François Chevoir, Jean-Noël Roux Laboratoire Navier (LCPC, ENPC, CNRS) DENSE GRANULAR MATERIALS Microscopic origins of macroscopic behaviour GdR CHANT.

Slides:



Advertisements
Similar presentations
Mechanics of Composite Materials
Advertisements

Example: Derive EOM for simple 1DOF mechanical system
Coulomb or Dry Friction Damping.
Deformation of Sediments via Grain-Scale Simulations: Variational Algorithm Ran Holtzman, Dmitriy Silin, Tad Patzek U.C. Berkeley
Review Chap. 7 Potential Energy and Energy Conservation
Lecture 2 Free Vibration of Single Degree of Freedom Systems
Kinetics of Particles Impulse and Momentum.
Chapter 11 Angular Momentum
Revision Previous lecture was about Harmonic Oscillator.
Micromechanics Macromechanics Fibers Lamina Laminate Structure Matrix.
Chapter Outline Shigley’s Mechanical Engineering Design.
Some Ideas Behind Finite Element Analysis
Physics 111: Mechanics Lecture 10 Dale Gary NJIT Physics Department.
Dynamics of Rotational Motion
Chapter 8 Rotational Equilibrium and Rotational Dynamics.
2008 Physics 2111 Fundamentals of Physics Chapter 11 1 Fundamentals of Physics Chapter 12 Rolling, Torque & Angular Momentum 1.Rolling 2.The Kinetic Energy.
Jump to first page 1 Normal stress = Chapter 2 Mechanics of Materials Example: Estimate the normal stress on a shin bone ( 脛骨 ) ATensile stress (+) Compressive.
Granular flows under the shear Hisao Hayakawa* & Kuniyasu Saitoh Dept. Phys. Kyoto Univ., JAPAN *
Modeling Static Friction of Rubber-Metal Contact
Chapter 12: Rolling, Torque and Angular Momentum.
Physics 111: Elementary Mechanics – Lecture 11 Carsten Denker NJIT Physics Department Center for Solar–Terrestrial Research.
UNC Chapel Hill S. Redon - M. C. Lin Rigid body dynamics II Solving the dynamics problems.
Physics of Rolling Ball Coasters
1 MFGT 242: Flow Analysis Chapter 3: Stress and Strain in Fluid Mechanics Professor Joe Greene CSU, CHICO.
MECH 221 FLUID MECHANICS (Fall 06/07) Chapter 4: FLUID KINETMATICS
Physics 106: Mechanics Lecture 06 Wenda Cao NJIT Physics Department.
Semester Physics 1901 (Advanced) A/Prof Geraint F. Lewis Rm 560, A29
Hydrodynamic Slip Boundary Condition for the Moving Contact Line in collaboration with Xiao-Ping Wang (Mathematics Dept, HKUST) Ping Sheng (Physics Dept,
A Generalized Frame work Viscous Fluid Flow… P M V Subbarao Professor Mechanical Engineering Department I I T Delhi Construction of Navier-Stokes Equations.
Jamming Peter Olsson, Umeå University Stephen Teitel, University of Rochester Supported by: US Department of Energy Swedish High Performance Computing.
Shawn Kenny, Ph.D., P.Eng. Assistant Professor Faculty of Engineering and Applied Science Memorial University of Newfoundland ENGI.
Spring Forces and Simple Harmonic Motion
1 TENSORS/ 3-D STRESS STATE. 2 Tensors Tensors are specified in the following manner: –A zero-rank tensor is specified by a sole component, independent.
Conservation Laws for Continua
Rotation and angular momentum
Spring Topic Outline for Physics 1 Spring 2011.
Rigid Body: Rotational and Translational Motion; Rolling without Slipping 8.01 W11D1 Today’s Reading Assignment Young and Freedman: 10.3.
ME 520 Fundamentals of Finite Element Analysis
Give the expression for the velocity of an object rolling down an incline without slipping in terms of h (height), M(mass), g, I (Moment of inertia) and.
Chapters 10, 11 Rotation and angular momentum. Rotation of a rigid body We consider rotational motion of a rigid body about a fixed axis Rigid body rotates.
Viscoelasticity While water and air are Newtonian, lots of other common stuff isn’t: –Blood, paint, and many others have nonlinear viscosity (the faster.
Chapter 7. Free and Forced Response of Single-Degree-of-Freedom Linear Systems 7.1 Introduction Vibration: System oscillates about a certain equilibrium.
Fluid Flows due to Pure Mechanical Forces… P M V Subbarao Professor Mechanical Engineering Department I I T Delhi Construction of Navier-Stokes Equations.
1 (a)Discrete Dynamical Systems : 1.Inverted Double Pendulum: Consider the double pendulum shown: 2.Some analytical models of nonlinear physical systems.
Lecture 3 Kinematics Part I
Elasticity I Ali K. Abdel-Fattah. Elasticity In physics, elasticity is a physical property of materials which return to their original shape after they.
EXPLORATION GEOPHYSICS THE EXPLORATION TASK PLAN EXPLORATION APPROACH FOR A MATURE TREND GATHER DATA FOR A MATURE TREND DEVELOP PLAY PROSPECT FRAMEWORK.
Chapter 7: Rotational Motion and the Law of Gravity Angular Speed & Acceleration  A unit of angular measure: radian y x P r  s = r  where s,r in m,
Plastic Deformation Permanent, unrecovered mechanical deformation  = F/A stress Deformation by dislocation motion, “glide” or “slip” Dislocations –Edge,
Rheophysics of wet granular materials S. Khamseh, J.-N. Roux & F. Chevoir IMA Conference on Dense Granular Flows - Cambridge - July 2013.
A novel approach for thermomechanical analysis of stationary rolling tires within an ALE-kinematic framework A. Suwannachit and U. Nackenhorst Institute.
Rheophysics of athermal granular materials
PHY205 Ch16: Rotational Dynamics 1.Combination Translational and Rotational motion and Atwood machine 2.Discuss Ball rolling down incline from 3 different.
Chapter 10 Lecture 18: Rotation of a Rigid Object about a Fixed Axis: II.
Boundary Value Problems in Elasticity
Rigid Body: Rotational and Translational Motion; Rolling without Slipping 8.01 W11D1.
EAG 345 – GEOTECHNICAL ANALYSIS
Course Outline Course Outline Exam topics MATLAB tutorial
Mechanical Vibrations
Chapter 4 Fluid Mechanics Frank White
Continuum Mechanics (MTH487)
Chapter six: Friction Section A Frictional Phenomena 1.
PHYS 1443 – Section 003 Lecture #18
Continuum Mechanics for Hillslopes: Part V
Continuum Mechanics for Hillslopes: Part III
Engineering Mechanics: Statics
Thermodynamic Energy Balances in Solids
Chapter 11 Angular Momentum
Rigid Body: Rotational and Translational Motion; Rolling without Slipping 8.01 W11D1 Today’s Reading Assignment Young and Freedman: 10.3.
Rigid Body: Rotational and Translational Motion; Rolling without Slipping 8.01 W11D1 Today’s Reading Assignment Young and Freedman:
Presentation transcript:

François Chevoir, Jean-Noël Roux Laboratoire Navier (LCPC, ENPC, CNRS) DENSE GRANULAR MATERIALS Microscopic origins of macroscopic behaviour GdR CHANT Ecole Nationale des Ponts et Chaussées Cité Descartes, Nov. 2007

GRANULAR MATERIALS Variety of material nature, properties, uses… Assemblies of solid objects interacting at their contacts

OUTLINE 1. Macroscopic aspects: known properties and phenomena, simple modelling schemes 2. Microscopic models for grains and contacts 3. Some connections between 1 and 2 for solidlike granular assemblies 4. Dense granular flows

Macroscopic behaviour of granular materials. Phenomenological description Internal friction and dilatancy Density and structure of packings Constitutive law Elasticity Strain localization

INTERNAL FRICTION On any plane cut through the material, shear component  of stress vector .n limited as Internal friction angle A slope inclined at angle cannot be stable With z = normal to free surface, x = along slope, assuming all derivatives vanish except w.r.t. z, use:

DILATANCY Deviatoric and volumetric strains couple Dense assemblies have to dilate to get sheared (grains packs in flexible membrane under vacuum are rigid) In simple shear define dilatancy angle Classically invoked picture: 2 nd row moves up, slope angle 

See other document (pdf) for more on macroscopic behavior

Contact law: normal elastic force Normal contact force between smooth objects: Hertz law d h  d = effective diameter (sphere diameter if identical)  h = normal deflection of contact  E,  Young modulus and Poisson ratio  Valid for smooth objects   radius of contact region prop. to

Contact law: tangential elasticity and friction Tangential ‘elastic’ force is history-dependent,to be dealt with incrementally Stiffness at zero tangential relative displacement : Coulomb condition: Apply condition locally for force density on surface History-dependent slip and no-slip regions within contact surface with

History dependence of contact law: Even without any sliding zone within contact surface ! (Elata and Berryman, Mechanics of Materials, 24, )

Simplified contact law. Thermodynamic consistence Keep = u T -independent ? increase in stored elastic energy in tangential elasticity in case of a receding normal relative motion Rescale F T when F N is reduced ( proportionnally to stiffness)

Further simplification: linear unilateral elasticity Use constantand Keep correct order of magnitude for normal deflection h or Assume rigid, undeformable contacts and penalize impenetrability constraints. Motivation: Definition and use of limit of rigid contacts ?

Contact forces in rolling and pivoting. Objectivity Tangential elastic/frictional forces are not determined by current position/orientation of grains. Evolution for arbitrary motions ? Rolling = rotation about axis in tangential plane Pivoting = rotation about normal axis Possible rule for tangential force: 1. Follow rolling motion of normal vector n 2. Rotate about n with average angular velocity of the 2 solids Ensures objectivity. (e.g. tangential force should follow global rigid body motion) (Most often, rule 1 is adopted – without discussion - but not rule 2 !) u T constant

Viscous part of contact law. Damping, restitution. Add viscous terms in contact forces, opposing relative motion at contact point : With linear elasticity, a pair in contact is a damped harmonic oscillator If not overdamped, restitution coefficients e N,T relate to ratio  N,T of damping coefficient to critical value (e.g. ) as In Hertzian case, similar definition possible with tangent stiffnesses K N,T Ad-hoc parameters, little physical justification Coulomb condition: includes viscous terms ? Yes  forbid traction. No  viscous fluid ?

Remarks on contact laws Strong stress concentration in contacts (worse for angular contacts) In experimental practice, only measured or controlled with relatively large, regular-shaped bodies Dissipative part of contact law ??? Tempting to use rigid contacts… But other approach is needed then … and what about macroscopic elasticity ? Necessary anyway to systematically assess parameter influence

See other document (pdf) for part III, about micro/macro connections for solidlike granular materials