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Lectures Mathematical foundations of elasticity theory

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Lectures Mathematical foundations of elasticity theory has contents: Boundary conditions, properties of W, square root theorem, formula for the square root, material symmetry, the ballistic free energy,...and other contents.

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Mathematical Foundations of

Elasticity Theory

John Ball Oxford Centre for Nonlinear PDE

©J.M.Ball

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Reading

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Prentice Hall 1983

Lecture note 2/1998 Variational models for microstructure and phase transitions

Stefan Müller

http://www.mis.mpg.de /

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J.M Ball, Some open problems in

elasticity In Geometry, Mechanics, and Dynamics, pages 3 59,

Springer, New York, 2002.

You can download this from my webpage

http://www.maths.ox.ac.uk/~ball

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Elasticity Theory

The central model of solid mechanics Rubber, metals (and

alloys), rock, wood, bone … can all be modelled as elastic

materials, even though their chemical compositions are very

different.

For example, metals and alloys are crystalline, with grains

consisting of regular arrays of atoms Polymers (such as rubber) consist of long chain molecules that are wriggling in thermal

motion, often joined to each other by chemical bonds called

crosslinks Wood and bone have a cellular structure …

6

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A brief history

1678 Hooke's Law

1705 Jacob Bernoulli

1742 Daniel Bernoulli

1744 L Euler elastica (elastic rod)

1821 Navier, special case of linear elasticity via molecular model

(Dalton’s atomic theory was 1807)

1822 Cauchy, stress, nonlinear and linear elasticity

For a long time the nonlinear theory was ignored/forgotten.

1927 A.E.H Love, Treatise on linear elasticity

1950's R Rivlin, Exact solutions in incompressible nonlinear elasticity

(rubber)

1960 80 Nonlinear theory clarified by J.L Ericksen, C Truesdell …

1980 Mathematical developments, applications to materials,

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Label the material points of the body by the positions x ∈ Ω they occupy in the reference

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Deformation gradient

F = Dy(x, t), Fiα = ∂x∂yi

α.

9

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To avoid interpenetration of matter, we quire that for each t, y( ·, t) is invertible on Ω, with sufficiently smooth inverse x( ·, t) We also suppose that y( ·, t) is orientation preserving; hence

re-J = det F (x, t) > 0 for x ∈ Ω (1)

By the inverse function theorem, if y( ·, t) is C1, (1) implies that y( ·, t) is locally invertible.

10

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Global inverse function theorem for

C1 deformations

Let Ω ⊂ R n be a bounded domain with chitz boundary ∂Ω (in particular Ω lies on one side of ∂Ω locally) Let y ∈ C1( ¯ Ω; R n ) with

Lips-det Dy(x) > 0 for all x ∈ ¯ Ω

and y |∂Ω one-to-one Then y is invertible on

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Variational formulation of nonlinear

elastostatics

We suppose for simplicity that the body is mogeneous, i.e the material response is the same at each point In this case the total elas- tic energy corresponding to the deformation

ho-y = ho-y(x) is given bho-y

I(y) =

Ω W (Dy(x)) dx,

where W = W (F ) is the stored-energy function

of the material We suppose that W : M+3×3 →

R is C1 and bounded below, so that without loss of generality W ≥ 0.

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We will study the existence/nonexistence of minimizers of I subject to suitable boundary conditions.

Issues.

1 What function space should we seek a

minimizer in? This controls the allowable

sin-gularities in deformations and is part of the mathematical model

2 What boundary conditions should be

specified?

3 What properties should we assume

about W ?

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The Sobolev space W1,p

W 1,p = {y : Ω → R 3 : y 1,p < ∞}, where

y 1,p = ( Ω[|y(x)|p + |Dy(x)|p] dx)1/p if 1 ≤ p < ∞

ess supx∈Ω (|y(x)| + |Dy(x)|) if p = ∞

Dy is interpreted in the weak (or distributional)sense, so that

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We assume that y belongs to the largest Sobolev space W 1,1 = W 1,1(Ω; R3 ), so that in particu- lar Dy(x) is well defined for a.e x ∈ Ω, and

I(y) ∈ [0, ∞].

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y ∈ W 1,∞

y ∈ W 1,1

(because every y ∈ W 1,1 is absolutely uous on almost every line parallel to a given direction)

contin-Lipschitz

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y(x) = 1+ |x| |x| x

y ∈ W 1,p for 1 ≤ p < 3.

Exercise: prove this.

Cavitation

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Boundary conditions

We suppose that ∂Ω = ∂Ω1 ∪ ∂Ω 2 ∪ N, where

∂Ω1, ∂Ω2 are disjoint relatively open subsets

of ∂Ω and N has two-dimensional Hausdorff measure H2(N ) = 0 (i.e N has zero area).

We suppose that y satisfies mixed boundary conditions of the form

y |∂Ω1 = ¯ y( ·), where ¯ y : ∂Ω1 → R3 is a given boundary dis- placement.

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By formally computing

d

dτ I(y+τ ϕ)| τ =0 = d

dτ Ω W (Dy+τ Dϕ) dx | t=0 = 0,

we obtain the weak form of the Euler-Lagrange

equation for I, that is

Ω DF W (Dy) · Dϕ dx = 0 (∗) for all smooth ϕ with ϕ |∂Ω1 = 0.

TR(F ) = DF W (F ) is the

Piola-Kirchhoff stress tensor

(A · B = tr AT B)

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If y, ∂Ω1 and ∂Ω2 are sufficiently regular then (*) is equivalent to the pointwise form of the equilibrium equations

Div DF W (Dy) = 0 in Ω, together with the natural boundary condition

of zero applied traction

DF W (Dy)N = 0 on ∂Ω2, where N = N (x) denotes the unit outward nor- mal to ∂Ω at x.

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Hence our variational problem becomes:

Does there exist y∗ minimizing

I(y) =

Ω W (Dy) dxin

A = {y ∈ W 1,1 : y invertible, y|∂Ω1 = ¯y}?

We will make the invertibility condition moreprecise later

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Thus if I(y) < ∞ then det Dy(x) > 0 a.e However this does not imply local invertibil-ity (think of the map (r, θ) → (r, 2θ) in planepolar coordinates, which has constant positiveJacobian but is not invertible near the origin),nor is it clear that det Dy(x) ≥ µ > 0 a.e

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We suppose that W is frame-indifferent, i.e.

(H2) W (RF ) = W (F )

for all R ∈ SO(3), F ∈ M3×3.

In order to analyze (H2) we need some linear algebra.

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Square root theorem

Let C be a positive symmetric n × n matrix Then there is a unique positive definite sym- metric n × n matrix U such that

C = U2(we write U = C1/2).

28

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Formula for the square root

Since C is symmetric it has a spectral position

decom-C =

n i=1

λiˆei ⊗ ˆei.Since C > 0, it follows that λi > 0 Then

U =

n i=1

λ1/2i ˆei ⊗ ˆei

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Polar decomposition theorem

Let F ∈ M+n×n Then there exist positive nite symmetric U , V and R ∈ SO(n) such that

defi-F = RU = V R

These representations (right and left tively) are unique

respec-30

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Proof. Suppose F = RU Then U2 = F T F :=

C Thus if the right representation exists U must be the square root of C But if a ∈

R n is nonzero, Ca · a = |F a|2 > 0, since F is nonsingular Hence C > 0 So by the square root theorem, U = C1/2 exists and is unique.

Let R = F U−1 Then

RT R = U−1FT F U−1 = 1 and det R = det F (det U )−1 = +1.

The representation F = V R1 is obtained larly using B := F F T , and it remains to prove

simi-R = simi-R1 But this follows from F = R1 RT1 V R1 , and the uniqueness of the right representation.

31

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Exercise: simple shear

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Hence (H2) implies that

W (F ) = W (RU ) = W (U ) = ˜ W (C).

Conversely if W (F ) = ¯ W (U ) or W (F ) = ˜ W (C) then (H2) holds.

Thus frame-indifference reduces the dependence

of W on the 9 elements of F to the 6 elements

of U or C.

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Material Symmetry

In addition, if the material has a nontrivialisotropy group S, W satisfies the material sym-metry condition

W (F Q) = W (F ) for all Q ∈ S, F ∈ M+3×3

The case S = SO(3) corresponds to an isotropic

material

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The strictly positive eigenvalues v1, v2, v3 of U

(or V ) are called the principal stretches.

Proposition 1

W is isotropic iff W (F ) = Φ(v1, v2, v3), where

Φ is symmetric with respect to permutations

of the vi.

Proof Suppose W is isotropic Then F =

RDQ for R, Q ∈ SO(3) and D = diag (v 1 , v2, v3).

Hence W = W (D) But for any permutation

P of 1, 2, 3 there exists ˜ Q such that

˜

Qdiag (v1, v2, v3) ˜ QT = diag (vP 1, vP 2, vP 3).

The converse holds since QT F T F Q has the

same eigenvalues (namely vi2) as F T F

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(H1) and (H2) are not sufficient to prove the existence of energy minimizers We also need growth and convexity conditions on W The growth condition will say something about how fast W grow for large values of F The convex- ity condition corresponds to a statement of the type ‘stress increases with strain’ We return

to the question of what the correct form of this convexity condition is later; for a summary of older thinking on this question see Truesdell & Noll.

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Why minimize energy?

This is the deep problem of the approach to

equilibrium , having its origins in the Second

Law of Thermodynamics

We will see how rather generally the balance

of energy plus a statement of the Second Lawlead to the existence of a Lyapunov functionfor the governing equations

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∂E tR · y t dS +

E r dx −

∂E qR · N dS, (1) for all E ⊂ Ω, where ρ R = ρR(x) is the density

in the reference configuration, U is the internal

energy density, b is the body force, tR is the

Piola-Kirchhoff stress vector, qR the reference

heat flux vector and r the heat supply.

Balance of Energy

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We assume this holds in the form of the Clausius

Second Law of Thermodynamics

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The Ballistic Free Energy

Suppose that the the mechanical boundary ditions are that y = y(x, t) satisfies

con-y(·, t)|∂Ω1 = ¯y(·) and the condition that theapplied traction on ∂Ω2 is zero, and that thethermal boundary condition is

θ(·, t)|∂Ω3 = θ0, qR · N|∂Ω\∂Ω3 = 0,where θ0 > 0 is a constant Assume that the

heat supply r is zero, and that the body force

is given by b = −gradyh(x, y),

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Thus from (1), (2) with E = Ω and the ary conditions

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Lya-For thermoelasticity, W (F, θ) can be fied with the Helmholtz free energy U (F, θ) −θη(F, θ) Hence, if the dynamics and bound-ary conditions are such that as t → ∞ we have

identi-yt → 0 and θ → θ0, then this is close to sayingthat y tends to a local minimizer of

Iθ0(y) =

Ω[W (Dy, θ0) + h(x, y)] dx

The calculation given follows work of Duhem,Ericksen and Coleman & Dill

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Of course a lot of work would be needed tojustify this (we would need well-posedness ofsuitable dynamic equations plus information onasymptotic compactness of solutions and more;this is currently out of reach) Note that it isnot the Helmoltz free energy that appears inthe expression for E but U − θ0η, where θ0 isthe boundary temperature.

For some remarks on the case when θ0 depends

on x see J.M Ball and G Knowles,

Lyapunov functions for thermoelasticity with

spatially varying boundary temperatures Arch.

Rat Mech Anal., 92:193—204, 1986.

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Existence in one dimension

To make the problem nontrivial we consider

an inhomogeneous one-dimensional elastic terial with reference configuration Ω = (0, 1) and stored-energy function W (x, p), with cor- responding total elastic energy

ma-I(y) = 1

0 [W (x, yx(x)) + h(x, y(x))] dx, where h is the potential energy of the body force.

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We seek to minimize I in the set of admissibledeformations

A = {y ∈ W 1,1(0, 1) : yx(x) > 0 a.e.,

y(0) = α, y(1) = β},where α < β (We could also consider mixedboundary conditions y(0) = α, y(1) free.)

(Note the simple form taken by the invertibilitycondition.)

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(H4) W (x, p) is convex in p, i.e.

W (x, λp + (1 − λ)q) ≤ λW (x, p) + (1 − λ)W (x, q)for all p > 0, q > 0, λ ∈ (0, 1), x ∈ (0, 1)

If W is C1 in p then (H4) is equivalent to the stress Wp(x, p) being nondecreasing in the strain p.

(H5) h : [0, 1] × R → [0, ∞) is continuous.

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i.e y(j) ∈ A, I(y(j)) → l as j → ∞.

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We may assume that

lim j →∞ 0 1 W (x, y x (j) ) dx = l 1 ,

lim j →∞ 0 1 h(x, y (j) ) dx = l 2 ,

where l = l 1 + l 2

Since Ω Ψ(yx(j)) dx ≤ M < ∞, by the de la

Vall´ee Poussin criterion (see e.g One-dimensional

variational problems, G Buttazzo, M Giaquinta,

S Hildebrandt, OUP, 1998 p 77) there exists

a subsequence, which we continue to call yx(j)

converging weakly in L1(0, 1) to some z.

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Let y∗(x) = α+ 0x z(s) ds, so that yx∗ = z Then

y(j)(x) = α + 0x yx(j)(s) ds → y∗(x)

for all x ∈ [0, 1] In particular y∗(0) = α,

y∗(1) = β

By Mazur’s theorem, there exists a sequence

z(k) = ∞j=k λ(k)j yx(j) of finite convex nations of the yx(j) converging strongly to z,

combi-and so without loss of generality almost where

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Also by Fatou’s lemma

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So limp→∞ W (p)p = ∞ says that you can’t get

a finite line segment from an infinitesimal one with finite energy.

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x = 0

x = 1

y(0) = 0

y(1) = α

Assume constant density

ρR and pressure pR in the reference configuration.

Assume gas deforms adiabatically so that the pressure p and density ρ satisfy pρ−γ = pRρ−γR , where γ > 1 is a constant.

Simplified model of atmosphere

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The potential energy of the column is

0

pR(γ − 1)yx(x)γ−1 + ρRgy(x) dx

= ρRg 1

0

k

yx(x)γ−1 + (1 − x)yx(x) dx,where k = ρ pR

R g(γ −1).

We seek to minimize I in

A = {y ∈ W 1,1(0, 1) : yx > 0 a.e.,

y(0) = 0, y(1) = α }.

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Then the minimum of I(y) on A is attained iff

α ≤ αcrit, where αcrit = γ γ

αcrit can be interpreted

as the finite height of

the atmosphere predicted

by this simplified model

(cf Sommerfeld).

If α > αcrit then minimizing sequences y(j) for

I converge to the minimizer for α = αcrit plus

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For details of the calculation see J.M Ball,

Loss of the constraint in convex variational

problems, in Analyse Math´ ematiques et

Appli-cations, Gauthier-Villars, Paris, 1988, where a

general framework is presented for minimizing

a convex functional subject to a convex

con-straint, and is applied to other problems such

as Thomas-Fermi and coagulation-fragmentation equations.

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Proof Define p(j) as shown.

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If W (x, ·) is not convex then the minimum is

in general not attained For example consider

the problem

inf

y(0)=0,y(1)=32

1 0

(yx − 1)2(yx − 2)2

2 x)2 dx.

Then the infimum is zero

but is not attained

1 3/2

slopes 1 and 2

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More generally we have the following result.

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Let l = infy∈A 01 W (yx) dx,

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j+1 k j k

j−1 1

0 W (zx) dx + Cj−2

≤ l + 2ε for j sufficiently large Hence m ≤ l and so

l = m.

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But by assumption there exists y∗ with

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There are two curious special cases when the minimum is nevertheless attained when W is not convex Suppose that (H1), (H3) hold and that either

(i) I(y) = 01 W (x, yx) dx, or

(ii) I(y) = 01[W (yx) + h(y)] dx.

Then I attains a minimum on A.

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(i) can be found in Aubert & Tahraoui (J ferential Eqns 1979) and uses the fact that

Dif-infy∈A 01 W (x, yx) dx = infy∈A 01 W ∗∗(x, yx) dx, where W ∗∗ is the lower convex envelope of W

W (x, p)

p

W ∗∗(x, p)

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The Euler-Lagrange equation in 1D

Let y minimize I in A and let ϕ ∈ C0∞(0, 1)

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However, there is a serious problem in makingthis calculation rigorous, since we need to pass

to the limit τ → 0+ in the integral

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But Wp can be much bigger than W For

example, when p is small and W (p) = 1p then

|W p (p) | = p12 is much bigger than W (p) Or if

p is large and W (p) = exp p2 then

|W p (p) | = 2p exp p2 is much bigger than W (p).

It turns out that this is a real problem and not just a technicality Even for smooth ellip- tic integrands satisfying a superlinear growth

condition there is no general theorem of the

one-dimensional calculus of variations saying that a minimizer satisfies the Euler-Lagrange equation.

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Consider a general one-dimensional integral ofthe calculus of variations

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It follows that u is a smooth solution of the

Euler-Lagrange equation dxd fp = fu on (0, 1).

Suppose u ∈ W 1,1(0, 1) satisfies the weak form

of the Euler-Lagrange equation

bounded on compact subsets of (0, 1).

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Also if u(j) ∈ W 1,∞ converges a.e to u∗ then

I(u(j)) → ∞ (the repulsion property), explaining the numer- ical results.

For this problem one has that

I(u∗ + tϕ) = ∞ for t = 0, if ϕ(0) = 0

u∗

u∗ + tϕ

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Derivation of the EL equation for 1D

elasticity

Theorem 3

Let (H1) and (H5) hold and suppose further

that Wp exists and is continuous in (x, p) ∈

[0, 1] × (0, ∞), and that h y exists and is

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Pick any representative of yx and let

Ωj = {x ∈ [0, 1] : 1j ≤ yx(x) ≤ j} Then Ωj ismeasurable, Ωj ⊂ Ωj+1 and

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