Biological fluid mechanics at the micro‐ and nanoscale Lecture 6: From Liquids to Solids: Rheological Behaviour Anne Tanguy University of Lyon (France) From Liquids to Solids: Rheological behaviour I. Elastic Solid II. Plastic Flow III. Visco-elasticity IV. Non-Linear rheology Al polycristal (Electron Back Scattering Diffraction) Dendritic growth in Al: Cu polycristal : cold lamination (70%)/ annealing. TiO2 metallic foams, prepared with different aging, and different tensioactif agent: Si3N4 SiC dense What is a « continuous » medium? 1) Two close elements evolve in a similar way. 2) In particular: conservation of proximity. « Field » = physical quantity averaged over a volume element. = continuous function of space. 3) Hypothesis in practice, to be checked. At this scale, forces are short range (surface forces between volume elements) In general, it is valid at scales >> characteristic scale in the microstructure. Examples: crystals d >> interatomic distance (~ Å ) polycrystals d >> grain size (~nm ~mm) regular packing of grains d >> grain size (~ mm) liquids d >> mean free path disordered materials d >> 100 interatomic distances (~10nm) I. Elastic Moduli REMINDER: The Navier-Stokes equation: with for a « Newtonian fluid » 2 3 P I 2h e ( h ).v I wit h e v Thus: for an incompressible, Newtonian fluid. (h dynamical viscosity) S The case of an Elastic Solid: No transport of matter, displacement field u d S S Stress is related to the Strain u wit h e v Hooke’s Law: ij ij0 Cijkl. kl dt (anisotropy) 21 Elastic Moduli Cijlk in a 3D solid. k ,l Thus: 2 u 2 r .(C ( x, y, z ):S u) f t for a Linear Elastic Solid (1635-1703) 1678: Robert Hooke develops his “True Theory of Elasticity” Ut tensio, sic vis (ceiii nosstuv) “The power of any spring is in the same proportion with the tension thereof.” Hooke’s Law: τ = G γ or (Stress = G x Strain) where G is the RIGIDITY MODULUS Example of an homogeneous and isotropic medium: stress componentsσ ij ij0 2m. ij .tr . ij equationsof motion: 2u 2 2m .(.u ) m. ( u ) f ext t 1 V 3 tr 1 compressibility V P tr 2m / 3 2 Elastic Moduli (,m) u F Traction: F u E. S L v u . L L E, Young modulus , Poisson ratio Simple Shear: u Hydrostatic compression: P F u m. S L m, shear modulus 3 3(1 2 ) 3 2m E , compressibility. Sound waves in an isotropic medium: 2 sound wave velocities cL and cT Onde longitudinale: .. cL 2 . 2 , cL 2m 2 2 lmn c L . cL . . n2 m 2 l 2 L Onde longitudinale: Le mouvement des atomes est dans le sens de la propagation Ondes transverses: simple shear m cT . , cT cL .. 2 2 Onde transverse: Le mouvement des atomes est perpendiculaire au sens de la propagation Examples of anisotropic materials (crystals): Ex. cobalt Co: HC FCC T=450°C The number of Elastic Moduli depends on the Symetry FCC 3 moduli C11 C12 C44 HCP 5 moduli C11 C12 C13 C33 C44 C66=(C11-C12)/2 3 moduli (3 equivalent axis) 6 (5) moduli (rotational invariance around an axis) Voigt notation: C C ( ) C C ( ) C C ( E ) (11) 1 ( 22) 2 (33) 3 ( 23) 4 (31) 5 (12) 6 21 independent Elastic Moduli Microscopic expression for the local Elastic Moduli: Simple example of a cubic crystal. On each bond: dEij d2Eij 1 2 r0 (rij r0 ) . 2 r0 ... Eij rij Eij r0 (rij r0 ). dr 2 dr strain stress Elastic Modulus rij r0 r0 d2Eij r0 (rij r0 ). 2 4 fij d r '11 2 4 r0 2 r0 11 2 1 d E ij r0 E ij r0 C11 '11 / 11 . 3 r0 dr 2 r0 General case: Local Elastic Moduli at small strain 1 C (i) Vi E ri1i2 . ( i1i2i3i4 ) ri1i2 ri3i4 2 C1 ~ 2 m 1 eq, .ri1i2 eq, eq .ri3i4 ri1i2 .ri3i4 C2 ~ 2 m 2 eq, eq .ri3i4 eq, .n(i1i2i3i4 ) i (i1i2i3i4 ) Born-Huang C3 ~ 2 (+m 2D Lennard-Jones Glass N=216 225 L=483 Example of an amorphous material M. Tsamados et al. (2007) Progressive convergence to an isotropic material at large scale II. Plastic Flow Plastic Flow: S F u Lz In the Linear Elastic Regime: F/S = E.u/Lz Strain Compressive stress Elastic modulus Plastic Threshold y . Visco-plastic Flow flow F/S vitreloy Plastic Flow Elasticité+ Viscoelasticity Elasticity E u/Lz Rheological Description of the Plastic Flow: . Rheological law: shear stress , at a given P and T, as a function of shear strain, strain rate. Creep experiment: at a constant , what is (t)? Relaxation exp.: at a constant , what is (t)? (here: (t)=m. if Y /m and (t)=Y else) Apparent viscosity: h(t,,d/dt) = (t,,d/dt) / (d/dt) (here: h=∞ if Y /m and h=0 else) Here, no temporal dependence (≠ viscous flow) Example: Flow due to an external force (cf. Poiseuille flow) Binary Lennard-Jones Glass at T=0.2<Tg for tW=104 LJ F. Varnik (2008) Not a Poiseuille Flow at small T (Visco-Plastic) ≠Poiseuille P III. Visco-elasticity Progressive flow of a solid (1643-1727) 1687: Isaac Newton addresses liquids and steady simple shearing flow in his “Principia” “The resistance which arises from the lack of slipperiness of the parts of the liquid, other things being equal, is proportional to the velocity with which the parts of the liquid are separated from one another.” Newton’s Law: τ = η dγ/dt where η is the Coefficient of Viscosity Newtonian Different behaviours: Newtonian Viscous Fluid: Ex. Water, honey.. h cste 0 d 1 1 . (t ) (t ) (t ' )dt .t dt h h0 h t Kelvin-Voigt Solid: E V d (t ) m. (t ) h . dt m .t 0 h (t ) . 1 e m Maxwell Fluid: Delayed Elasticity (anelastic behaviour). characteristic time t c h m Ex. Solid close to Tf Instantaneous Elasticity + Viscous Flow E V L2 kT 0 t d 1 d 1 in crystals . . (t ) (t ) . 0 , h 3 Da dt m dt h m h General Linear Visco-Elastic Behaviour: (t ) f 0 . (t ) t . f t t '. (t ' )dt' 0 (memoryeffect) Dynamical Rheometers: Oscillatory forcing: 0 sin(t ) Response: 0 sin(t ) G( ) G' ( ) iG' ' ( ) tan( ) G' ' / G' " internalfriction" G' (). 0 .sin(t ) G' ' (). 0 . cos(t ) G’, Storage (Elastic) Modulus Instantaneous response Example of Perfect Elastic Solid: G’’, Loss (Viscous) Modulus Delay G' m a nd G' ' 0 Example of Newtonian Viscous Fluid: G' 0 and G' ' h. 2 2 2 h m Example of Maxwell Fluid:G ' m. and G ' ' h.. 2 m 2 2h 2 m 2h 2 0 : viscousresponseG' 0 and G' ' h. : elasticresponseG' m and G' ' 0 Pastes Energy Balance: . 0 d 2 P . .G ' ( ).sin(2t ) . 0 .G ' ' ( ).sin 2 (t ) dt 2 T /4 . 0 2 . 0 2 4 P (t )dt .G ' ( ) .G ' ' ( ) T 0 2 2 Elastic Energy Stored during T/4 And then given back (per unit volume and unit time). Averaged Dissipated Energy per unit time, during T/4, due to viscous friction >0 G ' ' dissipatedenergy tan G' storedenergy Loss Factor (Internal Friction) Loss factor Material > 100 Polymer or Elastomer (example : Butyl rubber) 10-1 Natural rubber, PVC with plasticizer, Dry Sand, Asphalte, Cork, Composite material with sandwich structure (example 3 layers metal / polymer / metal) 10-2 Plexiglas, Wood, Concrete, Felt, Plaster, Brick 10-3 Steel, Iron, Lead, Copper, Mineral Glass 10-4 Aluminium, magnésium Viscoelasticity of Polymers: General features amorphous crystalline Storage Modulus Internal Friction Viscoelasticity of Polymers: Examples Viscoelasticity of Mineral Glasses: Examples SiO2 – Na2O Si– Al-O-N Lekki et al. Viscoelasticity and crystallization Polymer (PET) Mineral Glass ZrF4 Cristallization: G’ increases, mobility decreases Frequency dependent behaviour SiO2-Na20-Ca0 Example of Blood Red Cells: (t)/0 G’ G’’ Macroscopic creep in Metals: Creep T> Lead Romanian Pipe Metals 0,3-0,4 Tm Ceramics 0,4-0,5 Tm Polymers Tg ~ 1h Dislocation creep: b=0 m=4-6 Nabarro-Herring creep: b=2 m=1 Non-Linear behaviour 0.3 Tm<T<0.7 Tm Linear (Newtonian) flow diffusion of defects T>0.7 Tm Metling Temperatures, for P=1 atm, Ice: Tm=273°K, Lead: Tm=600°K, Tungsten: Tm=3000°K m 10-1 Theoretical Limit Plasticity 10-2 Athermal Elastic Limit 10-3 Creep Dislocation Core Volume 10-4 10-5 Elasticity 10-6 0 0,3 Creep Diffusion Grain Volume Boundaries 0,5 0,7 1 T Tm IV. Non-Linear Rheology Pastes Colloids Powders Metallic Glass Mineral Glass (SiO2, a-Si) Polymers (PMMA,PC) From the Liquid to the Amorphous Solid: Non-Linear Rheological Behaviour F. Varnik (2006) 3D Lenard-Jones Glass Non-Linear Rheological Behaviours: Shear softening Ex. painting, shampoo n . K . with n 1 Ostwald (1925) Shear thickening Ex. wet sand, polymeric oil, silly-putty n . K . with n 1 Plastic Fluid Ex. amorphous solids, pastes . C 0 n . C C K . Bingham n 1, Herschel- Bulkley n 1, Casson Example: in amorphous systems (glasses, colloids..) Ex. Beads made of polyelectric gel with <1 Ex. Lennard-Jones Glass Tsamados, 2010 . xy / h . shear softening Simulations of Rheological Behaviour at constant Strain Rate and Temperature in an amorphous glassy material (Lennard-Jones Glass) Low strain rate Progressive Diffusion of Local Rearrangements Finite Size Effects Large strain rate Nucleation of Local Rearrangements M. Tsamados 2010 Density of nucleating centers per unit strain Diffusion of plasticity Cooperativity Maximum when L1=L2 h ? m Lecture 7 Atomistic Modelling: Classical Molecular Dynamics Simulations for fluid dynamics. I. Description II. The example of Wetting III. The example of Shear Deformation Classical Molecular Dynamics Simulations consists in solving the Newton’s equations for an assembly of particles interacting through an empirical potentiaL; In the Microcanonical Ensemble (Isolated system): Total energy E=cst In the Canonical Ensemble: Temperature T=cst with if no external force Different possible thermostats: Rescaling of velocities, Langevin-Andersen, Nosé-Hoover… more or less compatible with ensemble averages of statistical mechanics. Equations of motion: the example of Verlet’s algorithm. Adapt the equations of motion, to the chosen Thermostat for cst T. Thermostats: after substracted the Center of Mass velocity, or the Average Velocity along Layers dv • Langevin Thermostat: mi i G.vi Fi k (t ) dt Random force k(t) Friction force –G.v(t) with <k(t).k(t’)>=cste.2GkBT.(t-t’) • Andersen Thermostat: prob. of collision t, Maxwell-Boltzman velocity distr. • Nosé-Hoover Thermostat: dH 0 dt ' • Rescaling of velocities: • Berendsen Thermostat: with ( )1/2 Heat transfer. Coupling to a heat bath. Examples of Empirical Interactions: The Lennard-Jones Potential: 2-body interactions cf. van der Waals Length scales ij ≈ 10 Å Masses mi≈10-25 kg Energy ij≈ 1 eV ≈ 2.10-19J ≈ kBTm Time scale Time step t = 0.01 ≈ 10-14 s 106 MD steps ≈ 10-8 s = 10 ns or m. 2 0.1 2 1020 8 1012 s 10 s or D(T 1) 10 12 106x10-4=100% shear strain in quasi-static simulations N=106 particles, Box size L=100 ≈ 0.1 mm for a mass density =1. 3.N.Nneig≈108 operations at each « time » step. The Stillinger-Weber Potential: For « Silicon » Si, with 3-body interactions Stillinger-Weber Potential F. Stillinger and T. A. Weber, Phys. Rev. B 31 (1985) 4 ESW (1,2,...,N ) i , j ( A.r B ). e Melting T Vibration modes Structure Factor ( r a ) 1 2-body interactions (Cauchy Model) .(rij a ) 1 .(rik a ) 1 i , j ,k f (ijk ). e 3-body interactions The BKS Potential: For Silica SiO2, with long range effective Coulombian Interactions B.W.H. Van Beest, G.J. Kramer and R.A. Van Santen, Phys. Rev. Lett. 64 (1990) EBKS (r ) qi q j 4 0 r Aij e Bij r Cij r 6 où(i, j ) Si,O Ewald Summation of the long-range interactions, or Additional Screening (Kerrache 2005, Carré 2008) Example: Melting of a Stillinger-Weber glass, from T=0 to T=2. Microscopic determination of different physical quantities: -Density profile, pair distribution function -Velocity profile -Diffusion constant -Stress tensor (Irwin-Kirkwood, Goldenberg-Goldhirsch) -Shear viscosity (Kubo) II. The example of Wetting Surface Tension: coexistence beween the liquid and the gas at a given V. Surface Tension: h The Molecular Theory of Capillarity: Intermolecular potential energy u(r). Total force of attraction per unit area: Fz h 1. 2 dz d 3r. f z r h 21. 2 r (r h)u (r )dr h Work done to separate the surfaces: h0 h0 W 2 S Fz h dh 1. 2 dr .r 3 .u (r ) (I. Israelachvili, J.S.Rowlinson and B.Widom) 3 LV . cos SV SL for SV SL LV . III. The example of Shear Deformation Boundary conditions: Example: quasi-static deformation of a solid material at T=0°K Quasi-static shear at T=0. Fixed walls Or biperiodic boundary conditions (Lees-Edwards) At each step, apply a small strain ≈ 10-4 on the boundary, And Relax the system to a local minimum of the Total Potential Energy V({ri}). Dissipation is assumed to be total during . t a / c 1012 s Quasi-Static Limit .c lim.c 108 s 1 ( 10 4 u LJ ). t a a ux F xy shear stress S Ly st rain xy Rheological behaviour: Stress-Strain curve in the quasi-static regime ux 2 Ly F xy shear stress S ux Ly st rain xy ux 2 Ly y Local Dynamics: Global and Fluctuating Motion of Particles X F xy shear stress S ux Ly Local Dynamics: Global and Fluctuating Motion of Particles Transition from Driven to Diffusive motion due to Plasticity, at zero temperature. y _ max st rain xy cage effect (driven motion) ux 2 Ly p Diffusive n ~ xy Tanguy et al. (2006) Low Temperature Simulations: Athermal Limit . Typical Relative displacement due to the external strain Typical vibration of the atom due to thermal activation >> larger than a. .t k BT kh Convergence to the quasi-static behaviour, in the athermal limit: At T=10-8 (rescaling of the transverse velocity vy et each step) M. Tsamados (2010) . h . . . 0 .4 h . cste at finite T Effect of aging T= 0.2-0.5 Tg =0.435 Rescaling of transverse velocities in parallel layers Non-uniform Temperature Profile at Large Shear Rate Time needed to dissipate heat created by applied shear across the whole system c 1 m td L L . dQ xy . Heat creation rate due to plastic deformation dt tQ Time needed to generate kBT, . tQ t d k BT . xy . k BT .L . c. xy Visco-Plastic Behaviour: Non uniform T Flow due to an external force (cf. Poiseuille flow) F. Varnik (2008) The relative importance of Driving and of Temperature must be chosen carefully. See you in Lyon!