SOME ISSUES AND PERSPECTIVES IN GRANULAR PHYSICS

Similar documents
Granular packings: internal states, quasi-static rheology

Agnolin, I., Roux, J.-N. (2007): Internal states of model isotropic granular packings. III. Elastic properties. - Physical Review E, 76, 6, ,

The response of an idealized granular material to an incremental shear strain

Bifurcation Analysis in Geomechanics

Inhomogeneous elastic response of amorphous solids

Granular Micro-Structure and Avalanche Precursors

Micromechanics of granular materials: slow flows

Table of Contents. Foreword... xiii Introduction... xv

8.1. What is meant by the shear strength of soils? Solution 8.1 Shear strength of a soil is its internal resistance to shearing stresses.

Indiana University, January T. Witten, University of Chicago

MODELING GEOMATERIALS ACROSS SCALES JOSÉ E. ANDRADE DEPARTMENT OF CIVIL AND ENVIRONMENTAL ENGINEERING EPS SEMINAR SERIES MARCH 2008

Discrete Element Modelling in Granular Mechanics WUHAN seminars, China, 28th august-2nd september 2017

collisions inelastic, energy is dissipated and not conserved

Soil strength. the strength depends on the applied stress. water pressures are required

MODELING GEOMATERIALS ACROSS SCALES

STUDY OF THE MECHANICAL BEHAVIOUR OF THE BALLAST USING

Laboratory Testing Total & Effective Stress Analysis

Stress and fabric in granular material

Numerical Simulations of Triaxial Test with Sand Using DEM

SIMULATION OF A 2D GRANULAR COLUMN COLLAPSE ON A RIGID BED

Micro-Macro transition (from particles to continuum theory) Granular Materials. Approach philosophy. Model Granular Materials

Theory of Shear Strength

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay

Local Anisotropy In Globally Isotropic Granular Packings. Kamran Karimi Craig E Maloney

VISCOELASTIC PROPERTIES OF POLYMERS

Quasistatic rheology and the origins of strain

Micro-macro modelling for fluids and powders

Steady Flow and its Instability of Gravitational Granular Flow

Particle flow simulation of sand under biaxial test

A micromechanical approach to describe internal erosion effects in soils

MHA042 - Material mechanics: Duggafrågor

Clusters in granular flows : elements of a non-local rheology

Stress and Strains in Soil and Rock. Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University

Mechanics of Earthquakes and Faulting

SHEAR STRENGTH OF SOIL

SOIL MODELS: SAFETY FACTORS AND SETTLEMENTS

Geology 229 Engineering Geology. Lecture 5. Engineering Properties of Rocks (West, Ch. 6)

Joe Goddard, Continuum modeling of granular media

Module 5: Failure Criteria of Rock and Rock masses. Contents Hydrostatic compression Deviatoric compression

Development and application of time-lapse ultrasonic tomography for laboratory characterisation of localised deformation in hard soils / soft rocks

A Constitutive Framework for the Numerical Analysis of Organic Soils and Directionally Dependent Materials

Force, relative-displacement, and work networks in granular materials subjected to quasistatic deformation

Lateral Earth Pressure

Prestress stability. Lecture VI. Session on Granular Matter Institut Henri Poincaré. R. Connelly Cornell University Department of Mathematics

A discrete element analysis of elastic properties of granular materials

Coupling DEM simulations and Physical Tests to Study the Load - Unload Response of an Ideal Granular Material

The Stress Variations of Granular Samples in Direct Shear Tests using Discrete Element Method

Entropy and Material Instability in the Quasi-static Mechanics of Granular Media

Theory of Shear Strength

Discrete Element Modelling of a Reinforced Concrete Structure

Intro to Soil Mechanics: the what, why & how. José E. Andrade, Caltech

Triaxial Shear Test. o The most reliable method now available for determination of shear strength parameters.

The Influence of Contact Friction on the Breakage Behavior of Brittle Granular Materials using DEM

Axially Loaded Piles

Quasistatic behavior and force transmission in packing of irregular polyhedral particles

Available online at ScienceDirect. Procedia Engineering 103 (2015 )

A local constitutive model with anisotropy for ratcheting under 2D axial-symmetric isobaric deformation

202 Index. failure, 26 field equation, 122 force, 1

Limits of isotropic plastic deformation of Bangkok clay

GEO E1050 Finite Element Method Mohr-Coulomb and other constitutive models. Wojciech Sołowski

RHEOLOGY & LINEAR ELASTICITY. B Importance of fluids and fractures in deformation C Linear elasticity for homogeneous isotropic materials

20. Rheology & Linear Elasticity

TC211 Workshop CALIBRATION OF RIGID INCLUSION PARAMETERS BASED ON. Jérôme Racinais. September 15, 2015 PRESSUMETER TEST RESULTS

APPENDIX I. Deformation Analysis of the Left Abutment

SOIL SHEAR STRENGTH. Prepared by: Dr. Hetty Muhammad Azril Fauziah Kassim Norafida

Discrete element modeling of self-healing processes in damaged particulate materials

1.8 Unconfined Compression Test

Characterization of Thermo-mechanical Performances related to Breeder Pebble Beds by Discrete Element Method

Mechanics of Earthquakes and Faulting

The Role of Slope Geometry on Flowslide Occurrence

Shear dynamics simulations of high-disperse cohesive powder

TIME-DEPENDENT BEHAVIOR OF PILE UNDER LATERAL LOAD USING THE BOUNDING SURFACE MODEL

NUMERICAL MODELING OF INSTABILITIES IN SAND

ELASTOPLASTICITY THEORY by V. A. Lubarda

Recent Research on EPS Geofoam Seismic Buffers. Richard J. Bathurst and Saman Zarnani GeoEngineering Centre at Queen s-rmc Canada

Constitutive modelling of fabric anisotropy in sand

arxiv:cond-mat/ v2 [cond-mat.soft] 18 Dec 2006

Module-4. Mechanical Properties of Metals

An experimental assessment of displacement fluctuations in a 2D granular material subjected to shear

Game Physics. Game and Media Technology Master Program - Utrecht University. Dr. Nicolas Pronost

DYNAMIC ANALYSIS OF PILES IN SAND BASED ON SOIL-PILE INTERACTION

Brittle Deformation. Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm

On the mechanical behaviour of dry cohesionless soils by DEM simulations

Verification of the Hyperbolic Soil Model by Triaxial Test Simulations

Cyclic Behavior of Sand and Cyclic Triaxial Tests. Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University

arxiv:physics/ v1 [physics.comp-ph] 9 Nov 2005

Prediction of torsion shear tests based on results from triaxial compression tests

Experimental Validation of Particle-Based Discrete Element Methods

CALIBRATION OF AN ADVANCED SOIL CONSTITUTIVE MODEL FOR USE IN PROBABILISTIC NUMERICAL ANALYSIS

Mechanics of Earthquakes and Faulting

Basic Mechanical Properties of Wet Granular Materials: A DEM Study

Compression and swelling. Mechanisms of compression. Mechanisms Common cases Isotropic One-dimensional Wet and dry states

Breakdown of Elasticity Theory for Jammed Hard-Particle Packings: Conical Nonlinear Constitutive Theory

Mechanics PhD Preliminary Spring 2017

Reference material Reference books: Y.C. Fung, "Foundations of Solid Mechanics", Prentice Hall R. Hill, "The mathematical theory of plasticity",

Shear strength. Common cases of shearing In practice, the state of stress in the ground will be complex. Common cases of shearing Strength

Cavity Expansion Methods in Geomechanics

Effect of structural design on fundamental frequency of reinforced-soil retaining walls

Liquefaction and Post Liquefaction Behaviour of Granular Materials: Particle Shape Effect

Turbulentlike Quantitative Analysis on Energy Dissipation in Vibrated Granular Media

Transcription:

1 SOME ISSUES AND PERSPECTIVES IN GRANULAR PHYSICS Jean-Noël Roux Laboratoire des Matériaux et des Structures du Génie Civil Unité Mixte de Recherche LCPC-ENPC-CNRS Institut Navier, Champs-sur-Marne, France Partly inspired by (or emerged from) the...

2 Recent granular trimester at Institut Henri Poincaré January 5 April 8, 2005. Organized by A. Barrat (CNRS, LPTHE, Orsay), Ph. Claudin (CNRS, PMMH, Paris) and J.-N. Roux 12 resident, invited scientists for one month at least, and many participants for shorter durations (60, outside meetings) Sets of lectures : dense granular flows (O. Pouliquen); geophysical applications (B. Andreotti); granular systems and glassy dynamics (J. Kurchan, D. Dean); Geometry, rigidity and stability (R. Connelly) ; quasistatic rheology and microstructure (F. Radjai) ; results on granular systems in soil mechanics (F. Tatsuoka)

3 Recent granular trimester at Institut Henri Poincaré many seminars, some gathered in one day on the same theme : Isostatic structures (D. Wu); Cosserat modelling (E. Grekova) 3 thematic meetings (2-3 days) : liquid-solid transition (F. Chevoir, O. Pouliquen) ; instabilities, bifurcations, localisation (J. Sulem, I. Vardoulakis); discrete numerical simulations (S. Luding, J.-N. Roux) See web site http://www.ihp.jussieu.fr

4 Some results and perspectives about solid-like granular materials Currently investigated and debated issues Presentation will hopefully provoke discussions Relies heavily on discrete computer simulations of granular materials Focus on material behavior, i. e., stress/strain/internal state relationships within homogeneous samples, to be applied locally in the general, inhomogeneous case ( boundary value problem)

5 Outline Some basic features of macroscopic granular mechanics Ingredients of a microscopic model Grain-level approach to mechanical properties: selected topics 1. Frictionless systems: isostaticity property (in the rigid limit), minimization property... and consequences 2. Granular packings with friction: internal states, dependence on assembling procedure and micromechanical parameters 3. Elasticity : elastic domain, prediction of elastic moduli 4. Quasistatic (non-elastic) response, type I : deformation of contact network 5. Quasistatic deformation, type II : rearrangements (network continuously broken and repaired)

ɛ 1, σ 1 Rheometry of solid granular materials: triaxial apparatus uniform stress and strain q = σ 1 σ 3 peak 6 σ 2 = σ 3 σ 3 σ 3 σ PSfrag 10 replacements 1000kP a ɛ 10 2 s role of density σ 1 /σ 3 maximum ɛ v = volumetric strain (dilatancy) ɛ v ɛ 1 Dense and loose systems approach same critical state for large strains Irreversibility most accurate devices measurements of ɛ 10 6

σ 1 A simplified model ɛ v 7 σ 3 1+sin Φ 1 sin Φ ments PSfrag replacements slope 1 2ν slope E ɛ 1 slope 2 sin ψ 1 sin ψ ɛ 1 Linear elasticity + Mohr-Coulomb plasticity criterion, here written with principal stresses σ 1 σ 2 σ 3 0: f(σ) = σ 1 σ 3 2 σ 1 + σ 3 2 sin ϕ 0 + flow rule (dilatancy). Plastic potential ( ɛ p = λ g σ, λ 0) g(σ) = σ 1 σ 3 2 σ 1 + σ 3 2 sin ψ

Basic characteristics of solid material behaviour 8 Mohr-Coulomb model contains basic ingredients with essentially model-independent definition internal friction angle ϕ, associated with peak strength strain level necessary to mobilize internal friction dilatancy angle (ψ < ϕ) How could one obtain a prediction of those quantities? Insufficiencies of the Mohr-Coulomb model: no difference between peak and residual strength does not include role of initial density elasticity is non-linear and pre-peak response is predominantly non elastic (non reversible). Elastic moduli for slope of stress-strain curve = misleading term

9 Observations and models for sands Elasticity: moduli measured as slope of stress-strain curves if ɛ 10 5 (typically). Values agree with sound propagation measurements Anisotropy : peak strength, pre-peak strains depend on initial (inherent) anisotropy effects of stress history (overconsolidation) Shear banding: both theoretical and experimental studies. Entails particle size effects Slow dynamics, creep Well characterised and documented phenomena in soil mechanics literature. Phenomenological laws available. Practical importance (foundation engineering) established

10 Creep and elastic domain di Benedetto et al. Under constant stress, samples creep (for hours, days...). Elastic moduli measures on unloading... or cycling, or reloading at constant rate after creep period

11 Contact laws : schematic presentation t ij F N ij n ij j i U N ij = n ij.(u i u j ) U N ij Fij T µ F N ij U T ij = t ij.(u i u j )+R i δθ i +R j δθ j (rigidity matrix G) U ij T analogous to macroscopic laws, but... µf N ij

12 Role of geometry: rearrangements as origins of packing deformation Example with frictionless, rigid disks, one mobile grain and two equilibrium positions Potential energy Q = F x /F y vs. position x. minimization Macroscopic behavior naïve average of contact law

13 Ingredients of a microscopic model. Dimensionless parameters Model involves geometry, inertia, contact law + parameters of the experiment: strain rate ɛ, pressure P. Stiffness number κ, κ = K N /P (linear 2D), κ = K N /(P a) (linear 3D), κ = (E/(1 ν 2 )P ) 2/3 for Hertz contacts. Rigid grain limit: κ K N /K T or Poisson coefficient ν of the grain material Reduced strain rate or inertia number I = ɛ m/ap. Quasi-static limit: I 0 ζ ratio of viscous damping to its critical value in a contact Friction coefficient µ

Granular disorder I : forces 14 Normal force intensity line width

Granular disorder II : displacements 15 Non-affine part of displacement field between two neighbouring equilibrium configurations (biaxial compression). Non negligible, often dominant

16 mechanical properties are simpler Frictionless systems statistical properties are more complicated studied by several authors (C. Moukarzel, A. Tkachenko et al., R. Ball..., JNR), often attributed exotic properties can be dealt with by rigidity theory (bar frameworks, tensegrities... R. Connelly s lectures at IHP) discrete maths literature in the κ limit, properties reduce to geometry

17 Frictionless systems: minimization property The potential energy of external forces (+ elastic energy if deformable grains) is minimized in mechanical equilibrium. Applies to rigid grains (κ = + ), with impenetrability constraints. Normal contact forces are Lagrange multipliers Example: local density maximum in configuration space = stable mechanical equilibrium under isotropic pressure With cohesionless spheres, zero variation to first order means instability If minimization problem becomes convex, then the solution is unique. Happens: for rigid cables within the approximation of small displacements (ASD: linearize distance variations)

18 Frictionless systems, rigid grains: isostaticity property I Isostaticity properties = properties of rigidity matrix G. Its transpose expresses mechanical equilibrium conditions as linear relations between contact forces and external forces with generic disorder, absence of force indeterminacy. Sets upper bound on coordination numbers (4 for disks and 6 for general objects in 2D; 6 for spheres, 10 for axisymmetric objects and 12 in general in 3D see Donev et al. on spheroids) Once contacts are known, contact forces resolving the load, if they exist, are uniquely determined (isostatic problem) if uniqueness property holds, then the list of force carrying contacts is also determined (not true in general)

19 Role of geometry: rearrangements as origins of packing deformation Potential energy Q = F x /F y vs. position x. minimization Isostaticity of each equilibrium contact set, no uniqueness

20 Role of the ASD With the ASD: Uniqueness elastic behaviour Minimization of potential energy Q = F x /F y versus position x.

21 Cables versus struts Minimization of potential energy Q = F x /F y versus position Uniqueness. No force indeterminacy, but stable mechanism (kernel of G). Elastic behaviour x.

22 Frictionless cohesionless rigid spheres: isosaticity property II In equilibrium, the force-carrying structure is devoid of force indeterminacy and devoid of mechanisms (floppy modes). It is an isostatic structure Matrix G is square and inversible: one-to-one correpondence between applied load and contact forces only true for spheres, for which there is a lower bound on coordination number z (excluding rattlers). z = 6 (3D), z = 4 (2D) Apart from the motion of rattlers, equilibrium states are isolated points in configuration space. Particles rearrange by jumping to different configurations with different contact network topology

23 Frictionless systems, rigid grains, no cohesion: fragility property Distribution of deviator stress intervals for which a given configuration is stable (biaxial compression of rigid frictionless disk assemblies satisfying isostaticity property in 2D), 1000 N 5000 particles, Combe and Roux 2000

24 Consequences Response to stress increments involves rearrangements (except if δσ σ) how forces distribute on isostatic network (ignoring sign conditions) : still open question (depends on fabric?) isostaticity is compatible with elastic behaviour (cable networks). Arguments predicting exotic properties should not apply to cable networks what about soft grains?

4900 disks in equilibrium (isotropic stress state, two wall d.o.f.). n = 4633 disks and N = 2n + 2 = 9268 contacts carry forces. Isostatic force-carrying structure 25

Generically disordered assemblies of spheres (nearly) rigid, frictionless, cohesionless contacts 26

27 Triaxial tests on frictionless spheres From initial isotropic state, apply: σ 1 = p q/2 σ 2 = p q/2 σ 3 = p + q increasing stepwise q/p by 0.02, waiting for equilibrium

Triaxial tests on frictionless spheres Packing fraction Φ and axial strain ɛ 3 vs. principal stress ratio. n = 1372 (small symbols), n = 4000 (connected dots) 28

Triaxial tests on frictionless spheres Fabric parameter χ = 3 n 2 z 1 versus principal stress ratio. 29

30 Triaxial tests on frictionless spheres: conclusions Apparently, no clear approach to stress-strain curve (it was concluded before that no such curve existed, Combe 2000) evidence for a fabric/stress ratio relationship internal friction angle 5 or 6 degrees no dilatancy, RCP density for different stress states

31 Cut through dense sphere packing Difficult to obtain coordination number from direct observations

Microstructures of frictional packings 32 Much wider variety than with frictionless ones: different solid fractions Φ possible (while disordered frictionless packs never below RCP density) deposition anisotropy independence between density and coordination number. Example: Numerical procedure (C) designed to mimic vibration compaction produces high density (Φ 0.635), low coordination number (z 4.5), high rattler fraction (13%) isotropic sphere packings under low pressure with µ = 0.3

Initial states, coordination number and packing fraction 33 Simulated glass bead packs (E = 70GPa), assembled in isotropic states by different procedures. Packing fractions (at 10 kpa): Φ A = 0.637 > Φ C = 0.635 > Φ B = 0.625 > Φ D = 0.606

34 Effect of pressure increase on coordination number relatively moderate in most usual experimental range (no more than a few MPa) Both µ and ζ have influence (see e.g., Silbert et al.) on result of assembling process, while dense flow or quasi-static deformation are not sensitive to viscous dissipation More studies needed: incomplete experimental or numerical knowledge, no theory for the sudden arrest of flow and compression of a granular gas into a quiescent solid

35 ELASTICITY OF GRANULAR PACKINGS Elasticity of contact network (= spring network if friction not mobilized, which is usually the case at equilibrium) Effect of confining pressure on moduli Deviation from expected behaviour (e.g., from affine approximation) predicting growth as P 1/3 for Hertz contacts

Simulated glass beads: pressure-dependent elastic moduli 36 A = square dots C = open circles D = crosses B not shown (close to A) Moduli are shown with connected symbols Estimates (bounds) are shown as symbols (not connected) for A and C

37 Elasticity of sphere packings under isotropic pressure bulk modulus B satisfactorily bracketed by simple approximations (Voigt-Reuss type bounds) Shear modulus exhibits more anomalous behaviour, especially in low-z systems pressure increase faster than expected not due to z increase (would affect B as well as G) related to anomalous distribution of eigenvalues of stiffness matrix in systems with low force indeterminacy (see O Hern et al., Wyart et al.)? elastic moduli related to coordination number (rather than density)

38 ANELASTIC BEHAVIOUR OF CONTACT NETWORKS Emerging theme... see publications on set of possible contact forces, force indeterminacy... (McNamara et al., Snoeijer et al...) Static problem, can be dealt with regarding contact set as network of springs and plastic sliders in the recent literature, focus on forces rather than (small) displacements. Critical yield analysis formulation: consider e.g. an equilibrium state in 2D under σ 1 = σ 2 = p, apply σ 1 = p + q, σ 2 = p, by increments of q (biaxial compression). For which q value does the initial contact network become unstable? Ask whether contact forces exist that are both statically admissible (they balance the load), and plastically admissible (they satisfy Coulomb inequalities). This is a necessary condition for stability (supported load) Is it sufficient?

Some bad news 39 For a solution to exist, it is necessary that contact forces both plastically and statically admissible exist. For grains with Coulomb friction this is not sufficient. Example: y Grain mobile F ext t 1 n 1 α α Grain fixe n 2 t 2 Grain fixe x For α < ϕ (friction angle) all external forces can be balanced by contact forces in Coulomb cone (Halsey-Ertas ball in a groove system, See study by S. McNamara, R. García Rojo and H. Herrmann)

40 Biaxial compression test: static elastoplastic calculation vs. MD 0.9 0.8 q p 0-1e-06 ɛ v 0.7-2e-06 0.6-3e-06 0.5-4e-06 0.4-5e-06 ents MD 0.3 0.2 0.1 PSfrag replacements ɛ 1-6e-06-7e-06-8e-06 0-9e-06 0 1e-05 2e-05 3e-05 4e-05 5e-05 0 1e-05 2e-05 3e-05 4e-05 5e-05 4900 disks. Identical results for static (dots) and MD (curves) calculations. Results with G. Combe (2001,2002) ɛ 1

41 Biaxial compression: other results and remarks Strains are inversely proportional to K N (normal stiffness of contacts) Detailed comparisons show that static and dynamic methods locally give identical results (small systems) Static method applicable as long as initial network carries deviator (type I strains) It fails as soon as the network has to rearrange Contacts open, others yield in plastic sliding... non-elastic and non-linear behaviour Upper q limit of static method range appears to have finite limit q 1 as n, even for κ. Granular systems with friction are not fragile q 1 is strictly smaller than the deviator maximum

42 Properties of quasi-static regime I strains inversely proportional to κ (hence small), non reversible (plastic), but contained by contacts staying in elastic regime evolution via a continuous set of equilibrium states in configuration space (quasistatic in the strictest sense) little sensitivity to perturbations, return to equilibrium easy regime extends to large stress intervals when coordination number is high (large force indeterminacy), or upon unloading (friction being mobilized in the direction associated with loading)

43 Beyond stability of initial network, Regime II strains not sensitive to stiffness level κ larger fluctuations, slower approach to large system limit successive equilibrium states do not form continuous trajectory in configuration space: system has to evolve by dynamic crises. Quasistatic evolution in an extended sense (if details of the dynamics statistically irrelevant) Characteristic of quasistatic response of granular assemblies with low force indeterminacy

Triaxial compression, from isotropic initial state: influence of κ 44 Dense state (Φ 0.635 for large κ), coordination number z 4.6 if κ 10 4 (10 kpa). Strain independent on κ (type II) except at very low ɛ a (inset : slope = elastic modulus) Assembling method mimics compaction by vibration

Triaxial compression, from other isotropic initial state: 45 Dense state (Φ 0.637 for large κ), coordination number z 6 if κ 10 4 (10 kpa). Strain of order κ 1. Assembling method with µ = 0 (perfect lubrication). Type I strain regime

Internal state evolution in quasistatic deformation: contact orientations 46 Rothenburg ( 1990), Radjai, Kruyt and Rothenburg...

47 Microscopic theoretical approaches, attempted predictions Homogenization ideas (from continuum mechanics of disordered media): bounds, self-consistent estimates... limited to regime I. (Jenkins & La Ragione...) important to delineate regimes I and II! Attempts to describe internal state (complete list of state variables)... in other words : define an ensemble Variables include density, coordination number and fabric tensors (contact anisotropy)... Critical state = stationary state for such variables Neglect of specific geometry of granular packings, and of its variability... = pitfalls of modelling attempts