken into account. It is remarkable that the plastic microvariable, χph

12 ,does not vanish in the elastic phase, close to the interfaces, although no plasticdeformation takes place.

Size effect in a two–phase single crystal laminate 36/54

Page 37: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

The coefficients C s , D and C h can be identified using the interface andperiodicity conditions:

• Continuity of χp12 at x = ±s/2:

C s cosh“ωs s

2

”+ D = C h cosh

„ωh h

2

«(1)

• Continuity of the double traction, m12 = −M13 at x = ±s/2:

AsωsC s sinh“ωs s

2

”= −AhωhC h sinh

„ωh h

2

«(2)

Size effect in a two–phase single crystal laminate 37/54

Page 38: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Simple shear of a two–phase laminate

• Periodicity of displacement component u2. We have the constant stresscomponent

σ12 = µ(γ − γ + u2,1)

whose value is obtained from the plasticity criterion in the soft phase:

σ12 = τc + Hγcum − Asχps12,11

us2,1 =

σ12

µ− γ + γ =

τcµ− γ +

Asωs2C s

Hcosh (ωsx) +

H + µ

µD

in the soft phase and

uh2,1 =

σ12

µ− γ =

τcµ− γ +

H

µD

in the hard phase. The average on the whole structure,Z (s+h)/2

−(s+h)/2

u2,1 dx = 0

must vanish for periodicity reasons and gives„τcµ− γ

«(s + h) +

2AsωsC s

Hsinh

“ωs s

2

”+

H (s + h) + µs

µD = 0 (3)

Size effect in a two–phase single crystal laminate 38/54

Page 39: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plastic microdeformation and plastic slip

µ = 30000 MPa

s = 0.7µm

h = 0.3µm

As = Ah = 100 MPa.µm2

Hsχ = Hh

χ = 100000 MPa

τc = 20 MPa

lc =q

Aµ' 60 nm

0

0.002

0.004

0.006

0.008

0.01

0.012

0.014

0.016

0.018

-0.4 -0.2 0 0.2 0.4

x

γ(x)

Size effect in a two–phase single crystal laminate 39/54

Page 40: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plastic microdeformation and plastic slip

µ = 30000 MPa

s = 0.7µm

h = 0.3µm

As = Ah = 100 MPa.µm2

Hsχ = Hh

χ = 100000 MPa

τc = 20 MPa

lc =q

Aµ' 60 nm

0

0.002

0.004

0.006

0.008

0.01

0.012

0.014

0.016

0.018

-0.4 -0.2 0 0.2 0.4

x

γ(x)

γ(x) FE

Size effect in a two–phase single crystal laminate 39/54

Page 41: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plastic microdeformation and plastic slip

µ = 30000 MPa

s = 0.7µm

h = 0.3µm

As = Ah = 100 MPa.µm2

Hsχ = Hh

χ = 100000 MPa

τc = 20 MPa

lc =q

Aµ' 60 nm

0

0.002

0.004

0.006

0.008

0.01

0.012

0.014

0.016

0.018

-0.4 -0.2 0 0.2 0.4

x

χp12(x)γ(x)

Size effect in a two–phase single crystal laminate 39/54

Page 42: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plastic microdeformation and plastic slip

µ = 30000 MPa

s = 0.7µm

h = 0.3µm

As = Ah = 100 MPa.µm2

Hsχ = Hh

χ = 100000 MPa

τc = 20 MPa

lc =q

Aµ' 60 nm

0

0.002

0.004

0.006

0.008

0.01

0.012

0.014

0.016

0.018

-0.4 -0.2 0 0.2 0.4

x

χp12(x)γ(x)

χp12(x) FEγ(x) FE

Size effect in a two–phase single crystal laminate 39/54

Page 43: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Overall cyclic response

-50

-40

-30

-20

-10

0

10

20

30

40

50

-0.01 -0.005 0 0.005 0.01

<σ 1

2>

<2ε12>

MicrocurlClassic

Size effect in a two–phase single crystal laminate 40/54

Page 44: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Size effects

1e+02

1e+03

1e+04

1e+05

1e-06 1e-05 1e-04 1e-03 1e-02 1e-01 1e+00

Σ 12|

0.2

(MP

a)

l (mm)

curl H p (Hχ→ ∞)

microcurl (Hχ=109 MPa)

microcurl (Hχ=108 MPa)

microcurl (Hχ=107 MPa)

microcurl (Hχ=106 MPa)

Size effect in a two–phase single crystal laminate 41/54

Page 45: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Size effects

Flo

w s

tres

s, Σ

Microstructural length scale, l

∆Σ

Effect of H

cl

Effect of H

Scaling law l

n

n

Effect of A

χ

χ

Hχ and A can be calibrated to account for a scaling law 1/ln,0 < n < 2[Cordero et al., 2010]

Size effect in a two–phase single crystal laminate 42/54

Page 46: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 47: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Strain gradient plasticity as a limit case

• Size effect according to SGP

limHχ→∞

Σ12 = τc +12As〈γ〉

f 3s l2

physical meaning of a 1/l2 scaling law?

Size effect in a two–phase single crystal laminate 44/54

Page 48: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 49: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Boundary value problem for micromorphic crystals

• Shear test

• Periodic grains with randomorientations

• Periodic mesh

• Periodic boundaryconditions:u (x) = E∼.x + v (x), vperiodicχ∼

p(x) periodic

• 2 slip systems / grain

• The grain size d is rangingfrom tens of nanometers tohundreds of microns.

l2

d

2nn1

l1

E = 70000 MPaν = 0.3

A = 0.01MPa.mm2

Hχ = 106 MPa

Intrinsic length scale:

lc =√

AHχ

= 0.1µm

Grain size effect in polycrystalline aggregates 46/54

Page 50: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Boundary value problem for micromorphic crystals

d

d

φθφ

xy

Y

Xl

ln

n1

12

2

Grain size effect in polycrystalline aggregates 47/54

Page 51: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Boundary value problem for micromorphic crystals

-150

-100

-50

0

50

100

150

-0.01 -0.005 0 0.005 0.01

Σ 12 [

MP

a]

E12

Grain size effect in polycrystalline aggregates 48/54

Page 52: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 53: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Grain size effect

-20

0

20

40

60

80

100

120

140

160

0 0.01 0.02 0.03 0.04 0.05

Σ 12 [

MP

a]

E12

d = 0.4µm

2.0µm

4.0µm

10.0µm

200.0µm

Grain size effect in polycrystalline aggregates 50/54

Page 54: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Grain size effect

10

100

1000

1e-03 1e-02 1e-01 1e+00 1e+01 1e+02 1e+03

Σ 12|1

% [

MP

a]

d [µm]

m = -0.78 (set (e))

m = -0.67 (f)

m = -0.50 (g)

m

Grain size effect in polycrystalline aggregates 51/54

Page 55: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plan

1 The “microcurl” modelKinematics and balance equationsConstitutive equationsInternal stress arising from the modelInternal constraint and strain gradient plasticityLinearized formulation

2 Size effect in a two–phase single crystal laminateBoundary value problemInterface conditionsStrain gradient plasticity as a limit case

3 Grain size effect in polycrystalline aggregatesHall–Petch effectStrain localization in ultra–fine grains

Page 56: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Plastic strain fieldd = 200µm d = 20µm d = 10µm

d = 4µm d = 2µm d = 1µm

0 0.004 0.008 0.012 0.015 0.019 0.023 0.027 0.031 0.035 0.039

Grain size effect in polycrystalline aggregates 53/54

Page 57: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Dislocation density tensor fieldd = 200µm d = 20µm d = 10µm

d = 4µm d = 2µm d = 1µm

0 0.5 1.0 1.5 1.9 2.4 2.9 3.4 3.9 4.4 4.9

[mm ]-1

Grain size effect in polycrystalline aggregates 54/54

Page 58: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Cordero N.M., Gaubert A., Forest S., Busso E., Gallerneau F.,and Kruch S. (2010).Size effects in generalised continuum crystal plasticity fortwo–phase laminates.Journal of the Mechanics and Physics of Solids, vol. 58, pp1963–1994.

Forest S. (2009).The micromorphic approach for gradient elasticity,viscoplasticity and damage.ASCE Journal of Engineering Mechanics, vol. 135, pp 117–131.

Forest S. and Sievert R. (2003).Elastoviscoplastic constitutive frameworks for generalizedcontinua.Acta Mechanica, vol. 160, pp 71–111.

Forest S. and Sievert R. (2006).Nonlinear microstrain theories.

Grain size effect in polycrystalline aggregates 54/54

Page 59: Micromorphic Crystal Plasticity - sorbonne-universite.fr

International Journal of Solids and Structures, vol. 43, pp7224–7245.

Germain P. (1973).The method of virtual power in continuum mechanics. Part 2 :Microstructure.SIAM J. Appl. Math., vol. 25, pp 556–575.

Gurtin M.E. (2002).A gradient theory of single–crystal viscoplasticity thataccounts for geometrically necessary dislocations.Journal of the Mechanics and Physics of Solids, vol. 50, pp5–32.

Gurtin M.E. and Anand L. (2009).Thermodynamics applied to gradient theories involving theaccumulated plastic strain: The theories of Aifantis and Fleck& Hutchinson and their generalization.Journal of the Mechanics and Physics of Solids, vol. 57, pp405–421.

Grain size effect in polycrystalline aggregates 54/54

Page 60: Micromorphic Crystal Plasticity - sorbonne-universite.fr

Sedlacek R. and Forest S. (2000).Non-local plasticity at microscale : A dislocation-based modeland a Cosserat model.physica status solidi (b), vol. 221, pp 583–596.

Steinmann P. (1996).Views on multiplicative elastoplasticity and the continuumtheory of dislocations.International Journal of Engineering Science, vol. 34, pp1717–1735.

Grain size effect in polycrystalline aggregates 54/54