Generalized Hooke's
CH.6. LINEAR ELASTICITY
Multimedia Course on Continuum Mechanics Overview
Hypothesis of the Linear Elasticity Theory Lecture 1 Linear Elastic Constitutive Equation Lecture 2 Generalized Hooke’s Law Elastic Potential Lecture 3 Isotropic Linear Elasticity Isotropic Constitutive Elastic Constants Tensor Lecture 4 Lamé Parameters Isotropic Linear Elastic Constitutive Equation Young’s Modulus and Poisson’s Ratio Lecture 5 Inverse Isotropic Linear Elastic Constitutive Equation Spherical and Deviator Parts of Hooke’s Law Lecture 6 Limits in Elastic Properties Lecture 7
2 Overview (cont’d)
The Linear Elastic Problem Governing Equations Lecture 8 Boundary Conditions The Quasi-Static Problem Lecture 9 Solution Lecture 10 Displacement Formulation Stress Formulation Lecture 11 Saint-Venant’s Principle Lecture 12 Uniqueness of the solution Linear Thermoelasticity Hypothesis of the Linear Elasticity Theory Lecture 13 Linear Thermoelastic Constitutive Equation Inverse Constitutive Equation Lecture 14 Thermal Stress and Strain
3 Overview (cont’d)
Thermal Analogies Solution to the linear thermoelastic problem Lecture 15 1st Thermal Analogy 2nd Thermal Analogy Lecture 16 Lecture 17
Superposition Principle in Linear Thermoelasticity Lecture 18
Hooke’s Law in Voigt Notation Lecture 19
4 6.1 Hypothesis of the Linear Elasticity Theory Ch.6. Linear Elasticity
5 Hypothesis of the Linear Elastic Model
The simplifying hypothesis of the Theory of Linear Elasticity are:
1. ‘Infinitesimal strains and deformation’ framework
2. Existence of an unstrained and unstressed reference state
3. Isothermal, isentropic and adiabatic processes
8 Hypothesis of the Linear Elastic Model
1. ‘Infinitesimal strains and deformation’ framework the displacements are infinitesimal: material and spatial configurations or coordinates are the same ≈ 0 x= Xu + xX≈ material and spatial descriptions of a property & material and spatial differential operators are the same: xX= γγ()()()()xXXx,t= , t =Γ=Γ ,, tt ∂•() ∂•() = ∇∇()•=() • ∂∂Xx ∂x the deformation gradientF1 = ≈ F1 ≈ , so the current spatial ∂X density is approximated by the density at the reference configuration.
ρρ0 =ttF ≈ ρ Thus, density is not an unknown variable in linear elastic problems.
9 Hypothesis of the Linear Elastic Model
1. ‘Infinitesimal strains and deformation’ framework the displacement gradients are infinitesimal: The strain tensors in material and spatial configurations collapse into the infinitesimal strain tensor. EX()()(),,,ttt≈= exε x
10 Hypothesis of the Linear Elastic Model
2. Existence of an unstrained and unstressed reference state It is assumed that there exists a reference unstrained and unstressed neutral state, such that,
εε00()()xx0=,t =
σσ00()()x= x0,t = The reference state is usually assumed to correspond to the reference configuration.
11 Hypothesis of the Linear Elastic Model
3. Isothermal and adiabatic (=isentropic) processes In an isothermal process the temperature remains constant.
θθ()()()xx,,tt≡≡00 θ x ∀ x
In an isentropic process the entropy of the system remains constant. ds sts(XX ,)= ( ) = = 0 s = 0 dt In an adiabatic process the net heat transfer entering into the body is zero.
= ρ − ⋅ = ∀∆ ⊂ Qe0 ∫∫ r dV qn dS 0 V V VV∂ heat conduction internal REMARK from the exterior sources An isentropic process is an
ρ0 rt−⋅=∇ qx0 ∀∀ idealized thermodynamic process that is adiabatic, isothermal and reversible. 12 6.2 Linear Elastic Constitutive Equation Ch.6. Linear Elasticity
13 Hooke’s Law
R. Hooke observed in 1660 that, for relatively small deformations of an object, the displacement or size of the deformation is directly proportional to the deforming force or load. σ F= kl ∆ Fl∆ = E E Al F ε σ=E ε
Hooke’s Law (for 1D problems) states that in an elastic material strain is directly proportional to stress through the elasticity modulus.
14 Generalized Hooke’s Law
This proportionality is generalized for the multi-dimensional case in the Theory of Linear Elasticity. = σε(x,tt) () x:( x ,) C Generalized σεij= C ijkl kl ij,∈{ 1, 2, 3} Hooke’s Law It constitutes the constitutive equation of a linear elastic material. th The 4 order tensor is the constitutive elastic constants tensor: Has 34=81 components. Has the following symmetries, reducing the tensor to 21 independent components: REMARK minor CCijkl= jikl symmetries The current stress at a point CCijkl= ijlk depends only on the current strain at the point, and not on the past major = symmetries CCijkl klij history of strain states at the point.
15 Elastic Potential
The internal energy balance equation for the (adiabatic) linear elastic model is
global form stress power heat transfer rate d duρ ρρ u dV = 0 dV=σ :d dV +() r −∇⋅q dV dt ∫00 ∫dt ∫∫ V V VV= ε internal energy infinitesimal strains REMARK ()Vt ≡∀ Vt local form The rate of strain tensor is related to the d material derivative of the material strain T ()ρρ0 ur=σ : ε + −∇⋅q = ⋅⋅ dt tensor through: E F dF In this case, E = ε and F = 1 . Where: u is the specific internal energy (energy per unit mass). r is the specific heat generated by the internal sources. q is the heat conduction flux vector per unit surface.
16 Elastic Potential
The stress power per unit of volume is an exact differential of the internal energy density, uˆ , or internal energy per unit of volume: d duˆ(,)x t REMARK ()ρ0 uu= =ˆ = σε: dt dt The symmetries of the uˆ constitutive elastic Operating in indicial notation: constants tensor are used: duˆ 1 = =σε: =εσ=εε=εε+εε=C() CC minor CCijkl jikl ij ij ij ijkl kl ij ijkl kl ij ijkl kl dt C:ε 2 symmetries = Cijklε kl ik↔ CCijkl ijlk jl↔ major 11 CCijkl= klij =εε+ε=εε+εε=()ijC ijkl klε kl C klij ij ( ij CC ijkl kl ij ijkl kl ) symmetries 22 C d ijkl (εεC ) dt ij ijkl kl 1 d duˆ d 1 =εεijC ijkl kl = ()εε::C 2 dt dt dt 2 εε::C 17 Elastic Potential
duˆ 1 d =σε: = () ε ::C ε dt2 dt
Consequences: 1. Consider the time derivative of the internal energy in the whole volume: dd d ∫∫uˆˆ()xx,, t dV= u() t dV=Uˆ() t = ∫σε : dV stress VVdt dt dt Vpower
In elastic materials we talk about deformation energy because the stress power is an exact differential.
REMARK The stress power, in elastic materials is an exact differential of the internal energy U ˆ . Then, in elastic processes, we can talk of the elastic energy U ˆ () t . 18 Elastic Potential
duˆ 1 d =σε: = () ε ::C ε dt2 dt
Consequences: 2. Integrating the time derivative of the internal energy density, 1 utˆ ()x,,= εε()()() x t ::xC , ta+ x 2 and assuming that the density of the internal energy vanishes at the
neutral reference state, ut ˆ () xx ,0 0 = ∀ :
1 = 0 11 εε+==∀ ˆ ε= ε ε = σε ε ()()()x,t00 ::xC , ta x a () x 0 x u () :C : ( ): 2 22σ Due to thermodynamic reasons the internal energy is assumed always positive 1 uˆ ()ε= εε::C > 0∀≠ ε0 2
19 Elastic Potential σε()()x,tt= C () x: x ,
The internal energy density defines a potential for the stress tensor, and is thus, named elastic potential. The stress tensor can be computed as =σσT = ∂∂utˆ(ε (x , )) 1 1 1 1 ∂uˆ ()ε =(ε::CC ε) = : ε + ε : C = ( σ += σ ) σ σ = ∂∂εε ∂ε 2 222= σ
The constitutive elastic constants tensor can be obtained as the second derivative of the internal energy density with respect to the strain tensor field,
2 ∂σε() ∂∂2uˆ ()εε()C : ∂ uˆ ()ε = = = C Cijkl = ∂ε ∂ εε ⊗∂ ∂ ε ∂εij ∂ε kl
20 6.3 Isotropic Linear Elasticity
Ch.6. Linear Elasticity
21 Isotropic Constitutive Elastic Constants Tensor
An isotropic elastic material must have the same elastic properties (contained in C ) in all directions. All the components of C must be independent of the orientation of the chosen (Cartesian) system C must be a (mathematically) isotropic tensor.
C =λµ11 ⊗+2 I =++λδ δ µ δ δ δ δ ∈ Cijkl ij kl( ik jl il jk ) i, jkl , ,{} 1, 2, 3
Where: 1 is the 4th order unit tensor defined as []I =δδ + δδ I ijkl 2 ik jl il jk λ and µ are scalar constants known as Lamé‘s parameters or coefficients. REMARK The isotropy condition reduces the number of independent elastic constants from 21 to 2.
22 Isotropic Linear Elastic Constitutive Equation
Introducing the isotropic constitutive elastic constants tensor C = λµ 11 ⊗+ 2 I into the generalized Hooke’s Law σε = C : , in index notation:
σij=C ijkl ε kl =( λδ ij δ kl + µ( δ ik δ jl + δ il δ jk) ) ε= kl = ε 11ij =λδδij kl ε+ kl 2 µδδik jl ε+ kl δδ il jk ε kl = λTr()ε δµij + 2 ε ij 22 =εε = =εll = Tr(ε) ji ij 1 1 = ε+ εε= 2 ij 2 ij ij And the resulting constitutive equation is, Isotropic linear elastic σεε=λµTr ()1 + 2 constitutive equation. σ=+∈ λδ ε µ ε ij ij ll2 ij ij ,{} 1, 2, 3 Hooke’s Law
23 Elastic Potential
If the constitutive equation is, σεε=λµTr ()1 + 2 Isotropic linear elastic constitutive equation. σij=+∈ λδ ij ε ll2 µ ε ij ij ,{} 1, 2, 3 Hooke’s Law
Then, the internal energy density can be reduced to:
11 REMARK uˆ ()ε= σ : ε=(λµTr () ε1 + 2 ε) : ε= 22 The internal energy density is an =σ elastic potential of the stress tensor 11 as: =λµ ε1 ε+ ε:ε= Tr () :2 22ε ∂uˆ ()ε Tr( ) =σε()() =λµTr εε1 + 2 ∂ε 1 =λµTr2 ()ε + ε:ε 2
24 Inversion of the Constitutive Equation
1. ε is isolated from the expression derived for Hooke’s Law 1 σεε=λµTr ()1 + 2 ε=( σ−λ Tr () ε 1) 2µ 2. The trace of σ is obtained: Tr ()()σ= Tr(λ Tr ε11 +2 µ ε=) λ Tr()()()()() ε Tr+=+ 2 µ Tr ε 3 λµ 2 Tr ε =3 3. The trace of ε is easily isolated: 1 Tr ()εσ= Tr () 32λµ+ 4. The expression in 3. is introduced into the one obtained in 1. 11λ 1 ε= σ−λ Tr ()σ 1 ε=− Tr ()σ1 + σ 2µ 32 λµ+ 23µλ()+ 2 µ 2 µ
25 Inverse Isotropic Linear Elastic λ 1 ε=− Tr ()σ 1 + σ Constitutive Equation 23µλ()+ 2 µ 2 µ
The Lamé parameters in terms of E and ν : µλ()32+ µ ν E E = λ = λµ+ ()()1+−νν 12 λ E ν = µ =G = 2()λµ+ 21()+ν So the inverse const. eq. is re-written: νν1+ εσσ=−+Tr () 1 Inverse isotropic linear EE elastic constitutive equation. νν1+ ε=−+∈ σδ σ ij,{} 1, 2, 3 Inverse Hooke’s Law. ij EEll ij ij 11 εx =( σx −+ νσ() y σ z ) γxy = τ xy EG 11 εy =( σy −+ νσ()x σ z ) γxz = τ xz In engineering notation: EG 11 εz =( σz −+ νσ()x σ y ) γyz = τ yz EG
26 Young’s Modulus and Poisson’s Ratio
Young's modulus E is a measure of the stiffness of an elastic material. It is given by the ratio of the uniaxial stress over the uniaxial strain.
µλ()32+ µ E = λµ+
Poisson's ratio ν is the ratio, when a solid is uniaxially stretched, of the transverse strain (perpendicular to the applied stress), to the axial strain (in the direction of the applied stress).
λ ν = 2()λµ+
27 Example
Consider an uniaxial traction test of an isotropic linear elastic material such that: σ > x 0 E, ν y σστy= z = xy = τ xz = τ yz = 0 σ x σ x
σ x σ x x
z
Obtain the strains (in engineering notation) and comment on the results obtained for a Poisson’s ratio of ν = 0 and ν = 0.5 .
28 11 εx =( σx −+ νσ() y σ z ) γxy = τ xy σ > 0 EG x 11 εy =( σy −+ νσ() x σ z ) γxz = τ xz σστy= z = xy = τ xz = τ yz = 0 EG Solution 11 εz =( σz −+ νσ() x σ y ) γyz = τ yz EG
For ν = 0 : 1 εσx= x γxy = 0 1 There is no Poisson’s effect E εσx= x γxy = 0 E ν and the transversal normal ε=−= σγ0 εγ= 00= y E x xz y xz strains are zero. εγ= 00= ν z yz ε=−= σγ0 z E x yz
For ν = 0.5 : 1 1 The volumetric deformation is εσx= x γxy = 0 εσx= x γxy = 0 ε =++=εεε E E zero, tr xyz 0 , the 1 0.5 ε=−= σγ material is incompressible ε=−= σγ0 y x xz 0 y E x xz 2E and the volume is preserved. 1 0.5 ε=−= σγ ε=−= σγ0 z x yz 0 z E x yz 2E
29 Spherical and deviatoric parts of Hooke’s Law
The stress tensor can be split into a spherical, or volumetric, part and a deviatoric part: 1 σσ:=σ 11 = Tr () sph m 3 σσ=σ m1 + ′ σ′ =dev σ = σ−σ m1
Similarly for the strain tensor: 11 εε=11 = ) sph e Tr ( 1 33 εε= +e1 ´ 1 ε′ = dev εε= − e1 3 3
30 Spherical and deviatoric parts of Hooke’s Law
Operating on the volumetric strain: e = Tr()ε
νν1+ εσ=−+Tr () 1 σ EE
νν1+ e =−+Tr()()σσ Tr1 Tr() EE = 3 = 3σ m K : bulk modulus 31()− 2ν E (volumetric strain modulus) e = σ σ m = e E m 31()− 2ν def 2 E K =+=λµ 3 3(1− 2ν ) The spherical parts of the stress and strain tensor are directly related: σ m = Ke
31 Spherical and Deviator Parts of Hooke’s Law
νν1+ Introducing σσ = σ 1 + ′ into εσσ =−+ Tr () 1 : m EE νν1+ ε =−+++Tr ()σσ11σσ′′() 1 EEmm ν ν = 0 ++ν ν + νν + ν ′′1 1 13 1 ′ =−−σσmmTr()11 Tr ()σσ 1 + 1 +=−+ σm1 σ E= 3 E E E EE E E Taking into account that σ m = e : 31()− 2ν Comparing this 12−ν 1E 1 ++ νν 1 1 ε = ee11+=+σσ′′with the expression − ν 1 E312() EE3 εε= e1 ´+ 3 1+ν 11 1+ν = = ε´= σ ′ E 2µ 2G E The deviatoric parts of the stress and strain tensor are related component by component: σ ′′= 2Gε σεij ′′=2G ij ij , ∈ {1, 2, 3}
32 Spherical and deviatoric parts of Hooke’s Law
The spherical and deviatoric parts of the strain tensor are directly proportional to the spherical and deviatoric parts (component by component) respectively, of the stress tensor:
σε′′= 2G σ m = Ke ij ij
33 Elastic Potential
The internal energy density uˆ () ε defines a potential for the stress tensor and is, thus, an elastic potential: REMARK 1 ∂ ε ˆ ε= εε uˆ ( ) The constitutive elastic constants u () ::C σε= = : 2 ∂ε tensor C is positive definite due to thermodynamic considerations. Plotting u ˆ () ε vs. ε :
There is a minimum for ε = 0 :
∂uˆ ()ε =:()C ε = 0 ∂ε ε=0 ε=0
∂∂22uuˆˆ()εε() = =CC = ∂εε ⊗∂ ∂ εε ⊗∂ ε=0 εε=00=
34 Elastic Potential
The elastic potential can be written as a function of the spherical and deviatoric parts of the strain tensor: ε::CC ε= ( :: ε) ε=σ : ε 111 uˆ (ε) = ε::C ε = σε := λµTr (ε) 1 + 2 ε: ε= 222 = σ 11 =ee11 +εε´´: += = Tr (ε ) = e = e2 33 112 =λTr (ε) 1:: ε += µλ εεTr ( ε) + µ εε: 12 22=ee2 11: + 1 ::ε´ += εε ´´ 93 3 Tr(ε′)=0 K 122 1 122 1 2 uˆ (ε) =λ ee ++=+ µμεε´: ´ λµeμ +εε´: ´ =e + εε´´: 2 3 23 3 Elastic potential in terms of the 1 uˆ (ε) = Ke2 +≥µ εε´: ´ 0 spherical and deviatoric parts 2 of the strains.
35 Limits in the Elastic Properties
The derived expression must hold true for any deformation process: 1 uˆ ()ε=:Ke2 +≥µ εε´ :´ 0 2 Consider now the following particular cases of isotropic linear elastic material: Pure spherical deformation process ()1 1 ε = e 1 1 3 uˆ()1 = Ke2 ≥ 0 K > 0 bulk modulus 1 2 ε′() = 0 Pure deviatoric deformation process εε()2 = ′ Lamé’s second uˆ()2 =µ εε´´0: ≥ µ > 0 e()2 = 0 parameter REMARK ′′ εε:0=εεij ij ≥ 36 Limits in the Elastic Properties
K and µ are related to E and ν through:
E E K = > 0 µ =G = > 0 31()− 2ν 21()+ν REMARK In rare cases, a material can Poisson’s ratio has a non-negative value, have a negative Poisson’s ratio. E Such materials are named > 0 21()+ν E ≥ 0 Young’s auxetic materials. modulus ν ≥ 0
Therefore, E > 0 − ν 1 31() 2 0 ≤≤ν Poisson’s ratio E ≥ 0 2
37 6.4 The Linear Elastic Problem
Ch.6. Linear Elasticity
38 Introduction
The linear elastic solid is subjected to body forces and prescribed tractions: Initial actions: bx(),0 t = 0 tx(),0
bx(),t Actions through time: tx(),t
The Linear Elastic problem is the set of equations that allow obtaining the evolution through time of the corresponding displacements ux () , t , strains ε () x , t and stresses σ () x , t .
39 Governing Equations
The Linear Elastic Problem is governed by the equations: 1. Cauchy’s Equation of Motion. Linear Momentum Balance Equation. ∂2ux(),t ∇σ ⋅+()()x,,ttρρ bx = 00∂ t 2 2. Constitutive Equation. Isotropic Linear Elastic Constitutive Equation. This is a PDE system of σ ()()x,2t=λµ Tr εε1 + 15 eqns -15 unknowns: ux(),t 3 unknowns 3. Geometrical Equation. ε()x,t 6 unknowns Kinematic Compatibility. σ ()x,t 6 unknowns S 1 Which must be solved in ε()()x,,tt= ∇ ux =( u ⊗+⊗∇∇ u) 3 2 the RR × + space.
40 Boundary Conditions
Boundary conditions in space Affect the spatial arguments of the unknowns Are applied on the boundary Γ of the solid, which is divided into three parts: Prescribed displacements on Γ u : ux(,)tt= u* (,) x * ∀x ∈Γu ∀t uii()(){}xx, tu= , ti ∈ 1, 2, 3
Prescribed tractions on Γ σ : Γuu Γσσ Γ =Γ≡∂V σ ⋅= * (,)xnttt (,) x Γu Γ=Γσ uu Γ σ =Γ u σσ Γ=/{0} ∀x ∈Γσ ∀t σ ⋅= * ∈ ij ()(){}xx, tnj t j , t i 1, 2, 3
Prescribed displacements and stresses on Γ u σ : * uii()()xx,, tu= t (i, jk ,∈{} 1, 2, 3 i ≠ j) ∀x ∈Γσ ∀t σ ⋅=* u jk ()()xx,,tnk t j t
41 Boundary Conditions
42 Boundary Conditions
Boundary conditions in time. INTIAL CONDITIONS. Affect the time argument of the unknowns. Generally, they are the known values at t = 0 : Initial displacements: ux(),0 = 0 ∀∈ x V
Initial velocity: ∂ux(),t not =ux ()(),0 = v x ∀∈ x V ∂ 0 t t=0
43 The Linear Elastic Problem
Find the displacements ux () , t , strains ε () x , t and stresses σ () x , t such that
∂2ux(),t ∇σ⋅+()() x,,ttρρ00 bx = Cauchy’s Equation of Motion ∂ t 2 σ()()x,2t=λµ Tr εε1 + Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary conditions in space Γ=⋅σ : tnσ
ux(),0 = 0 Initial conditions (Boundary conditions in time) ux (),0 = v0
44 Actions and Responses
The linear elastic problem can be viewed as a system of actions or data inserted into a mathematical model made up of the EDP’s and boundary conditions , which gives a response (or solution) in displacements, strains and stresses. bx(),t * ux(),t tx(),t Mathematical * model ε()x,t ux(),t EDPs+BCs σ ()x,t vx0 () not not RESPONSES = R ()x,t ACTIONS = A ()x,t Generally, actions and responses depend on time. In these cases, the 3 problem is a dynamic problem, integrated in RR × + . In certain cases, the integration space is reduced to R 3 . The problem is termed quasi-static.
45 The Quasi-Static Problem
A problem is said to be quasi-static if the acceleration term can be considered to be negligible. ∂2ux(,)t a0= ≈ ∂ t 2
This hypothesis is acceptable if actions are applied slowly. Then, ∂2ux(,)t 22 22 ≈ ∂A/ ∂≈t 0 ∂R/ ∂≈t 0 2 0 ∂ t
46 The Quasi-Static Problem
Find the displacements ux () , t , strains ε () x , t and stresses σ () x , t such that ∂2ux(),t ρ ≈ 0 0 ∂ t 2
∇σ ⋅+()()x,,ttρ0 bx = 0 Equilibrium Equation
σ()()x,2t=λµ Tr εε1 + Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in Space Γ=⋅σ : tnσ
ux(),0 = 0 Initial Conditions ux (),0 = v0
47 The Quasi-Static Problem
The quasi-static linear elastic problem does not involve time derivatives. Now the time variable plays the role of a loading descriptor: it describes the evolution of the actions.
λ bx(), Mathematical ux(),λ * tx(),λ model ε()x,λ * ux(),λ EDPs+BCs σ ()x,λ not not ACTIONS = A ()x,λ RESPONSES = R ()x,λ
* For each value of the actions A () x , λ * -characterized by a fixed value λ - a response R () x , λ * is obtained. Varying λ * , a family of actions and its corresponding family of responses are obtained.
48 Example
Consider the typical material strength problem where a cantilever beam is subjected to a force Ft () at it’s tip. For a quasi-static problem,
The response is δ () tt = δλ (( )) , so for every time instant, it only depends on the corresponding value λ () t .
49 Solution of the Linear Elastic Problem
To solve the isotropic linear elastic problem posed, two approaches can be used: Displacement formulation - Navier Equations Eliminate σ () x , t and ε () x , t from the general system of equations. This generates a system of 3 eqns. for the 3 unknown components of ux () , t . Useful with displacement BCs. Avoids compatibility equations. Mostly used in 3D problems. Basis of most of the numerical methods.
Stress formulation - Beltrami-Michell Equations. Eliminates ux () , t and ε () x , t from the general system of equations. This generates a system of 6 eqns. for the 6 unknown components of σ () x , t . Effective with boundary conditions given in stresses. Must work with compatibility equations. Mostly used in 2D problems. Can only be used in the quasi-static problem.
50 Displacement formulation
∂2ux(),t ∇σ⋅+()()x,,ttρρ00 bx = Cauchy’s Equation of Motion ∂ t 2 σ()()x,2t=λµ Tr εε1 + Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in Space Γ=⋅σ : tnσ
ux(),0 = 0 Initial Conditions ux (),0 = v0
The aim is to reduce this system to a system with ux () , t as the only unknowns. Once these are obtained, ε () x , t and σ () x , t will be found through substitution.
51 Displacement formulation
Introduce the Constitutive Equation into Cauchy’s Equation of motion: σ()()x,2t=λµ Tr εε1 + ∂2u λ∇⋅ ε1 + µ ∇ε ⋅+ ρρ = []Tr() 2 00b 2 ∂2ux(),t ∂ t ∇σ⋅+()()x,,ttρρ bx = 00∂ t 2 Consider the following identities: = ∇∇⋅u ()() i ∂ ∂∂uu ∂∂ ∂ ∇ε⋅()Tr()1u =εδ =kk δ = =()∇ ⋅= i ()11 ij ij ∂xj ∂∂ xxjk ∂∂ xx ik ∂ x i = ∇ ⋅ u =⋅∈∇∇(){}u i 1, 2, 3 i
∇⋅=⋅()Tr () ε1 ∇∇()u
52 Displacement formulation
Introduce the Constitutive Equation into Cauchy’s Equation of motion: σ()()x,2t=λµ Tr εε1 + ∂2u λ∇⋅ ε1 + µ ∇ε ⋅+ ρρ = []Tr() 2 00b 2 ∂2ux(),t ∂ t ∇σ⋅+()()x,,ttρρ bx = 00∂ t 2 Consider the following identities: = ∇2 u = ()∇∇()⋅u () i i ∂∂ε ∂1∂∂uuuu 112 ∂∂ ∂ 11 ()∇ε⋅ =ij =ii +j = +j =∇2 u +()∇ ⋅=u i () ∂ ∂ ∂ ∂ ∂∂ ∂ ∂ i ∂ xj x j2 x j x i 22 xxjj x i x j 22xi = ∇ ⋅ 112 u =∇uu +⋅ ∇∇(){}i ∈1, 2, 3 22 i 11 ∇⋅= ε ∇∇() ⋅uu + ∇2 22
53 Displacement formulation
Introduce the Constitutive Equation into Cauchy’s Equation of Movement: σ()()x,2t=λµ Tr εε1 + ∂2u λ∇⋅ ε1 + µ ∇ε ⋅+ ρρ = []Tr() 2 00b 2 ∂2ux(),t ∂ t ∇σ⋅+()()x,,ttρρ bx = 00∂ t 2 Replacing the identities: 11 ∇⋅=⋅()Tr () ε1 ∇∇()u ∇⋅= ε ∇∇() ⋅uu + ∇2 22 2 nd 112 ∂ u 2 order Then, λ∇() ∇⋅+u2 µ ∇∇ () ⋅+ u ∇ ub +ρρ00 = 22 ∂ t 2 PDE system ∂2u ()()λµ+∇∇ ⋅+u µ ∇2 ub + ρ = ρ The Navier Equations 002 ∂t are obtained: ()λµ+uj, ji + µ u i ,0 jj += ρ bu i ρ 0 i i ∈{}1, 2, 3
54 Displacement formulation
The boundary conditions are also rewritten in terms of ux () , t : σ()()x,2 t=λµ Tr εε1 + = ∇ ⋅ u t* =λµTr ()εε nn +⋅2 () 1 * =∇ S u =(uu ⊗+⊗∇∇ ) tn=σ ⋅ 2 t* =λµ()(∇ ⋅ un + u ⊗+⊗ ∇∇ u) ⋅ n The BCs are now:
uu= * on Γu * uii= ui ∈{}1, 2, 3
* REMARK λµ()(∇⋅un + u ⊗ ∇∇ + ⊗ u) ⋅= n t on Γσ The initial conditions λµun+ un +=∈ un t* i{}1, 2, 3 kk. i( i ,, j j ji j) i remain the same.
55 Displacement formulation
Navier equations in a cylindrical coordinate system: ∂eG2 ∂∂ω ∂ω 2u λ+ −zr +θ +=ρρ xr= cosθ ()22G Gbr 2 ∂∂rrθ ∂ z ∂ t x(r ,θθ , z )≡= yr sin 1 ∂e ∂∂ωω ∂2u ()λ+2G − 22 GGrz + +=ρρ b θ zz= r∂∂∂θ zrθ ∂ t2 ∂∂eG22 G∂∂ω 2u () λ+2Gr −()ω +rz += ρρ b ∂∂z rrθ r ∂θ z ∂t2
11∂uz ∂uθ ωrz= −Ωθ = − 2 rz∂∂θ
1 ∂∂uurz dV= r dθ dr dz Where: ωθ = −Ωzr = − 2 ∂∂zr
11∂ ()ruθ 1∂u r 11∂ ∂uθ ∂uz ωzr= −Ωθ = − e=() ru ++ 2 rr∂∂ rθ rr∂r r ∂∂θ z
56 Displacement formulation
Navier equations in a spherical coordinate system:
2 ∂∂eG22G∂ωθ ∂ ur ()λ+2Gb − ()ωθϕ sin + +=ρr ρ ∂∂rrsinθθ rsinθ ∂ ϕ ∂t2 xr= sinθϕ cos =θϕ ≡= θ ϕ λ + 2G ∂∂∂ω ∂2 xx()r, , yr sin sin () eG22r G uθ − + ()rbωϕθsin θρ+= ρ zr= cosθ r ∂∂∂θ rsin θϕ rr sin θ ∂t2 λ + ∂2 () 2G ∂∂eG22 G∂ωr uϕ −ω + += ρρ 2 ()rbθϕ2 = θ θϕ rsinθϕ∂∂ rr r ∂θ ∂t dV rsin dr d d
11∂ 1∂uθ ωr = −Ωθϕ = ()uϕ sin θ − 2rr sin θ∂∂ θ sin θ φ Where: 11∂u 1∂ ()ruϕ ω = −Ω = r − θϕr 2r sin θφ∂∂ rr
11∂ 1∂ur ωϕθ= −Ωr = ()ruθ− 2 rr∂∂ r θ 1 ∂ ∂∂ =2 θθ ++ e 2 ()r ur sin ()ruθϕsin ()ru rrsinθ∂∂∂ θϕ 57 Stress formulation
Equilibrium Equation ∇σ⋅+x,ttρ bx ,0 = ()()0 (Quasi-static problem) νν1+ ε()x,t=−+ Tr () σσ1 Inverse Constitutive Equation EE 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in Space Γ=⋅σ : tnσ
The aim is to reduce this system to a system with σ () x , t as the only unknowns. Once these are obtained, ε () x , t will be found through substitution and ux () , t by integrating the geometric equations. REMARK For the quasi-static problem, the time variable plays the role of a loading factor.
58 Stress formulation
Taking the geometric equation and, through successive derivations, the displacements are eliminated: 2222 Compatibility Equations ∂∂εεij ∂∂εε jl +−−=kl ik 0i , jkl , , ∈{} 1, 2, 3 ∂x ∂ x ∂∂ xx ∂ x ∂ x ∂∂ xx (seen in Ch.3.) kl i j jl ik Introducing the inverse constitutive equation into the compatibility equations and using the equilibrium equation: νν1+ ε=−σδ + σ ij EEpp ij ij ∂σ ij +=ρ0bj 0 ∂xi 2nd order Beltrami-Michell Equations The are obtained: PDE system 2 ∂∂ρρ∂ ρ b 2 1 ∂ σ kk ν ()00bbki() ()0 j ∇+σδij =− ij − − ij,∈{} 1, 2, 3 11+νν ∂∂xxij − ∂xk ∂ xj ∂ x i
59 Stress formulation
The boundary conditions are: Equilibrium Equations: ∇σ⋅+ρ0b =0 This is a 1st order PDE system, so they can act as boundary conditions of the (2nd order PDE system of the) Beltrami-Michell Equations
* Prescribed stresses on : Γ σ σ ⋅=nt on Γσ
60 Stress formulation
Once the stress field is known, the strain field is found by substitution. νν1+ ε()x,t=−+ Tr () σσ1 EE The calculation, after, of the displacement field requires that the geometric equations be integrated with the prescribed displacements on Γ : u 1 ε()x=( ux () ⊗+⊗∇∇ ux ()) x ∈V 2 * ux()= u () x ∀ x ∈Γu
REMARK This need to integrate the second system is a considerable disadvantage with respect to the displacement formulation when using numerical methods to solve the lineal elastic problem.
61 Saint-Venant’s Principle
From A. E. H. Love's Treatise on the mathematical theory of elasticity: “According to the principle, the strains that are produced in a body by the application, to a small part of its surface, of a system of forces statically equivalent to zero force and zero couple, are of negligible magnitude at distances which are large compared with the linear dimensions of the part.” REMARK This principle does not have a Expressed in another way: rigorous mathematical proof. “The difference between the stresses caused by statically equivalent load systems is insignificant at distances greater than the largest dimension of the area over which the loads are acting.”
(I) (II) ux()()PP,,tt≈ u x (I) (II) εε()()xxPP,,tt≈ ∀P | δ >> (I) (II) σσ()()xxPP,,tt≈
62 Saint-Venant’s Principle
Saint Venant’s Principle is often used in strength of materials. It is useful to introduce the concept of stress: The exact solution of this problem is very complicated.
This load system is statically equivalent to load system (I). The solution of this problem is very simple.
Saint Venant’s Principle allows approximating solution (I) by solution (II) at a far enough distance from the ends of the beam.
63 Uniqueness of the solution
The solution of the lineal elastic problem is unique: It is unique in strains and stresses. It is unique in displacements assuming that appropriate boundary conditions hold in order to avoid rigid body motions.
This can be proven by Reductio ad absurdum ("reduction to the absurd"), as shown in pp. 189-193 of the course book. This proof is valid for lineal elasticity in infinitesimal strains. The constitutive tensor C is used, so proof is not only valid for isotropic problems but also for orthotropic and anisotropic ones.
64 6.5 Linear Thermoelasticity
Ch.6. Linear Elasticity
65 Hypothesis of the Linear Thermo-elastic Model
The simplifying hypothesis of the Theory of Linear Thermo- elasticity are:
1. Infinitesimal strains and deformation framework Both the displacements and their gradients are infinitesimal.
2. Existence of an unstrained and unstressed reference state The reference state is usually assumed to correspond to the reference configuration. εε00()()xx0=,t =
σσ00()()x= x0,t = 3. Isentropic and adiabatic processes – no longer isothermal !!! Isentropic: entropy of the system remains constant Adiabatic: deformation occurs without heat transfer
66 Hypothesis of the Linear Thermo-Elastic Model
3. ( Hypothesis of isothermal process is removed) The process is no longer isothermal so the temperature changes throughout time: not θθ()()xx,t ≠= ,0 θ0 ∂θ ()x,t θ()x,0t = ≠ ∂t We will assume the temperature field is known.
But the process is still isentropic and adiabatic: s() t≡ cnt s = 0
=ρ − ⋅ = ∀∆ ⊂ Qe ∫∫ r dV qn dS 0 V V VV∂ internal heat conduction sources from the exterior ρ rt−⋅=∇ qx0 ∀∀
67 Generalized Hooke’s Law
The Generalized Hooke’s Law becomes:
σ()()()()xx,tt=CC :, εβ −θθ −0 =:, εβ x t −∆θ Generalized Hooke’s Law for σ=C ε −− βθθ(){}ij, ∈ 1, 2, 3 linear thermoelastic problems ij ijkl kl ij 0 Where is the elastic constitutive tensor. θ () x , t is the absolute temperature field.
θθ 00 = () x , t is the temperature at the reference state. β is the tensor of thermal properties or constitutive thermal constants tensor. It is a positive semi-definite symmetric second-order tensor. REMARK A symmetric second-order tensor A is positive semi-definite when zT·A·z > 0 for every non-zero column vector z. 68 Isotropic Constitutive Constants Tensors
An isotropic thermoelastic material must have the same elastic and thermal properties in all directions: th must be a (mathematically) isotropic 4 order tensor: C =λµ11 ⊗+2 I =++λδ δ µ δ δ δ δ ∈ Cijkl ij kl( ik jl il jk ) i, j , kl .{} 1, 2, 3 Where: 1 th I is the 4 order symmetric unit tensor defined as []I =δδik jl + δδ il jk ijkl 2 λ and µ are the Lamé parameters or coefficients.
β is a (mathematically) isotropic 2nd order tensor: β = β 1 β=βδ ∈ ij ij ij,{} 1, 2, 3 Where: β is a scalar thermal constant parameter.
69 Isotropic Linear Thermoelastic Constitutive Equation
Introducing the isotropic constitutive constants tensors β = β 1 and
C = λµ 11 ⊗+ 2 I into the generalized Hooke’s Law, σ = C : εβ −−()θθ0 (in indicial notation)
σij=C ijkl ε kl − βθθ ij () −=00( λδδij kl + µδδ( ik jl + δδ il jk) ) ε kl − βθθδ() −ij = = ε 11ij = λδδεij kl kl +2 µ δδεik jl kl + δδε il jk kl −− βθθδ()0 ij 22 = εll =εεji = ij = ∆θ = εij The resulting constitutive equation is,
σεε=λTr ()11 +2 µ −∆ βθ Isotropic linear thermoelastic σ= λδ ε + µ ε −∆ β θ δ ∈ constitutive equation. ij ij ll2 ij ij ij,{} 1, 2, 3
70 Inversion of the Constitutive Equation
1. ε is isolated from the Generalized Hooke’s Law for linear thermoelastic problems: εσ=−−11:: +∆θ β σε=: −∆β θ CC C α 2. The thermal expansion coefficients tensor α is defined as: def − αβ= C 1 : It is a 2nd order symmetric tensor which involves 6 thermal expansion coefficients
3. The inverse constitutive equation is obtained: − εσ=C 1 : +∆θ α
71 Inverse Isotropic Linear Thermoelastic Constitutive Equation
For the isotropic case:
− νν1+ C 1 =−11 ⊗+ I 12− ν EE →=α=−1 ββ11 C : () −1 νν1+ E Cijkl =−++δδij kl ( δδik jl δδ il jk ) i, j , kl . ∈{} 1, 2, 3 EE The inverse const. eq. is re-written: νν1+ εσσ=−Tr () 11 + +∆αθ EE Inverse isotropic linear thermo νν1+ elastic constitutive equation. ε=− σ δ + σ +∆ α θδ ij, ∈ 1, 2, 3 ij ll ij ij ij {} EE Where α is a scalar thermal expansion coefficient related to the scalar thermal constant parameter β through: 12− ν αβ= E 72 Thermal Stress
Comparing the constitutive equations,
σεε=λµ Tr ()1 + 2 Isotropic linear elastic constitutive equation. σεε=λ Tr ()11 +2 µ −∆ βθ Isotropic linear thermoelastic constitutive equation. t = σnt = σ
the decomposition is made: σσ=nt − σ t Where: σ nt is the non-thermal stress: the stress produced if there is no temperature increment. σ t is the thermal stress: the “corrector” stress due to the temperature increment.
73 Thermal Strain
Similarly, by comparing the inverse constitutive equations,
νν1+ Inverse isotropic linear elastic εσσ=−+ Tr () 1 EE constitutive eq. νν1+ εσσ=− Tr () 11 + +∆αθ Inverse isotropic linear thermoelastic EE t constitutive eq. = εnt = ε the decomposition is made: εε=nt + ε t Where: ε nt is the non-thermal strain: the strain produced if there is no temperature increment. ε t is the thermal strain: the “corrector” strain due to the temperature increment.
74 Thermal Stress and Strain
The thermal components appear when thermal processes are considered.
NON-THERMAL THERMAL TOTAL COMPONENT COMPONENT
σεnt = C : σβt = ∆θ σσ=nt − σ t Isotropic material: Isotropic material: σnt =λµTr() εε1 + 2 σt =βθ ∆ 1
− εσnt = C 1 : εαt = ∆θ εε=nt + ε t Isotropic material: Isotropic material: nt νν1+ ε=−+Tr() σσ1 εt =αθ ∆ 1 EE These are the equations used nt t in FEM codes. σ=CC:: ε = εε − −−11nt t ε=CC:: σ = σσ +
75 Thermal Stress and Strain
REMARK 1 In thermoelastic problems, a state of zero strain in a body does not necessarily imply zero stress. εσ=→=00nt
σσ=−t =−∆βθ1 ≠0
REMARK 2 In thermoelastic problems, a state of zero stress in a body does not necessarily imply zero strain. σε=→=00nt
εε==∆≠t αθ1 0
76 6.6 Thermal Analogies
Ch.6. Linear Elasticity
77 Solution to the Linear Thermoelastic Problem
To solve the isotropic linear thermoelastic problem posed thermal analogies are used. The thermoelastic problem is solved like an elastic problem and then, the results are “corrected” to account for the temperature effects. They use the same strategies and methodologies seen in solving isotropic linear elastic problems: Displacement Formulation - Navier Equations. Stress Formulation - Beltrami-Michell Equations. Two basic analogies for solving quasi-static isotropic linear thermoelastic problems are presented: 1st thermal analogy – Duhamel-Neumann analogy. 2nd thermal analogy
78 1st Thermal Analogy
The governing eqns. of the quasi-static isotropic linear thermoelastic problem are:
∇σ⋅+()()x,,ttρ0 bx = 0 Equilibrium Equation
σε()()x,,tt=C :x −∆βθ1 Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in Space Γ=⋅σ : tnσ
79 1st Thermal Analogy
The actions and responses of the problem are:
not not ()I ()I ACTIONS = A ()x,t RESPONSES = R ()x,t bx(),t ux(),t tx* (),t Elastic model ε()x,t * ux(),t EDPs+BCs σ ()x,t ∆θ ()x,t
REMARK ∆ θ () x , t is known a priori, i.e., it is independent of the mechanical response. This is an uncoupled thermoelastic problem.
80 1st Thermal Analogy
To solve the problem following the methods used in linear elastic problems, the thermal term must be removed. The stress tensor is split into σσ = nt − σ t and replaced into the governing equations: Momentum equations σ= σnt − σ t ∇ ⋅= σ ∇⋅σnt − ∇⋅ σ t = ∇⋅σnt − ∇()βθ ∆ βθ∆ 1
∇σ⋅+ρ0b0 = ∇⋅σnt +=ρ ˆ 1 0 b0 ∇ nt ⋅σ+ρ −∇ βθ ∆= 0 b0() 1 ρ0 bbˆ =−∆∇ ()βθ not ρ0 = bˆ
81 1st Thermal Analogy
Boundary equations: σ=σnt − σ t σσnt⋅−n t ⋅= nt* nt * * σ ⋅=ntˆ σ ⋅=nt Γσ : ˆ** σσnt ⋅=nt** +t ⋅ n = t +()βθ ∆ n tt=+∆()βθ n βθ∆⋅1 n tˆ* ANALOGOUS PROBLEM – A linear elastic problem can be solved as:
nt ˆ ˆ 1 ∇σ⋅+ρ0b0 = with bb=−∆∇()βθ Equilibrium Equation ρ0 σεεnt =C : =λµTr()1 + 2 ε Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu nt ˆ* ** Boundary Conditions in Space Γσ : σ ⋅=nt with ttˆ = +∆βθ n
82 1st Thermal Analogy
The actions and responses of the ANALOGOUS NON-THERMAL PROBLEM are:
not not ()II ()II ACTIONS = A ()x,t RESPONSES = R ()x,t
bxˆ (),t ux(),t Elastic model txˆ* (),t ε()x,t EDPs+BCs nt ux* (),t σ ()x,t
ORIGINAL PROBLEM (I) ANALOGOUS (ELASTIC) PROBLEM (II) 83 1st Thermal Analogy
If the actions and responses of the original and analogous problems are compared: ≡ b 1 b ˆˆ− ∇ ()βθ∆ ACTIONS b bb ρ ∗ 0 u u0∗ def ()I (,)tt−()II (,) = −= =0 =()III AAxx* * ** A t tˆˆ tt− * ≡ t −∆βθn () ∆θ 0 ∆θ ∆θ
RESPONSES uu 0 0 def ()I ()II ()III RR(,)xxtt− (,) =−=εε 0 = 0 =R nt nt σ σ σσ− −∆βθ1 = −σt
Responses are proven to be the solution of a thermoelastic problem under actions
84 1st Thermal Analogy
THERMOELASTIC ANALOGOUS THERMOELASTIC ORIGINAL ELASTIC (TRIVIAL) PROBLEM (I) PROBLEM (II) PROBLEM (III) 1 1 bx(),t bxˆ (),t =−∆ b ∇ ()βθ =∇ βθ ∆ ρ b () * 0 ρ0 tx(),t ** ()I ()II txˆ ()(),t =+∆ tβθ n ()III * x,t * x,t x,t tn=−∆()βθ A () ux(),t A () A () ux* (),t u0 ∗ = ∆θ ()x,t ∆=θ 0 ∆θ ()x,t
ux(),t ux(),t u0= ()I ()II ε()x,t ε()x,t ()III ε = 0 R ()x,t R ()x,t R ()x,t σ ()x,t σnt ()x,t σ =−=−∆σ t ()βθ1
86 2nd Thermal Analogy
The governing equations of the quasi-static isotropic linear thermoelastic problem are:
∇σ⋅+()()x,,ttρ0 bx = 0 Equilibrium Equation
εσ()()x,,tt=C-1 :x +∆αθ1 Inverse Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in Space Γ=⋅σ : tnσ
87 2nd Thermal Analogy
The actions and responses of the problem are:
not not ()I ()I ACTIONS = A ()x,t RESPONSES = R ()x,t bx(),t ux(),t tx* (),t Elastic model ε()x,t * ux(),t EDPs+BCs σ ()x,t ∆θ ()x,t
REMARK ∆ θ () x , t is known a priori, i.e., it is independent of the mechanical response. This is an uncoupled thermoelastic problem.
88 2nd Thermal Analogy
The assumption is made that ∆ θ (,) x t and α () x are such that the thermal t =αθ ∆ strain field ε1 is integrable (satisfies the compatibility equations). If the thermal strain field is integrable, there exists a field of thermal displacements, ux t () , t , which satisfies: 1 εt()()x,t =αθ ∆1 =∇Stuu =( t ⊗+⊗ ∇∇ ut) 2 1 ∂ ut ∂ ut εt =∆=+() α θδ i j ij, ∈{} 1, 2, 3 ij ij ∂∂ 2 xxji REMARK The solution ux t () , t is determined except for a rigid body motion characterized by a rotation tensor Ω ∗ and a displacement vector c * . The family of admissible solutions is u t ()() x ,, tt = ux + Ω ∗ ⋅+ x c * . This movement can be arbitrarily chosen (at convenience). Then, the total displacement field is decomposed by defining: def unt (,) xtt= ux (,) − ut (,) x t uu=nt + u t 89 2nd Thermal Analogy
To solve the problem following the methods used in linear elastic problems, the thermal terms must be removed. The strain tensor and the displacement vector splits, εε = nt + ε t and uu = nt + u t are replaced into the governing equations: Geometric equations:
S S nt t S nt S t S nt t ε∇=u = ∇() uu += ∇ u + ∇ u = ∇ u + ε εt εnt εnt= S∇u nt εε=nt + εt
Boundary equations:
uu= * unt+= uu t * Γ=: uu** unt =− u ut uu=nt + u t u
90 2nd Thermal Analogy
ANALOGOUS PROBLEM – A linear elastic problem can be solved as:
∇σ⋅+ρ0b0 = Equilibrium Equation εσnt = C-1 : Inverse constitutive Equation ε∇nt= Su nt Geometric Equation
Γ=−nt * t u : u uu * Boundary Conditions in space Γσ : σ ⋅=nt
91 2nd Thermal Analogy
The actions and responses of the ANALOGOUS PROBLEM are:
not not ()II ()II ACTIONS = A ()x,t RESPONSES = R ()x,t
nt bx(),t ux(),t Elastic model nt * ε ()x,t tx() ,t EDPs+BCs σ ()x,t unt = ux* ()(),,tt − uxt
ORIGINAL PROBLEM (I) ANALOGOUS PROBLEM (II)
92 2nd Thermal Analogy
If the actions and responses of the original and analogous problems are compared: ACTIONS bb 0 ∗∗tt def ()I ()II u uu− u ()III AA(,)xxtt−=−== (,) ** A tt 0 ∆∆θθ0
RESPONSES uunt u t ut def ()I ()II ()III RR(,)xxtt− (,) =−εε nt = ε t =∆= αθ1 R σσ 00
Responses are proven to be the solution of a thermo-elastic problem under actions
93 2nd Thermal Analogy
THERMOELASTIC ANALOGOUS THERMOELASTIC ORIGINAL ELASTIC TRIVIAL PROBLEM (I) PROBLEM (II) PROBLEM (III)
bx(),t b b0 = * ∗ t ∗ t ()I tx(),t ()II uu= − u ()III u = ux(),t x,t * x,t x,t A () ux(),t A () t* A () t0* = ∆θ ()x,t ∆=θ 0 ∆θ ()x,t
ux(),t uxnt (),t u= uxt (),t ()I ()II nt ε()x,t ε ()x,t ()III εε=t =()αθ ∆ 1 R ()x,t R ()x,t R ()x,t σ ()x,t σ ()x,t σ = 0
95 2nd Analogy in structural analysis
nt t uuxx= uuxx= =αθ ∆ x nt t εεxx= εxx= ε = αθ ∆ * t t Γ: uuu = − =−∆αθ Γ=: uu =∆αθ ux x xx= ux xx= 0
96 Thermal Analogies
Although the 2nd analogy is more commonly used , the 1st analogy requires less corrections.
The 2nd analogy can only be applied if the thermal strain field is integrable. It is also recommended that the integration be simple.
The particular case Homogeneous material: αα()x =const . = Lineal thermal increment: ∆=θ ax + by + cz + d is of special interest because the thermal strains are: ε t =α∆θ 1 =linear polinomial and trivially satisfy the compatibility conditions (involving second order derivatives).
97 Thermal Analogies
In the particular case Homogeneous material: αα()x =const . = Constant thermal increment: ∆=θθ()x const . =∆ the integration of the strain field has a trivial solution because the thermal strains are constant ε= t = ∆ θα 1 const . , therefore: rigid body motion (can be chosen arbitrarily: t ∗∗ ux(),t =αθ ∆ x +Ω ⋅+ xc at convenience) The thermal displacement is: uxt (),t =αθ ∆ x xu+t =+∆ xαθ x =+∆()1 αθ x
HOMOTHECY (free thermal expansion)
98 6.7 Superposition Principle
Ch.6. Linear Elasticity
99 Linear Thermoelastic Problem
The governing eqns. of the isotropic linear thermoelastic problem are:
∇σ⋅+()()x,,ttρ0 bx = 0 Equilibrium Equation
σε()()x,,tt=C :x −∆βθ1 Constitutive Equation 1 ε()()x,,tt= ∇S ux =( u ⊗+⊗∇∇ u) Geometric Equation 2
* Γ=u : uu * Boundary Conditions in space Γ=⋅σ : tnσ
ux(),0 = 0 Initial Conditions ux (),0 = v0
100 Linear Thermoelastic Problem
Consider two possible systems of actions:
()1 2 bx(),t bx() (),t ()1 2 tx* (),t tx*() (),t ()1 ()2 ()1 2 A ()x,t ≡ ux* (),t A ()x,t ≡ ux*() (),t ()1 2 ∆θ ()x,t ∆θ () ()x,t ()1 ()2 vx0 () vx0 ()
and their responses :
1 ()2 ux() (),t ux(),t ()1 1 ()2 ()2 R ()x,t ≡ ε() ()x,t R ()x,t ≡ ε ()x,t 1 ()2 σ() ()x,t σ ()x,t
101 Superposition Principle
()()()()()3 11 2 2 The solution to the system of actions AAA = λλ + where ()1 ()2 ()()()()()3 11 2 2 λ and λ are two given scalar values, is RRR = λλ + .
The response to the lineal thermoelastic problem caused by two or more groups of actions is the lineal combination of the responses caused by each action individually.
This can be proven by simple substitution of the linear combination of actions and responses into the governing equations and boundary conditions.
When dealing with non-linear problems (plasticity, finite deformations, etc), this principle is no longer valid.
102 6.8 Hooke’s Law in Voigt Notation
Ch.6. Linear Elasticity
103 Stress and Strain Vectors
Taking into account the symmetry of the stress and strain tensors,
these can be written in vector form: ε x 11 ε γγ ε y x xy xz εε ε 22 def x xy xz ε z not. 11 6 ε = ε εε= γ ε γ {}ε = ∈ R xy y yz xy y yz γ 22 xy εε ε xz yz z γ 11 xz γxz γε yz z 22 γ yz REMARK VOIGT σ The double contraction () σ:ε is NOTATION x σ transformed into the scalar (dot) y στx xy τ xz product () {}{} σε ⋅ : def σ z 6 σ ≡ τxy στ y yz {}σ = ∈ R vectors τ xy ττσxz yz z σ:ε={}{} σ ⋅ ε σij ε ij= σε i i τ xz 2nd order τ tensors yz
104 Inverse Constitutive Equation
The inverse constitutive equation is rewritten:
νν1+ t ε=−Tr () σσ11 + +∆αθ {}{}{}ε=⋅+Cˆ −1 σε EE
t Where Cˆ − 1 is an elastic constants inverse matrix and {} ε is a thermal strain vector: αθ∆ 00 1 −−νν εt ≡∆αθ 0 00 00 EE E 00αθ∆ −−νν1 0 00 EE E −−νν1 0 00 E EE Cˆ −1 = αθ∆ 1 0 0 0 00 αθ∆ G αθ∆ 1 t 00 0 0 0 {}ε = G 0 1 00 0 00 0 G 0
105 Hooke’s Law
By inverting the inverse constitutive equation, Hooke’s Law in terms of the stress and strain vectors is obtained:
t {}{}{}σ=⋅−Cˆ () εε νν 1 000 −−νν ˆ 11 Where C is an elastic νν 1 000 constants matrix : 11−−νν νν 1000 −ν 11−−νν ˆ E ()1 C = 12− ν ()()1+−νν 12 000 0 0 21()−ν 12− ν 000 0 0 21()−ν 12− ν 000 0 0 21()−ν
106 Chapter 6 Linear Elasticity
6.1 Hypothesis of the Linear Theory of Elasticity The linear theory of elasticity can be considered a simplification of the general theory of elasticity, but a close enough approximation for most engineering ap- plications. The simplifying hypotheses of the linear theory of elasticity are a) Infinitesimal strains. The displacements and its gradients are small, see Chapter 2. • Small displacements. The material configuration (corresponding to the reference time t0) is indistinguishable from the spatial one (correspond- ing to the present time t) and, consequently, the spatial and material co- ordinates cannot be distinguished from each other either, see Figure 6.1.
= + =⇒ ≈ x X u x X (6.1) Theory≈ 0 and Problems
Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar
Figure 6.1: Small displacements are considered in the linear theory of elasticity.
263 264 CHAPTER 6. LINEAR ELASTICITY
From (6.1), one can write ∂x F = = 1 =⇒ |F| ≈ 1 . (6.2) ∂X
Remark 6.1. As a consequence of (6.1), there is no difference be- tween the spatial and material descriptions of a property,
x = X =⇒ γ (x,t)=γ (X,t)=Γ (X,t)=Γ (x,t) , and all references to the spatial and material descriptions (in addition to any associated concepts such as local derivative, material deriva- tive, etc.) no longer make sense in infinitesimal elasticity. Likewise, the spatial Nabla differential operator (∇) is indistin- guishable from the material one ∇¯ , ∂ (•) ∂ (•) = =⇒ ∇(•)=∇¯ (•) . ∂X ∂x
Remark 6.2. As a consequence of (6.2) and the principle of conser- vation of mass, the density in the present configuration ρt ≡ ρ (X,t) coincides with the one in the reference configuration ρ0 ≡ ρ (X,0) (which is assumed to be known), ρ = ρ |F| ≈ ρ , Theory0 t and Problemst and, therefore, the density is not an unknown in linear elasticity problems. Continuum Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar • Small displacement gradients. As a consequence, no distinction is made between the material strain tensor E(X,t) and the spatial strain tensor e(x,t), which collapse into the infinitesimal strain tensor ε (x,t).
E(X,t) ≈ e(x,t)=ε (x,t) ⎧ ⎪ 1 ⎨⎪ ε = ∇Su = (u ⊗ ∇ + ∇ ⊗ u) 2 (6.3) ∂ ⎪ 1 ∂ui u j ⎩ εij = + i, j ∈{1,2,3} 2 ∂x j ∂xi
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Linear Elastic Constitutive Equation. Generalized Hooke’s Law 265
b) Existence of a neutral state. The existence of a neutral state in which the strains and stresses are null is accepted. Usually, the neutral state is under- stood to occur in the reference configuration. ε (x,t )=0 0 (6.4) σ (x,t0)=0
c) The deformation process is considered (in principle) to be isothermal1 and adiabatic.
Definition 6.1. Isothermal processes are those that take place at a temperature θ (x,t) that is constant along time,
θ (x,t) ≡ θ (x) . Adiabatic processes are those that take place without heat generation at any point and instant of time.
Heat generated inside a domain V per unit of time:
Qe = ρrdV− q · n dS = 0 ∀ΔV ⊂ V V ∂V =⇒ ρr − ∇ · q = 0 ∀x ∀t Slow deformation processes are commonly considered to be adia- batic.
Theory and Problems 6.2 Linear Elastic Constitutive Equation. Generalized Hooke’sContinuum Law Mechanics for Engineers © X. Oliver and C. Agelet de Saracibar Hooke’s law for unidimensional problems establishes the proportionality be- tween the stress, σ, and the strain, ε, by means of the constant named elastic modulus, E, σ = Eε . (6.5) In the theory of elasticity, this proportionality is generalized to the multidimen- sional case by assuming the linearity of the relation between the components of the stress tensor σ and those of the strain tensor ε in the expression known as generalized Hooke’s law,
1 The restriction to isothermal processes disappears in the linear theory of thermoelasticity, which will be addressed in Section 6.6.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 266 CHAPTER 6. LINEAR ELASTICITY
⎧ ⎨ σ (x,t)=C : ε (x,t) Generalized (6.6) Hooke’s law ⎩ σij = Cijklεkl i, j ∈{1,2,3} which constitutes the constitutive equation of a linear elastic material. The fourth-order tensor C (denoted as tensor of elastic constants) has 34 = 81 components. However, due to the symmetry of the tensors σ and ε, it must exhibit certain symmetries in relation to the exchange of its indexes. These are: C = C ijkl jikl → C = C minor symmetries ijkl ijlk (6.7)
Cijkl = Ckli j → major symmetries
Consequently, the number of different constants in the tensor of elastic constants C is reduced to 21.
Remark 6.3. An essential characteristic of the elastic behavior (which is verified in (6.5)) is that the stresses at a certain point and time, σ (x,t), depend (only) on the strains at said point and time, ε (x,t), and not on the history of previous strains.
6.2.1 Elastic Potential Consider the specific internal energy u(x,t) (internal energy per unit of mass) and the density of internalTheory energy uˆ(x and,t) (internal Problems energy per unit of volume), which related through uˆ(x,t)=ρ u(x,t) , Continuum Mechanics0 for Engineers © X. Oliver and C.uˆ Agelet de Saracibar (6.8) (ρ ) ρ du ≈ ρ du = d 0 u = duˆ , dt 0 dt dt dt where ρ0 ≈ ρ (see Remark 6.2) has been taken into account. Consider now the energy equation in its local form2, du duˆ . duˆ . ρ = = σ : d + ρ r − ∇ · q = σ : ε =⇒ = σ : ε , (6.9) 0 dt dt 0 dt
. 2 The identity d = ε, characteristic of the infinitesimal strain case, is considered here.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Linear Elastic Constitutive Equation. Generalized Hooke’s Law 267
where the adiabatic nature of the deformation process (ρ0 r − ∇ · q = 0) has been considered. Then, the global (integral) form of the energy equation in (6.9)is obtained by integrating over the material volume V.
Global form of the energy equation in linear elasticity dU d duˆ . = udVˆ = dV = σ : ε dV dt dt dt ≡ (6.10) Vt V V V with U (t)= uˆ(x,t) dV V
Here, U (t) is the internal energy of the material volume considered.
Remark 6.4. The stress power (in the case of linear elasticity) is an exact differential, . dU stress power = σ : ε dV = . V dt
Replacing now (6.6)in(6.9), i ↔ k ↔ j l duˆ not . . . . 1 . . = uˆ = σ : ε = ε σ = ε C ε = ε C ε + ε C ε = dt ij ij ij ijkl kl 2 ij ijkl kl ij ijkl kl = 1 ε. C Theoryε + ε. C andε = Problems1 ε. C ε + ε C ε. = 2 ij ijkl kl kl kli j ij 2 ij ijkl kl ij ijkl kl = 1 d ε C ε = 1 d (ε C ε) , Continuumij ijkl Mechanicskl : : for Engineers 2 dt © X. Oliver2 dt and C. Agelet de Saracibar (6.11) where the symmetries in (6.7) have been taken into account. Integrating the ex- pression obtained and imposing the condition that the density of internal energy 3 uˆ(x,t0) in the neutral state be null (for t = t0 ⇒ ε (x,t0)=0) produces the density of internal energy.
3 The conditionu ˆ(x,t0)=0 can be introduced without loss of generality.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 268 CHAPTER 6. LINEAR ELASTICITY ⎫ 1 ⎪ uˆ(x,t)= (ε (x,t) : C : ε (x,t)) + a(x) ⎬ 2 =⇒ ⎪ uˆ(x,t )=0 ∀x ⎭ 0 (6.12) 1 =⇒ ε (x,t ) : C : ε (x,t )+a(x)=a(x)=0 ∀x 2 0 0 = 0 Density of 1 1 uˆ(ε)= (ε : C : ε)= ε C ε (6.13) internal energy 2 2 ij ijkl kl
Now, (6.13) is differentiated with respect to ε, considering once more the symmetries in (6.7). ⎧ ⎪ ⎪ ∂uˆ(ε) 1 1 1 1 ⎨⎪ = C : ε + ε : C = C : ε + C : ε = C : ε = σ ∂εε 2 2 2 2 ⎪ ⎪ ∂uˆ(ε) 1 1 1 1 ⎩ = Cijklεkl + εkl Ckli j = Cijklεkl + Cijklεkl = Cijklεkl = σij ∂εij 2 2 2 2 ⎧ (6.14) ⎪ ∂ (ε) ⎨⎪ uˆ = σ =⇒ ∂εε ⎪ (6.15) ⎪ ∂uˆ(ε) ⎩ = σij i, j ∈{1,2,3} ∂εij Equation (6.15) qualifies the density of internal energyu ˆ(ε) as a potential for the stresses (which are obtained by differentiation of this potential), named elastic potential. Theory and Problems ⎧ ⎪ ⎪ 1 1 ⎨⎪ uˆ(ε)= ε : C : ε = σ : ε Continuum Mechanics2 for Engineers2 © X. Oliver and C. Agelet= σ de Saracibar Elastic potential ⎪ (6.16) ⎪ ∂ (ε) ⎩⎪ uˆ = σ ∂εε
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Isotropy. Lame’s´ Constants. Hooke’s Law for Isotropic Linear Elasticity 269
6.3 Isotropy. Lame’s´ Constants. Hooke’s Law for Isotropic Linear Elasticity
Definition 6.2. An isotropic material is that which has the same properties in all directions.
The elastic properties of a linear elastic material are contained in the tensor of elastic constants C defined in (6.6) and (6.7). Consequently, the components of this tensor must be independent of the orientation of the Cartesian system used4.
Consider, for example, the systems {x1,x2,x3} and {x1 ,x2 ,x3 } in Figure 6.2, the constitutive equation for these two systems is written as
{x1,x2,x3} =⇒ [σ ]=[C] : [ε] (6.17)
{x1 ,x2 ,x3 } =⇒ [σ ] =[C] : [ε] and, for the case of an isotropic material, the components of C in both sys- tems must be the same ( [C]=[C] ). Therefore, the aforementioned definition of isotropy, which has a physical character, translates into the isotropic charac- ter, in the mathematical sense, of the tensor of elastic constants C. ⎧ ⎪ ⎨⎪C = λ1 ⊗ 1 + 2μI Tensor of elastic C = λδ δ + μ δ δ + δ δ (6.18) constants ⎪ ijkl ij kl ik jl il jk ⎩⎪Theory and Problems i, j,k,l ∈{1,2,3} Continuum Mechanics for Engineers Here, λ and μ are known© X. as OliverLame’s´ constantsand C. Agelet, whichde characterize Saracibar the elastic behavior of the material and must be obtained experimentally.
Remark 6.5. The isotropy condition reduces the number of elastic constants of the material from 21 to 2.
4 A tensor is isotropic if it maintains its components in any Cartesian coordinate system. The most general expression of a fourth-order isotropic tensor is C = λ1⊗1+2μI , ∀λ, μ. Here, the fourth-order symmetric (isotropic) unit tensor I is defined by means of its components as [ ] = δ δ + δ δ / I ijkl ik jl il jk 2.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 270 CHAPTER 6. LINEAR ELASTICITY
Figure 6.2: Representation of the Cartesian systems {x1,x2,x3} and {x1 ,x2 ,x3 }.
Introducing (6.18)in(6.6) results in the isotropic linear elastic constitutive equation, 1 1 σ = C ε = λδ δ ε +2μ δ δ ε + δ δ ε . (6.19) ij ijkl kl ij kl kl 2 ik jl kl 2 il jk kl ε ε ε = ε ll ij ji ij εij ⎧ ⎨ Constitutive eqn. for a σ = λ Tr (ε)1 + 2μεε linear elastic material. ⎩ (6.20) Hooke’s law. σij = λδijεll + 2μεij i, j ∈{1,2,3}
6.3.1 Inversion of Hooke’s Law. Young’s Modulus. Poisson’s Ratio The constitutive equation (6.20) provides the stresses in terms of the strains. To obtain its inverse expression,Theory the following and procedure Problems is followed. a) The trace of (6.20) is obtained, ⎫ ⎪ TrContinuum(σ )=λ Tr (ε)Tr (1 Mechanics)+2μ Tr (ε)=(3λ for+ 2μ Engineers)Tr (ε) ⎪ © X. Oliver and C. Agelet de Saracibar⎬⎪ 3 =⇒ ⎪ ( = )=⇒ σ = λε δ + με =( λ + μ)ε ⎪ i j ii ll ii 2 ii 3 2 ll ⎭⎪ (6.21) 3 1 =⇒ Tr (ε)= Tr (σ ) . (3λ + 2μ) b) ε is isolated from (6.20) and introduced in (6.21), 1 1 λ 1 ε = − λ Tr (ε)1 + σ = − Tr (σ )1 + σ . (6.22) 2μ 2μ 2μ (3λ + 2μ) 2μ
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Isotropy. Lame’s´ Constants. Hooke’s Law for Isotropic Linear Elasticity 271
The new elastic properties E (Young’s modulus) and ν (Poisson’s ratio) are de- fined as follows. ⎫ ⎪ Young’s modulus or μ (3λ + 2μ) ⎪ E = ⎬ tensile (elastic) modulus λ + μ =⇒ ⎪ λ ⎪ Poisson’s ratio ν = ⎭ 2(λ + μ) ⎧ (6.23) ⎪ ⎪ ν ⎨⎪ λ = E ( + ν)( − ν) =⇒ 1 1 2 ⎪ ⎪ E ⎩ μ = = G shear (elastic) modulus 2(1 + ν)
Equation (6.22) can be expressed in terms of E and ν, resulting in the inverse Hooke’s law. ⎧ ⎪ ⎪ ν 1 + ν ⎪ ε = − Tr (σ )1 + σ Inverse constitutive ⎨ E E ν + ν (6.24) equation for an isotropic ⎪ ε = − σ δ + 1 σ ⎪ ij ll ij ij linear elastic material ⎪ E E ⎩ i, j ∈{1,2,3}
Finally, (6.24) is rewritten, using engineering notation for the components of the strain and stress tensors. Theory and Problems 1 1 εx = (σx − ν (σy + σz)) γxy = τxy ContinuumE Mechanics for EngineersG ε = ©1 ( X.σ − Oliverν (σ + andσ )) C. Ageletγ = 1 deτ Saracibar (6.25) y E y x z xz G xz ε = 1 (σ − ν (σ + σ )) γ = 1 τ z E z x y yz G yz
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 272 CHAPTER 6. LINEAR ELASTICITY
Example 6.1 – Consider an uniaxial tensile test of a rectangular cuboid composed of an isotropic linear elastic material with Young’s modulus E and shear modulus G, such that its uniform stress state results in
σx = 0 and σy = σz = τxy = τxz = τyz = 0 . Obtain the strains in engineering notation.
Solution
From (6.25) one⎧ obtains ⎧ ⎪ σ ⎪ τxy ⎪ ε = x ⎪ γ = = 0 ⎨⎪ x ⎨⎪ xy E σ τG σ = σ = =⇒ ε = −ν x τ = τ = τ = =⇒ γ = xz = y z 0 ⎪ y xy xz yz 0 ⎪ xz 0 ⎪ E ⎪ G ⎩⎪ σx ⎩⎪ τyz ε = −ν γ = = 0 z E yz G Therefore, due to these strains, the rectangular cuboid subjected to an uni- axial tensile test, shown in the figure below, stretches in the x-direction and contracts in the y- and z-directions.
Theory and Problems 6.4 Hooke’s Law in Spherical and Deviatoric Components ConsiderContinuum the decomposition Mechanics of the stress tensor forσ and Engineers the deformation tensor ε in their spherical and deviatoric© X. Oliver parts, and C. Agelet de Saracibar
1 σ = Tr (σ )1 + σ = σ 1 + σ , (6.26) 3 m
1 1 ε = Tr (ε)1 + ε = e1 + ε . (6.27) 3 3
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Hooke’s Law in Spherical and Deviatoric Components 273
The volumetric strain e = Tr (ε) is obtained by computing the trace of (6.24).
ν 1 + ν 1 − 2ν e = Tr (ε)=− Tr (σ )Tr (1)+ Tr (σ )= Tr (σ ) = E E E 3 3σm (6.28) ( − ν) = 3 1 2 σ E m ⎧ ⎪ ⎪ E ⎨ σm = e = Ke =⇒ 3(1 − 2ν) ⎪ (6.29) ⎪ def 2 E ⎩ K = λ + μ = = bulk modulus 3 3(1 − 2ν) Introducing (6.26), (6.27) and (6.29)in(6.24), results in
ν 1 + ν 1 − 2ν 1 + ν ε = − 3σ 1 + (σ 1 + σ )= σ 1 + σ = E m E m E m E E e 3(1 − 2ν) 1 1 + ν 1 1 1 + ν (6.30) = e1 + σ =⇒ ε = e1 + ε = e1 + σ 3 E 3 3 E
+ ν =⇒ ε = 1 σ = 1 σ = 1 σ . E 2μ 2G Equations (6.29) and (6.30) relate the spherical part (characterized by the mean σ σ ε stress m and the volumetricTheory strain e) and and the Problems deviatoric part ( and ) of the stress and strain tensors as follows.
Continuumσ = Mechanics for Engineers m Ke © X. Oliver and C.Spherical Agelet de part Saracibar (6.31) σ = 2Gε Deviatoric part σ ij = 2Gε ij i, j ∈{1,2,3}
Remark 6.6. Note the proportionality between σm and e as well as
between σ ij and ε ij (component to component), see Figure 6.3.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 274 CHAPTER 6. LINEAR ELASTICITY
Figure 6.3: Hooke’s law in spherical and deviatoric components.
6.5 Limits in the Values of the Elastic Properties Thermodynamic considerations allow proving that the tensor of elastic constants C is positive-definite5, and, thus, ε : C : ε > 0 ∀ε = 0 . (6.32)
Remark 6.7. As a consequence of (6.32), the elastic potential is al- ways null or positive, 1 uˆ(ε)= ε : C : ε ≥ 0 . 2
Remark 6.8. The elastic potential has a minimum at the neutral state, that is, for ε = 0 (see Figure 6.4). In effect, from (6.15), 1 Theory∂uˆ(ε and) Problems∂ 2uˆ(ε) uˆ(ε)= ε : C : ε , σ = = C : ε and = C . 2 ∂εε ∂εε ⊗ ∂εε ε = Then,Continuum for 0, Mechanics for Engineers ∂uˆ(ε) © X. Oliver( andε) C. Agelet de Saracibar = 0 =⇒ uˆ has an extreme ∂εε (maximum-minimum) at ε = 0. ε= 0 ∂ 2 (ε) uˆ = C =⇒ ∂εε ⊗ ∂εε The extreme is a minimum. ε=0 positive- definite
5 A fourth-order symmetric tensor A is defined positive-definite if for all second-order tensor x = 0 the expression x : A : x = xij Aijkl xkl > 0 is satisfied and, in addition, x : A : x = 0 ⇔ x = 0.
X. Oliver and C. Agelet de Saracibar Continuum Mechanics for Engineers.Theory and Problems doi:10.13140/RG.2.2.25821.20961 Limits in the Values of the Elastic Properties 275
Figure 6.4: Elastic potential.
Consider the expression of the elastic potential (6.16) and the constitutive equation (6.20), then,
1 1 1 uˆ(ε)= ε : C : ε = σ : ε = λ Tr (ε)1 + 2μεε : ε = 2 2 2 1 1 (6.33) = λ Tr (ε) 1 : ε +μεε : ε = λ Tr2 (ε)+μεε : ε . 2 2 Tr (ε)
Expression (6.33) can also be written in terms of the spherical and deviatoric components of strain6,