Lecture 1 NONLINEAR ELASTICITY

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Transcription:

Lecture 1 NONLINEAR ELASTICITY

Soft-Matter Engineering: Mechanics, Design, & Modeling Mechanics Rigid/Hard Systems bending or torsion (but not stretching) small strains (~0.1% metals; ~1% plastics) linearized stress-strain response; Linear Elasticity Soft Systems stretch (~10-100% strain) large deflections (including self-contact) nonlinear stress-strain response; Finite Elasticity Design Actuators/Transducers pneumatics, dielectrics, shape memory, IPMCs, bio-hybrid Circuits/Sensors flex circuits, conductive fabrics, wavy circuits, soft microfluidics Modeling derived from governing equations of nonlinear elasticity Pneumatics elastic shell theory Dielectrics elastic membrane theory Shape Memory elastic rod theory

THEORY OF ELASTICITY (Displacement Formulation) Displacement of points in an elastic body: u = u(x) X B 0 Balance Laws: E σ = 0 X B 0 (internal) σ n = t X B 0 (boundary) Strains ~ gradient of displacements u ε(x) Strain Tensor ~ rotation + stretch ~ stretch + rotation Constitutive Law: Relate strains (or stretch) with stress: ε σ(x) Stess Tensor

THEORY OF ELASTICITY Choice of materials dictates the limits of stress and strain as well as the constitutive law. For small strains, the constitutive law can be linearized: for linear elastic, homogenous, isotropic solids, use Hooke s Law w/ Hooke s Law, elasticity can be represented by only two values: - Young s modulus (E) and Poisson s ratio (ν) - Shear modulus (µ) and Bulk modulus (K) - Lame constants λ and µ For large strains, the constitutive relationships are typically nonlinear and require additional elastic coefficients. In most cases, the constitutive law and its coefficients must be determined experimentally with materials testing equipment.

Uniaxial Loading Reference A 0 Current A B 0 B F L 0 L = L 0 + ΔL, Strain: ε = ΔL L 0 Stretch: λ = L L 0 =1+ε Incompressibility: V = V 0!AL = A 0 L 0!A = A 0 /λ, Recall the definition for engineering/nominal stress: σ e = F A 0 This is valid for small deformations but significantly underestimates the true ( Cauchy ) stress for moderate deformations: σ = F A = λσ e

Uniaxial Loading For uniaxial loading with small strains, σ e and ε are related by Hooke s Law: F σ e = Eε F = EA 0 ( λ 1) EA 0 λ What happens if we replace σ e with σ? 1 EA 0 F EA 0 λ σ = Eε F = EA 0 1 1 λ lim λ F = EA 0 1 These represent two distinct constitutive models, neither of which is realistic for elastomers.

Rubber Mechanics Vulcanized natural rubber macromolecule: ~5000 isoprene units (C-C bonding) cis-1,4-polyisoprene molecular spaghetti Sulfer cross-links every ~100 units (2%) Between the cross-links, each isoprene unit is a freely rotating link If monomer units are free to rotate, why is there any resistance to deformation? For any load and configuration, we can calculate the Gibbs free energy Π of the rubber system. Changes in Π are subject to the 1 st Law of Thermodynamics: δπ = δ(u Q) 1 st Law: δu = δq! δπ = 0 U = Γ TS = Helmholtz Free Energy Γ = internal chemical bonding energy S = system entropy δq = B t δuds = applied mechanical work

Gibbs Free Energy for a 1-DOF System Π, Solutions δπ = 0, α, α 1, α 2, α 3, A B L = L 0 + ΔL, δq = FδL δq δu = 0 F = du dl At static equilibrium, the system free (potential) energy must be stationary w.r.t. shape/ configuration.

Principle of Stationary Potential At static equilibrium, the total potential energy Π = Π(u) must be stationary w.r.t. infinitesimally small changes in u. If the deformation can be parameterized so that Π = Π(α 1, α 2,, α n ), then this implies the Rayleigh-Ritz criterion for equilibrium: Π = Π =... = Π = 0 α 1 α 2 α n Consider a 1-DOF system, i.e. Π = Π(α) e.g. uniaxial loading: α = λ, inflating sphere: α = R In this case, α is the solution to the equation dπ/dα = 0

2 nd Law of Thermodynamics 2 nd Law of Thermodynamics: ΔS tot = ΔS + ΔS e 0 S and S e are the entropy of the system and surrounding (external), respectively ΔS e = Ω/T, where Ω is the heat transferred from the surroundings For fixed surface tractions and fixed temperature it follows (by definition) that ΔΠ = Ω TΔS This implies ΔS tot = ΔS Ω/T= ΔΠ/T, i.e. total entropy decreases with increasing Gibbs free energy (potential energy) Now suppose that is locally Π maximized any perturbation will cause Π to decrease and universal entropy to increase. After perturbation, will the system return to its original state? It can t returning to the original state requires a decrease in S tot, hence violating the 2 nd Law. Therefore such equilibrium states are unstable. In the absence of external tractions (e.g. fixed kinematic constraints/ displacements), a separate analysis is performed using Helmholtz (U) instead of Gibbs (Π) free energy.

Principle of Minimum Potential Π, Solutions that maximize Π are unstable (i.e. α 2* ) α 1, α 2, α 3, α, Solutions that minimize Π are stable (i.e. α 1 * and α 3* ) Consider the solution α = α 2 * Changing α results in a decrease in Gibbs Free Energy For fixed surface tractions, this corresponds to an increase in universal Entropy S tot This implies that returning to the extremizing value α = α 2 * will decrease S tot Therefore, α = α 2 * is a solution that violates the 2 nd Law of Thermodynamics In contrast, for α = α 1 * or α = α 3 * Changing α increases Π and hence reduces total entropy The system will spontaneously return to the equilibrium state in order to increase universal Entropy.

Polymers Semi-Crystaline e.g. HDPE Relatively rigid Completely Amorphous e.g. Vulcanized Rubber Soft & Stretchable Crystalline, semi-crystalline, and glassy materials deform through lengthening/shortening of interatomic bonds!change in internal energy (Γ) Elastomers deform through changes in macromolecular configuration ( morphology )!change in entropy (S) Partial straightening is an ordering processes that decreases entropy and thus requires mechanical work input. In the case of uniaxial loading, recall that F = du/dl. F T ds Noting that U = Γ TS and δγ 0, it follows that dl T What is the entropy of rubber and how does it scale with stretch?

Entropy of of Rubber Ref: Entropy and Rubber Elasticity by Leonard Nash J. Chemical Education, 56 (6) 363-368 (1979) The configurational entropy is defined as S = k ln(m), where k = Boltzmann s constant M = discrete number of configurations that the macromolecular chains can adopt to fill a prescribed volume. Simplifying assumptions: N chains each with n links of uniform length l This ignores the stochasticity of chain lengths and cross-linking For random shapes, there exists a root-meansquare average end-to-end length r u ~ ln 1/2 For an end-to-end vector R = xi + yj + zk, M = M N 0 exp 3N x2 + y 2 + z 2 2 2r u ( ) Here, M0 is the number of possible configurations for a single chain when R = 0 (i.e. chain loops around)

Entropy of of Rubber S = Nkln M 0 3Nk 2r u 2 x 2 + y 2 + z 2 ( ) Now consider the following deformation: x = λ x x 0 y = λ y y 0 z = λ z z 0 where x 0 2 = y 0 2 = z 0 2 = r u2 /3, and define S u as the initial entropy (i.e. prior to deformation). ( ) ΔS = S S u = Nk 2 λ 2 + λ 2 x y + λ 2 z 3 For incompressible deformation and uniaxial loading, λ x = λ, λ y = λ z = λ -1/2 ΔS = Nk 2 λ2 + 1 λ 3 ds dλ T = Nk λ 1 λ 2

Entropy of Rubber F = T ds dl T = T ds dλ T dλ dl Noting that L = λl 0 and dλ/dl = 1/L 0, F = NkT λ 1 L 0 λ 2 Expressing this in terms of a nominal engineering stress σ e = F/A 0, and noting that A 0 L 0 = V 0 = V, σ e = C 1 λ 1 where C λ 2 1 = NkT/V

BALANCING FORCES Another difference between linear and nonlinear/finite elasticity is the configuration or placement in which we balance forces: REFERENCE A 0 CURRENT A B 0 B F L 0 L = L 0 + ΔL, At static equilibrium, the forces acting on the body must balance. However, for the same forces, we will calculate different stresses (and thus different strains/stretches) depending on what placement we are in.

EXAMPLE L 0, A 0, θ 0, 2P L, 2P θ, F = EA 0 3 λ 1 λ 2 P = Fcosθ 0 = EA 0 3 λ 1 λ 2 cosθ 0 P = Fcosθ L 0 sinθ 0 = Lsinθ cosθ = 1 1 ( λ 1 2 cos2 θ 0 ) We must balance forces in the Current Placement!!! P = EA 0 3 λ 1 λ 2 1 1 λ 1 2 cos2 θ 0 ( )

NEO-HOOKEAN SOLID For a Neo-Hookean Solid, recall the expression for the change in Helmholtz free energy: ΔU = TΔS = NkT 2 ( λ 2 x + λ 2 y + λ 2 z 3) This implies that strain energy density has the form W = C ( 1 λ 2 1 + λ 2 2 + λ 2 3 3) σ i = 2C 1 λ i 2 p Example 1: Uniaxial Loading σ 1 = σ λλ 2 2 =1 σ 2 = σ 3 = 0 λ 2 = 1 λ 1 = λ λ λ 2 = λ 3 σ 2 = 0 2C 1 λ p p = 2C 1 λ σ = 2C 1 λ 2 p σ = 2C 1 λ 2 1 λ

NEO-HOOKEAN SOLID Example 2: Equibiaxial Loading σ 1 = σ 2 = σ λ 1 = λ 2 = λ σ 3 = 0 λ 2 λ 3 =1 λ 3 = 1 λ 2 σ 3 = 0 2C 1 λ p p = 2C 1 4 λ 4 σ = 2C 1 λ 2 p σ = 2C 1 λ 2 1 λ 4 Example 3: Sphere Inflation R 0 R p E 3 t 0 E 1 E 2 l 0 l 0 l t l assume equibiaxial loading: R >> t! σ 1 = σ 2 =: σ >> σ 2 ~ p

BALLOON INFLATION CONT. λ 1 = λ 2 = λ R λ R 3 = 1 = 1 0 λ 1 λ 2 λ 2 W = C 1 2λ 2 + 1 λ 3 4 Π= WV U p Π= 4πR 2 0 t 0 C 1 2 R R 0 V = V 0 4πR 2 0 t 0 U p = pv e 2 + R 0 R At equilibrium, Π must be minimized w.r.t. R. This implies dπ/dr = 0: 4 3 4 3 πr 3 p V e = 4 3 πr 3 dπ dr = 4πR 2 4R t 0 0 C 1 2 R 4R 4 R 0 0 0 R 5 R 4 4πR 2 p 0

BALLOON INFLATION CONT. Solve for p: 0.45 p = 2t E R 0 0 3R 0 R R 7 0 R 7 0.4 0.35 0.3 pr 0 /Et 0 0.25 0.2 0.15 0.1 0.05 0 1 1.5 2 2.5 3 3.5 4 4.5 5 R/R 0

WHAT ABOUT SHEAR?! In addition to stretch, materials typically undergo shear. However, for any elastic deformation, there is always an orientation where shear disappears. Consider an elastic body with reference placement B 0. During deformation, points X B 0 get mapped to a final position x = χ(x) = X + u, where x B are the final positions B is the current placement u = u(x) is the displacement field The strain tensor ε is calculated from the gradient of x: ε = ε(f) F = χ= Deformation Gradient Both ε and F are 2 nd order tensors (~3x3 matrices)

WHAT ABOUT SHEAR?! According to the Polar Decomposition Theory, F can be represented as F = RU, where R is a rotation tensor and U is a tensor with only diagonal elements: χ! Stretch (U)! Rotation (R)! λ 1! λ 2! E 2 E 1 " $ U ~ $ $ # λ 1 0 0 0 λ 2 0 0 0 λ 3 % ' ' ' & For any deformation, there exist principal directions (p 1, p 2, p 3 ) along which the material undergoes only pure axial stretch.

EXAMPLE Consider a cylinder under pure torsion. Just because it doesn t change length or diameter, it is incorrect that it contains zero stretch: E 2 χ! E 1 shear w.r.t. (E 1, E 2 ) χ! λ 2! λ 1! stretch w.r.t. (p 1, p 2 )

GENERAL LOADING CONDITIONS In general, during virtual displacement, prescribed surface tractions t perform mechanical work on the elastic body: δq = B t δuds As before, this work must all be stored as elastic strain energy, i.e. δq δu δu δq = 0 Now consider the following loading conditions: Concentrated Traction = Point Load Concentrated Traction Couple = Moment Enclosed Air Pressure

Concentrated Traction = Point Load: B t δuds = F δu Concentrated Traction Couple = Moment: B t δuds = Mδθ Enclosed Air Pressure: t δuds = pn δuds = pδv e B B!!

The potential energy Π of an elastic body represents the total energy associated with both the internal elastic strain energy w and the mechanical work Q of external tractions t: F M t δu = δq δwdv = t uds+ F δu + Mδθ + pδv e B o Π =!! B 0 B ') + ) δ( WdV t uds F u Mθ pv e, *) B -) = 0 B o δπ = 0 WdV t uds F u Mθ B pv e

The condition δπ = 0 implies that the potential energy must be stationary at static equilibrium. Since the functional Π = Π(u) is smooth and continuous, this condition is satisfied when minimized w.r.t. kinematically admissable deformations u!k. Here, K represents the space of all possible functions u = u(x) that satisfy the prescribed kinematic boundary conditions. If the deformation can be parameterized so that Π = Π(α 1, α 2,, α n ) is a function of scalars instead of a functional, then the condition δπ = 0 corresponds to (Rayleigh-Ritz criterion) Π α 1 = Π α 2 =... = Π α n = 0