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On stress-gradient materials: formulation and homogenization

Sébastien Brisard, Vinh Phuc Tran, Karam Sab, Johann Guilleminot

To cite this version:

Sébastien Brisard, Vinh Phuc Tran, Karam Sab, Johann Guilleminot. On stress-gradient materials:

formulation and homogenization. Encounter of the third kind on generalized continua and microstruc- tures, Apr 2018, Arpino, Italy. �hal-01758985�

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S. Brisard1, V.P. Tran1,2, K. Sab1, J. Guilleminot3

On stress-gradient materials:

formulation and homogenization

4 April 2018

Encounter of the Third Kind — Generalized continua and microstructures

1Université Paris-Est, Laboratoire Navier, UMR 8205, CNRS, ENPC, IFSTTAR, F-77455 Marne-la-Vallée, France

2Université Paris-Est, Laboratoire Modélisation et Simulation Multi Échelle (MSME), UMR 8208, CNRS, F-77454 Marne-la-Vallée, France

3Department of Civil and Environmental Engineering, Duke University, Durham, NC 27708, USA

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Stress-gradient elasticity in a nutshell

The Stress Principle of Cauchy

σ⋅∇+b=0 and σ⟧⋅n=0 (SA) Cauchy elasticity

Wc[σ]= wc(σ)d V W c[σ]= wc(σ , σ⊗∇)d V

Stress-gradient elasticity

Forest and Sab (2012), Mechanics Research Communications 40 (first derivation) Sab, Legoll and Forest (2016), Journal of Elasticity 123(2) (mathematical justification) Forest and Sab (2017), Mathematics and Mechanics of Solids (extension to finite strain)

Polizzotto (2014, 2016), International Journal of Solids and Structures

Alternative model (not discussed here) A mature model

(4)

In the present talk

A brief overview of the stress-gradient model

Decomposition of the stress-gradient

Stress boundary conditions

Homogenization of stress-gradient materials

Hill–Mandel lemma, boundary conditions

Softening size effect

Application to composites with spherical inclusions

Eshelby’s inhomogeneity problem

Mori–Tanaka estimates of effective compliance Some open questions

Tran, Brisard, Guilleminot and Sab (2018), International Journal of Solids and Structures

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Derivation of the stress-gradient model for elasticity

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Roadmap

Minimize complementary stress energy under SA constraint

Cauchy elasticity: elastic equilibrium of fixed solid is retrieved

Stress-gradient elasticity: elastic equilibrium of fixed solid is defined

At this point, “fixed” not really meaningful, since dofs not (yet) defined

“Trace” of the stress-gradient is prescribed

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Decomposition of stress-gradient (1/2)

Wc[σ]= wc(σ , σ⊗∇)d V

Classical equilibrium equation (σ⊗∇):I2=σ⋅∇=−b

Orthogonal decomposition of stress gradient σ⊗∇=Q+R with R :I2=0 and QR=0 R=I'6(σ⊗∇)

Complementary stress energy of stress-gradient materials

Wc[σ]= wc(σ , Q,R)dV

Equivalent expression of complementary stress energy

(projection onto space of trace-free, third-rank tensors)

(8)

Decomposition of stress-gradient (2/2)

Modeling assumption Q=−12 I4b

Wc[σ]= wc(σ , Q,R)dV = wc(σ ,R)d V

No strain measure attached to Q (generalized prestress) Orthogonal decomposition of stress gradient

σ⊗∇=Q+R with R :I2=0 and QR=0 Q is in fact fully prescribed

(straightforward linear algebra)

with R=I' (σ⊗∇)

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Constrained minimization of energy

Initial problem

Stress-gradient as independent variable

Minimize: Wc[σ]= wc(σ ,I'6(σ⊗∇))d V

subject to: σ⋅∇+b=0

Minimize: Wc[σ ,R]= wc(σ ,R)d V

subject to: {R=σI⋅∇ +'6(bσ=⊗∇)0 uΦ

Lagrange multipliers

(10)

Elastic equilibrium of fixed, SG bodies

Field equations

R=I'6(σ⊗∇) Φ=∂R wc

e=∂σ wc σ⋅∇+b=0

e=Φ⋅∇ +ε[u]

Generalized stress-strain relations Generalized strain-displacement relations Generalized equilibrium equations

Boundary conditions

Φn+sym(un)=0 6 scalar boundary conditions

Continuity conditions

Φn+sym(un)⟧=0

σ⟧=0

Weaker continuity of “displacements”

Stronger continuity of “stresses”

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Linear elasticity

Complementary stress energy density wc(σ ,R)=12 σ :S:σ+12 R MR

No σ–R coupling for centrosymmetric materials!

Stress-strain relationships e=Sσ and Φ=MR

S and M have major and minor symmetries

Generalized compliance M operates on trace-free tensors M=I'6MI'6

or

σ=C e and R=LΦ

C=S1 and L=M+

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Isotropic linear elasticity

General isotropic linear stress-gradient elasticity

I'6=J6+K6

Simplified model for isotropic linear stress-gradient elasticity 2 μ S=12 ν

1+ν J4+K4 2 μ

2 M=12 ν

1+ν J6+K6

0 J6 0

J6

H6 K6

K6 0

H6 H6

H6 0

H6 K6

J6 2 μM=2J J6+2K K6+2H H6

M=I'6MI'6

Altan and Aifantis (1992), Scripta Metallurgica et Materialia 26(2)

Altan and Aifantis (1997), Journal of the Mechanical behavior of Materials 8(3)

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Homogenization

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Setting the stage for homogenization

The 3 cases

Stress-gradient (micro)→stress-gradient (macro)

Cauchy (micro)→stress-gradient (macro)

Stress-gradient (micro)→Cauchy (macro) Separation of scales

Classical condition

dLmesoLmacro

Microstructure RVE Structure

Additional condition for stress-/strain- gradient materials d or d

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Effective and apparent properties

Effective behaviour: stress-gradient →Cauchy (d)

e⟩=Seff:σ

σ⟩= 1 V

Ω

σ d V

e⟩= 1 V

Ω

e d V = 1 V

Ω

ε[u]dV + 1 V

Ω

Φn d S

σ⋅∇=0

e=Sσ Φ=M(σ⊗∇) e=Φ⋅∇ +ε[u]

+ boundary conditions!

e⟩=Sapp(Ω):σ

Local problem on SVE Ω

Apparent elastic properties of (large) SVE Ω

No body forces!

(16)

Boundary conditions

Generalized Hill–Mandel lemma

σ*:e+(σ*⊗∇)Φ⟩=⟨σ*:e

Uniform stress boundary conditions

σ|Ω=σ e⟩=Sσ (Ω):σ⟩=Sσ (Ω):σ

Uniform strain boundary conditions

Φn+sym(un)=sym[(ex)⊗n] σ⟩=Cε(Ω):e⟩=Cε(Ω):e Uniform traction boundary conditions

σ|Ωn=σn e⟩=ST(Ω):σ⟩=ST (Ω):σ a⋅[Φn+sym(un)]⋅a=0 a=I nn

(17)

Variational formulation

Minimum of complementary stress energy

σ :Sσ (Ω):σ=inf {⟨σ:S:σ+(σ⊗∇)M(σ⊗∇ )⟩}

subject to: σ⋅∇=0 and σ|Ω=σ Minimum of strain energy

e:Cε(Ω):e=inf {⟨ε[u]:C :ε[u]+ΦLΦ⟩}

subject to: Φn+sym(un)=sym[(ex)⊗n] Bounds for finite-size SVEs

Cσ (ΩI)≤Cσ(ΩII)≤CeffCε(ΩII)≤Cε(ΩI) for ΩIΩII

Huet (1990), Journal of the Mechanics and Physics of Solids 38(6)

(18)

Softening size-effect

Variational definition of apparent compliance (uniform σ BC)

Fixed microstructure, variable material internal length

Scaled microstructure, constant material internal length If SISII and MIMII everywhere in Ω , then SIeffSIIeff

For SI=SII and MI= I2

II2 MII: if III then SIeffSIIeff More generally: if ( d )I( d )II then SIeffSIIeff

If d d then CeffCeff Softening size-effect!

(19)

Eshelby’s inhomogeneity problem for stress-gradient elasticity

(20)

Problem setting

σ ez

σ ez

Matrix: μm , νm , ℓm μi, νi , ℓi

νi=νm=0.25 μi=10 μm

(21)

Some tedious calcs later…

Hat tip to VP Tran!

http://www.sympy.org

Axial stress along vertical axis Axial stress at origin

Theorem of Eshelby (1957) does not hold!

Eshelby (1957). Proc. Royal Soc. A 241(1226)

(22)

Dilute stress concentration tensor

σi= 1

V σ d V =B:σ

Axial stress along vertical axis Axial stress at origin

(23)

Mori–Tanaka estimates for composites with spherical inclusions

(24)

Problem setting

μm, νm=0.25, m

μi=10 μm , νi=0.25 , ℓi

Volume fraction of inclusions: f

(25)

Estimates of bulk and shear moduli

Strain- and stress- gradient models are not equivalent!

Effective bulk modulus Effective shear modulus

Seff=Sm+f (SiSm):B:[(1f )I4+f B]1

Benveniste (1987), Mechanics of Materials 6(2) Ma and Gao (2014), Acta Mechanica 225(4-5)

(26)

Some questions

(27)

The total complementary energy

Ω

u b T

Ωu ΩT Assumption 1: Stress Principle of Cauchy

σ⋅∇=0 and σn|Ω=T

Assumption 2: complementary work of prescribed displacements

Vc=

Ωu

uσnd S

Minimization of complementary energy Minimize: Πc=WcV c

subject to: σ⋅∇=0 and σn| =T

(28)

The general BVP

Field equations

R=I'6(σ⊗∇) Φ=∂R wc

e=∂σ wc σ⋅∇+b=0

e=Φ⋅∇ +ε[u]

Boundary conditions

ΩT :

{

a⋅[Φn+σsymn|Ω(u=Tn)]⋅a=0

Continuity conditions

Φn+sym(un)⟧=0

σ⟧=0

Ωu: Φn+sym(un)=sym(un)

a=I2nn

(29)

The total potential energy

Potential strain energy

Work of prescribed body forces and tractions V =

Ω

bu d V +

ΩT

T⋅[u+2Φ :nn−(Φ nnn)n]d S

Minimization of total potential energy Minimize: Π=W V

W= w(e ,Φ)d V

subject to:

{

ΩuΩ:T :Φan⋅[+Φsymn+(symun()=usymn)]⋅a(u=0n)

u+2Φ:nn−(Φ nnn)n=u

(30)

Conclusion & perspectives

Summary

Simplified model for isotropic linear elasticity

General framework for stress-gradient→Cauchy homogenization

Softening size-effect

Mori–Tanaka estimates for spherical inclusions Outlook

Hashin–Shtrikman (size-dependent) bounds on effective properties

Cauchy→stress-gradient homogenization

Understand the meaning of u (use above)

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Thanks for your attention!

[email protected] http://navier.enpc.fr/BRISARD-Sebastien http://sbrisard.github.io

This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ or send a letter to Creative

This work has benefited from a French government grant managed by ANR within the frame of the national program Investments for the Future ANR-11-LABX-022-01.

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