Nonlinear elasticity and gels

Similar documents
Analysis and numerics of the mechanics of gels

arxiv: v2 [math.ap] 16 Oct 2012

LONG-TIME EXISTENCE OF CLASSICAL SOLUTIONS TO A 1-D SWELLING GEL

Fundamentals of Fluid Dynamics: Elementary Viscous Flow

Downloaded 04/01/13 to Redistribution subject to SIAM license or copyright; see

You may not start to read the questions printed on the subsequent pages until instructed to do so by the Invigilator.

Large Deformation of Hydrogels Coupled with Solvent Diffusion Rui Huang

Relaxation methods and finite element schemes for the equations of visco-elastodynamics. Chiara Simeoni

On pore fluid pressure and effective solid stress in the mixture theory of porous media

A Thermomechanical Model of Gels

Existence of minimizers for the pure displacement problem in nonlinear elasticity

Flow and Transport. c(s, t)s ds,

Constitutive models. Constitutive model: determines P in terms of deformation

ON LIQUID CRYSTAL FLOWS WITH FREE-SLIP BOUNDARY CONDITIONS. Chun Liu and Jie Shen

Analysis of a non-isothermal model for nematic liquid crystals

Formulation of the problem

Smoluchowski Navier-Stokes Systems

Continuum Mechanics Fundamentals

FINITE ELEMENT APPROXIMATION OF STOKES-LIKE SYSTEMS WITH IMPLICIT CONSTITUTIVE RELATION

Functional Grading of Rubber-Elastic Materials: From Chemistry to Mechanics

TWO-DIMENSIONAL MAGMA FLOW *

Chapter 1. Continuum mechanics review. 1.1 Definitions and nomenclature

An introduction to implicit constitutive theory to describe the response of bodies

Linear Constitutive Relations in Isotropic Finite Viscoelasticity

Received: 21 January 2003 Accepted: 13 March 2003 Published: 25 February 2004

in this web service Cambridge University Press

On the Rank 1 Convexity of Stored Energy Functions of Physically Linear Stress-Strain Relations

A dynamic model of polyelectrolyte gels. A dissertation submitted to the faculty of the graduate school of the university of minnesota by.

Non-linear Wave Propagation and Non-Equilibrium Thermodynamics - Part 3

Nonlinear Equations for Finite-Amplitude Wave Propagation in Fiber-Reinforced Hyperelastic Media

ENERGY-MINIMIZING INCOMPRESSIBLE NEMATIC ELASTOMERS

Nonlinear stability of steady flow of Giesekus viscoelastic fluid

A review of Continuum Thermodynamics

The inviscid limit to a contact discontinuity for the compressible Navier-Stokes-Fourier system using the relative entropy method

Author(s) Huang, Feimin; Matsumura, Akitaka; Citation Osaka Journal of Mathematics. 41(1)

Second-gradient theory : application to Cahn-Hilliard fluids

UNSTEADY POISEUILLE FLOW OF SECOND GRADE FLUID IN A TUBE OF ELLIPTICAL CROSS SECTION

Euler Equations: local existence

Existence of global weak solutions to implicitly constituted kinetic models of incompressible homogeneous dilute polymers

MHA042 - Material mechanics: Duggafrågor

Stability of Thick Spherical Shells

Linearized theory of elasticity

A monolithic fluid structure interaction solver Verification and Validation Application: venous valve motion

Fundamentals of Linear Elasticity

Getting started: CFD notation

LOCAL WELL-POSEDNESS FOR AN ERICKSEN-LESLIE S PARABOLIC-HYPERBOLIC COMPRESSIBLE NON-ISOTHERMAL MODEL FOR LIQUID CRYSTALS

On the characterization of drilling rotation in the 6 parameter resultant shell theory

EPSRC Centre for Doctoral Training in Industrially Focused Mathematical Modelling

Can constitutive relations be represented by non-local equations?

Role of thermodynamics in modeling the behavior of complex solids

Existence and uniqueness of the weak solution for a contact problem

Linearized Theory: Sound Waves

Phase Transition Dynamics in Polymer Gels

OPTIMAL CONTROL AND STRANGE TERM FOR A STOKES PROBLEM IN PERFORATED DOMAINS

Causal Dissipation for the Relativistic Fluid Dynamics of Ideal Gases

This introductory chapter presents some basic concepts of continuum mechanics, symbols and notations for future reference.

Archimedes Center for Modeling, Analysis & Computation. Singular solutions in elastodynamics

Simulation of Thermomechanical Couplings of Viscoelastic Materials

Weak Convergence Methods for Energy Minimization

Juan E. Santos a,b,c, Gabriela B. Savioli a and Robiel Martínez Corredor c a

Self-folding thermo-magnetically responsive softmicrogrippers

A hierarchy of higher order and higher grade continua Application to the plasticity and fracture of metallic foams

New sufficient conditions for the Hadamard stability of a Mooney-Rivlin elastic solid in uniaxial deformation

THE L 2 -HODGE THEORY AND REPRESENTATION ON R n

Level Set Tumor Growth Model

Similarity Approach to the Problem of Second Grade Fluid Flows over a Stretching Sheet

Iranian Journal of Mathematical Sciences and Informatics Vol.2, No.2 (2007), pp 1-16

Spectral theory for magnetic Schrödinger operators and applicatio. (after Bauman-Calderer-Liu-Phillips, Pan, Helffer-Pan)

Variable Exponents Spaces and Their Applications to Fluid Dynamics

MHD Free convection flow of couple stress fluid in a vertical porous layer

V (r,t) = i ˆ u( x, y,z,t) + ˆ j v( x, y,z,t) + k ˆ w( x, y, z,t)

Approximation of fluid-structure interaction problems with Lagrange multiplier

Existence and Uniqueness of the Weak Solution for a Contact Problem

Part IV: Numerical schemes for the phase-filed model

Generalized Newtonian Fluid Flow through a Porous Medium

Mechanical Properties of Polymer Rubber Materials Based on a New Constitutive Model

A unifying model for fluid flow and elastic solid deformation: a novel approach for fluid-structure interaction and wave propagation

KINEMATICS OF CONTINUA

Unsteady Flow of a Newtonian Fluid in a Contracting and Expanding Pipe

Measure-valued - strong uniqueness for hyperbolic systems

LECTURE # 0 BASIC NOTATIONS AND CONCEPTS IN THE THEORY OF PARTIAL DIFFERENTIAL EQUATIONS (PDES)

Introduction to Continuum Mechanics

Applications of parabolized stability equation for predicting transition position in boundary layers

The Non-Linear Field Theories of Mechanics

Course Syllabus: Continuum Mechanics - ME 212A

Fluid Dynamics Exercises and questions for the course

International Journal of Pure and Applied Mathematics Volume 58 No ,

Numerical Simulations on Two Nonlinear Biharmonic Evolution Equations

Lecture No 1 Introduction to Diffusion equations The heat equat

Chapter 2 CONTINUUM MECHANICS PROBLEMS

Local invertibility in Sobolev spaces. Carlos Mora-Corral

The Multiple Solutions of Laminar Flow in a. Uniformly Porous Channel with Suction/Injection

INDEX 363. Cartesian coordinates 19,20,42, 67, 83 Cartesian tensors 84, 87, 226

EXISTENCE AND REGULARITY OF SOLUTIONS FOR STOKES SYSTEMS WITH NON-SMOOTH BOUNDARY DATA IN A POLYHEDRON

In this section, thermoelasticity is considered. By definition, the constitutive relations for Gradθ. This general case

ELASTOPLASTICITY THEORY by V. A. Lubarda

Transient Interfacial Phenomena in Miscible Polymer Systems (TIPMPS)

Large bending deformations of pressurized curved tubes

Elements of Continuum Elasticity. David M. Parks Mechanics and Materials II February 25, 2004

4 Constitutive Theory

Transcription:

Nonlinear elasticity and gels M. Carme Calderer School of Mathematics University of Minnesota New Mexico Analysis Seminar New Mexico State University April 4-6, 2008 1 / 23

Outline Balance laws for gels Free energy: elastic plus mixing Constrained elasticity Deformable porous media Applications 2 / 23

Gels We model a gel as incompressible, immiscible mixture of polymer and solvent. immisc Component 1: polymer; Component 2: solvent Ω 0 reference configuration of the gel; X Ω 0 Ω t domain occupied by the gel at time t > 0; x Ω t 3 / 23

Gels We model a gel as incompressible, immiscible mixture of polymer and solvent. immisc Component 1: polymer; Component 2: solvent Ω 0 reference configuration of the gel; X Ω 0 Ω t domain occupied by the gel at time t > 0; x Ω t φ i v i T i i volume fraction velocity field Cauchy stress tensor friction force Φ polymer deformation map:x = Φ(X, t) F polymer deformation gradient; F = X Φ, det F > 0 φ = φ(x, t), v = v(x, t)... For a survey on gels, see [Tanaka, 1981]; theory of mixtures, [Truesdell, 1984]; model, [Calderer-Chabaud, 2008] and [Calderer-Zhang, 2008] 3 / 23

Balance laws ρ 1 t + (v 1 )ρ 1 + ρ 1 v 1 = 0 ρ 2 t + (v 2 )ρ 2 + ρ 2 v 2 = 0 ρ 1 v 1 t + ρ 1(v 1 )v 1 = T 1 + f 1 ρ 2 v 2 t + ρ 2(v )v 2 = T 2 + f 2 φ 1 + φ 2 = 1 Add up equations of balance of mass: div(φ 1 v 1 + φ 2 v 2 ) = 0 Lagrangian form of balance of mass: φ det F = φ 0 5 / 23

Free energy Elastic stored energy function (per unit reference volume) Flory-Huggins mixing energy (per unit deformed volume) µ(φ 1 )W (F ) h(φ 1, φ 2 ) 6 / 23

Free energy Elastic stored energy function (per unit reference volume) µ(φ 1 )W (F ) Flory-Huggins mixing energy (per unit deformed h(φ 1, φ 2 ) volume) Total energy: E = {µ(φ 1 )W (F ) + det F h(φ 1, φ 2 )} dx Ω 0 Ψ(F, φ) := µ(φ)w (F ) + det F h(φ, 1 φ), φ := φ 1 6 / 23

Elastic and Flory-Huggins free energies Prototype of Flory-Huggins energy: h(φ 1, φ 2 ) = aφ 1 log φ 1 + bφ 2 log φ 2 + χφ 1 φ 2 7 / 23

Elastic and Flory-Huggins free energies Prototype of Flory-Huggins energy: h(φ 1, φ 2 ) = aφ 1 log φ 1 + bφ 2 log φ 2 + χφ 1 φ 2 Isotropic elasticity: W (F ) = µ(φ)w(i 1, I 2, I 3 ) + B(φ)((det F ) k (det F ) k ), k > 0, {I 1, I 2, I 3 } principal invariants of C = F T F solid limit: lim φ 1 µ(φ) = µ 0, shear modulus; fluid limit: lim φ 0 µ(φ) = 0 0 W (F ) K F T F β, det F > 0 Example: neo-heokean elasticity W (F ) = tr (FF T ). from statistical mechanics Derived 7 / 23

Shape of free energy function with respect to χ (1) Swollen (φ 0.3) 8 / 23

Shape of free energy function with respect to χ (1) Swollen (φ 0.3) (2) Swollen and collapsed 8 / 23

Shape of free energy function with respect to χ (1) Swollen (φ 0.3) (3) Swollen and collapsed (2) Swollen and collapsed 8 / 23

Shape of free energy function with respect to χ (1) Swollen (φ 0.3) (3) Swollen and collapsed (2) Swollen and collapsed (4) Collapsed (φ 0.7) 8 / 23

Boundary conditions Let Ω = Γ 1 Γ 2, Γ 1 Γ 2 = 0 Elasticity 1. Displacement: Φ = Φ 0, on Γ 1 2. Traction: (T 1 + T 2 )ν = t 0, on Γ 2 Permeability of membrane φ 1. impermeable: ν = 0 on Ω (or part of it) 2. fully permeable: φ 2 p + Π 2 (φ 1, φ 2 ) = P 0, P 0 pressure of surrounding solvent Π 2 osmotic pressure of in-gel solvent 3. semi-permeable: P ( p + Π 2 (x, t) ) = κ(v 2 v 1 ) ν, κ > 0 permeability constant 9 / 23

Equilibrium states: convex mixing energy X 0 = {u : u u 0 + W 1,2β 0, det F > 0 a.e.} X Γ = {u : u u 0 + W 1,2β Γ, det F > 0 a.e.} W 1,2β Γ = {u W 1,2β, u = 0 on Γ Ω 0 } Minimize E = {µ(φ 1 )W (F ) + det F h(φ 1, φ 2 )} dx Ω 0 subject to φ det F = φ 0, 0 < φ 0 < 1, u X 0 X Γ 10 / 23

Equilibrium states: convex mixing energy X 0 = {u : u u 0 + W 1,2β 0, det F > 0 a.e.} X Γ = {u : u u 0 + W 1,2β Γ, det F > 0 a.e.} W 1,2β Γ = {u W 1,2β, u = 0 on Γ Ω 0 } Minimize E = {µ(φ 1 )W (F ) + det F h(φ 1, φ 2 )} dx Ω 0 subject to φ det F = φ 0, 0 < φ 0 < 1, u X 0 X Γ Theorem (Zhang-2007) Let Ω 0 be bounded and with Lipschitz boundary. Let β > 3 2. Suppose that g(s) = sh( 1 s, 1 1 s ) is a convex monotonically decreasing function of s. Assume that W (F ) is polyconvex. Then there exists at least one minimizer of E in X 0 and in X Γ. Existence theorems in nonlinear elasticity, see [Ball, 1977] and [Ciarlet, 1987] 10 / 23

Nonconvex free energy Suppose that h is nonconvex with respect to φ. 11 / 23

Nonconvex free energy Suppose that h is nonconvex with respect to φ. Modify the energy to include φ 2, and keep balance of mass constraint. X = {(u, φ) : φ W 1,2, u u 0 + W 1, 0, φ det F = φ 0, a.e 0 < φ < 1, u L < C < } Minimize (u,φ) X E = + {µ(φ 1 )W (F ) + det F h(φ 1, φ 2 } dx Ω 0 δ φ 2 dx Ω Ω δ φ 2 dx = (det( u)) 1 2 X adj ( u) 2 Ω 0 11 / 23

Existence theorem Theorem (Zhang, 2007) Let β > 0. Then for every C > 0 there exists a minimizer of the regularized energy in X. Proof: 1. u L < C implies det u 9C 3 2. There is a minimizing sequence {φ h, u h } X 3. Poincare inequality allows us to extract a subsequence (same label) u ū weak* in W 1, 4. 0 < φ h < 1, det u h > 1 and φ h > 1 9C 3 5. Obtain bound for R Ω 0 X φ h 2 6. u h ū weak* in W 1, and φ h φ weakly in W 1,2 7. Show that { φ, ū} X. Use the weak continuity of determinants 8. Proof of weak lower semicontinuity of last term in energy analogous to the case of liqud crystal elastomers [Calderer-Liu-Yan, 2006; 2008] 12 / 23

Mechanical dissipation and constitutive equations Postulate Second Law of Thermodynamics in form of Clausius-Duhem inequality (isothermal case): a tr(t T a v a ) φ a ψ a f a v a 0. 13 / 23

Mechanical dissipation and constitutive equations Postulate Second Law of Thermodynamics in form of Clausius-Duhem inequality (isothermal case): a Reversible components of the stress tr(t T a v a ) φ a ψ a f a v a 0. T r 1 = φ 1 Ψ F F T ( φ 1 p + π 1 ) I T r 2 = ( φ 2 p + π 2 ) I π i = h(φ 1,φ 2 ) φ i : osmotic pressures T i = Ti r + η i 2 ( v i + v T i ), f 1 = φ 1 p + β(v 1 v 2 ) = f 2 η i > 0 represents Newtonian viscosity 13 / 23

Energy relation Theorem (Calderer-Zhang, 2008). Let {φ i, v i, p} be a smooth solution of the governing equations. Then it satisfies the following equation of balance of energy: d [( φ 1 dt Ω(t) 2 v 1 2 + φ 2 2 v 2 2 ) + Ψ] dx (t 1 v 1 + t 2 v 2 ) ds 0, Ω(t) 14 / 23

Energy relation Theorem (Calderer-Zhang, 2008). Let {φ i, v i, p} be a smooth solution of the governing equations. Then it satisfies the following equation of balance of energy: d [( φ 1 dt Ω(t) 2 v 1 2 + φ 2 2 v 2 2 ) + Ψ] dx (t 1 v 1 + t 2 v 2 ) ds 0, Ω(t) It is a consequence of the constitutive equations satisfying the second law of thermodynamics Applying the divergence theorem to the terms of the surface terms, we obtain an energy inequality used in proving weak solutions 14 / 23

Governing system revisited ρ 1 t + (v 1 )ρ 1 + ρ 1 v 1 = 0 ρ 2 t + (v 2 )ρ 2 + ρ 2 v 2 = 0 ρ 1 v 1 t + ρ 1(v 1 )v 1 = T 1 + f 1 ρ 2 v 2 t + ρ 2(v )v 2 = T 2 + f 2 φ 1 + φ 2 = 1 15 / 23

Governing system revisited ρ 1 t + (v 1 )ρ 1 + ρ 1 v 1 = 0 ρ 2 t + (v 2 )ρ 2 + ρ 2 v 2 = 0 ρ 1 v 1 t + ρ 1(v 1 )v 1 = T 1 + f 1 ρ 2 v 2 t + ρ 2(v )v 2 = T 2 + f 2 φ 1 + φ 2 = 1 F t + (v 1 )F = ( v 1 )F 15 / 23

Governing system revisited ρ 1 t + (v 1 )ρ 1 + ρ 1 v 1 = 0 ρ 2 t + (v 2 )ρ 2 + ρ 2 v 2 = 0 ρ 1 v 1 t + ρ 1(v 1 )v 1 = T 1 + f 1 ρ 2 v 2 t + ρ 2(v )v 2 = T 2 + f 2 φ 1 + φ 2 = 1 F t + (v 1 )F = ( v 1 )F Difficulty in proving existence due to the last equation [Liu-Walkington, 2001]; it is a conservation law 15 / 23

Governing system revisited ρ 1 t + (v 1 )ρ 1 + ρ 1 v 1 = 0 ρ 2 t + (v 2 )ρ 2 + ρ 2 v 2 = 0 ρ 1 v 1 t + ρ 1(v 1 )v 1 = T 1 + f 1 ρ 2 v 2 t + ρ 2(v )v 2 = T 2 + f 2 φ 1 + φ 2 = 1 F t + (v 1 )F = ( v 1 )F Difficulty in proving existence due to the last equation [Liu-Walkington, 2001]; it is a conservation law It becomes simple if v 1 = 0, not the case here 15 / 23

Evolution equation for the deformation gradient Take divergence of equation: F is,it + v k F is,ik + v k,i F is,k = v i,ij F js + v i,j F js,i If v = 0, it reduces to div(f T ) t + (v ) div(f T ) = 0 Prescribe appropriate initial and boundary values so that div(f T ) = 0 for all time. 16 / 23

Special class of problems: Linearized elasticity 1 φ 1 v 1,t = div T r (F, φ) φ 1 p + η 1 v 1 + β(v 1 v 2 ) φ 2 (v 2,t + (v 2 )v 2 ) = φ 2 (p + π 2 ) +η 1 v 2 + β(v 2 v 1 ) φ 1 = φ 0 (1 tr ( u)) div(φ 1 v 1 + φ 2 v 2 ) = 0 F T F = I + ( u + u T ) + o( u ), v 1 = u t u denotes displacement vector u = x X Coupling of dissipative linear elasticity equations for the solid with Navier-Stokes equations for the polymer; note that the constraint is not the standard one For experimental and modeling references on mechanics of gels, see, [Tanaka-Filmore, 1979], [Doi-Yamaue, 2004, a, b] 1 MCC, Micek, Rognes; work in progress 17 / 23

Special class of problems: Deformable porous media 2 In applications η 1 >> η 2, polymer dissipation much larger than solvent s and also greater than elastic effects φ 0 ((K 2 3 G)( u)i + 2GE) = (p + Π 1 ) ( K B T N 2 V m ((1 φ 0 ) + φ 0 u) + (1 φ 0 )p ) = β(v 1 v 2 ), (φ 0 v 1 + (1 φ 0 )v 2 ) = 0, v 1 = u t. Coupling of steady state elasticity with Stokes problem for fluids, although constraint is non-standard. K, G are elastic moduli The second equation corresponds to Darcy s law Mathematical analogs found in geology in dealing with soil media and clays [Bennethum-Murad-Cushman, 2000] 2 MCC, Chabaud, Luo; work in progress 18 / 23

Special problems Application of finite element analysis to nonlinear problem (Rognes, Micek, MCC; work in progress) Analysis of nonlinear problem in one-dimensional geometry (Ming Chen, MCC; work in progress) 19 / 23

References I [Ball-1977]. J.M. Ball, Convexity conditions and existence theorems in nonlinear elasticity, Arch. Rat. Mech. Anal., 63, 337-403, 1977. [Bennethum-Murad-Cushman, 2000], Macroscale Thermodynamics and the Chemical Potential of Swelling Porous Media, Transport in Porous Media, 39, 187-225, 2000. [Calderer-Liu-Yan, 2006] M.C. Calderer, C. Liu and B. Yan, A model for total energy of nematic elastomers with non-uniform prolate spheroid s, Advances in applied and computational mathematics, 245 259, Nova Sci. Publ., Hauppauge, NY, 2006. [Calderer-Liu-Yan, 2008]. M.C. Calderer, C. Liu and B. Yan, A Mathematical Theory for Nematic Elastomers with Non-uniform Prolate Spheroids, submitted, 2008. [Calderer-Zhang, 2008]. M.C. Calderer and Hang Zhang, Incipient dynamics of swelling of gels, SIAM J. Appl. Math., in press; IMA preprint no. 2188, February 2008; http://www.ima.umn.edu/preprints/feb2008/feb2008.html 20 / 23

References II [Calderer-Chabaud, 2008]. M.C. Calderer, Brandon Chabaud, Suping Lyu and Hang Zhang, Modeling approaches to the dynamics of hydrogel swelling, submitted, IMA preprint no. 2189, February 2008; http://www.ima.umn.edu/preprints/feb2008/feb2008.html [Ciarlet-1987]. P.G. Ciarlet, Mathematical Elasticity, Vol 1, North-Holland, 1987. [Doi-Yamaue, 2004]. T. Yamaue and M. Doi, Swelling dynamics of constrained thin-plate gels under an external force, Phys. Rev. E, 70, 011401, 2004. [Doi-Yamaue, 2004]. T. Yamaue and M. Doi, Swelling dynamics of constrained thin-plate gels under an external force, Phys. Rev. E, 70, 011401, 2004. [Doi-Yamaue, 2004]. T. Yamaue and M. Doi, Swelling dynamics of constrained thin-plate gels under an external force, Phys. Rev. E, 70, 011401, 2004. 21 / 23

References III [Doi-Yamaue, 2004a]. T. Yamaue and M. Doi, Theory of one-dimensional swelling dynamics of polymer gels under mechanical constraint, Phys. Rev. E, 69, 011402, 2004. [Liu-Walkington, 2001]. C. Liu and N. J. Walkington, An Eulerian Description of Fluids Containing Visco-hyperelastic Particles, Arch. Rat. Mech. Anal., 159, 229-252, 2001. [Tanaka-Filmore, 1979]. T. Tanaka and D.J. Filmore, Kinetics of swelling gels, J. Chem. Phys., 70, 1214-1231, 1979. [Tanaka, 1981]. T. Tanaka, Gels, Scientific American, vol 244, 124-138. [Truesdell, 1984]. C. Truesdell, Rational Thermodynamics, Springer Verlag, second edition. [Zhang, 2007]. Hang Zhang, Ph.D. Thesis, Univeristy of Minnesota, July 2007. 22 / 23

Immiscibility and Incompressibility Immiscibility: the constitutive equations depend on volume fractions. It is always possible to distinguish between components Incompressibility: the intrinsic density is constant. Note that ρ = φγ ρ = mass of component, γ = mixture space So the incompressibility statement reduces to γ = constant mass of component component space Back 23 / 23