Stress and fabric in granular material

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

Micromechanics-based model for cement-treated clays

A micromechanical approach to describe internal erosion effects in soils

Ch 5 Strength and Stiffness of Sands

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

Radial Growth of a Micro-Void in a Class of. Compressible Hyperelastic Cylinder. Under an Axial Pre-Strain *

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

Particle flow simulation of sand under biaxial test

Numerical Simulations of Triaxial Test with Sand Using DEM

Quasistatic behavior and force transmission in packing of irregular polyhedral particles

Module 4 Lecture 20 Pore water pressure and shear strength - 4 Topics

MICROMECHANICAL CONSIDERATIONS OF PARTICLE BREAKAGE USING DISCRETE ELEMENT METHOD

Micromechanics of granular materials: slow flows

Determination of Poisson s Ratio of Rock Material by Changing Axial Stress and Unloading Lateral Stress Test

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

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

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

Distinct simulation of earth pressure against a rigid retaining wall considering inter-particle rolling resistance in sandy backfill

A comparison of discrete granular material models with continuous microplane formulations

Theory of Shear Strength

Experimental Validation of Particle-Based Discrete Element Methods

Huang, X; Hanley, K; O'Sullivan, C; Kwok, CY; Tham, LG

Bimodal Character of Stress Transmission in Granular Packings

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

Research Article Micromechanical Formulation of the Yield Surface in the Plasticity of Granular Materials

DEM SIMULATIONS OF DRAINED AND UNDRAINED BEHAVIOUR GUOBIN GONG

1. Background. is usually significantly lower than it is in uniaxial tension

A DISCRETE NUMERICAL MODEL FOR STUDYING MICRO-MECHANICAL RELATIONSHIP IN GRANULAR ASSEMBLIES CE-390

INTERPRETATION OF UNDRAINED SHEAR STRENGTH OF UNSATURATED SOILS IN TERMS OF STRESS STATE VARIABLES

Numerical Assessment of the Influence of End Conditions on. Constitutive Behavior of Geomaterials

Three-Dimensional Discrete Element Simulations of Direct Shear Tests

Lecture #7: Basic Notions of Fracture Mechanics Ductile Fracture

Granular Mechanics of Geomaterials (presentation in Cassino, Italy, 2006)

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

THE INTERPRETATION OF LABORATORY SOIL TESTS

Study on the Microstructure and Load Bearing Properties of Granular Material

SHEAR STRENGTH OF SOIL

Effect of embedment depth and stress anisotropy on expansion and contraction of cylindrical cavities

Changes in soil deformation and shear strength by internal erosion

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

MATHEMATICAL AND NUMERICAL MODEL OF ROCK/CONCRETE MECHANICAL BEHAVIOR IN A MULTI-PLANE FRAMEWORK

SHEAR STRENGTH OF SOIL

With high enough plate forces in opposite directions Bolts. How do these fail? Each pin has sheared into two pieces.

Hypoplastic Cam-clay model

A discrete element analysis of elastic properties of granular materials

SHEAR STRENGTH OF SOIL UNCONFINED COMPRESSION TEST

Experimental and numerical studies of load transfers and arching effect in the trap-door problem

Micro-macro Modeling of Particle Crushing Based on Branch Lengths. Esmaeel Bakhtiary 1, and Chloé Arson 2

Theory of Shear Strength

4 Undrained Cylindrical Cavity Expansion in a Cam-Clay Medium

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

Ch 4a Stress, Strain and Shearing

Temperature Dependent Mechanical Properties of Reservoir s Overburden Rocks During SAGD Process

PLASTICITY FOR CRUSHABLE GRANULAR MATERIALS VIA DEM

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

Constitutive modelling of fabric anisotropy in sand

Micromechanics of breakage in sharp-edge particles using combined DEM and FEM

Evaluation of undrained response from drained triaxial shear tests: DEM simulations and Experiments

POST-LIQUEFACTION STATE OF SAND, STRESS CORROSION CRACKING, AND RELAXATION OF DEVIATORIC STRESS IN PREVIOUSLY LIQUEFIED SAND BED

A rate-dependent Hosford-Coulomb model for predicting ductile fracture at high strain rates

Mechanics of Materials II. Chapter III. A review of the fundamental formulation of stress, strain, and deflection

Soil Mechanics: Limitations and Future Directions

STRESS DROP AS A RESULT OF SPLITTING, BRITTLE AND TRANSITIONAL FAULTING OF ROCK SAMPLES IN UNIAXIAL AND TRIAXIAL COMPRESSION TESTS

Cavity Expansion Methods in Geomechanics

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

Advanced Structural Analysis EGF Cylinders Under Pressure

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.

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

Simulation of the cutting action of a single PDC cutter using DEM

Numerical modeling of standard rock mechanics laboratory tests using a finite/discrete element approach

Effects of abrasion on the penetration of ogival-nosed projectiles into concrete targets

Mechanics PhD Preliminary Spring 2017

Classical fracture and failure hypotheses

Geng, Yan (2010) Discrete element modelling of cavity expansion in granular materials. PhD thesis, University of Nottingham.

(MPa) compute (a) The traction vector acting on an internal material plane with normal n ( e1 e

A Phenomenological Model of Brittle Rocks under Uniaxial Compression

Chapter 5 Shear Strength of Soil

Micro-macro modelling for fluids and powders

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

Drained Against Undrained Behaviour of Sand

INFLUENCE OF WATER-SOAKING TIME ON THE ACOUSTIC EMISSION CHARACTERISTICS AND SPATIAL FRACTAL DIMENSIONS OF COAL UNDER UNIAXIAL COMPRESSION

Finite Element Method in Geotechnical Engineering

The Mine Geostress Testing Methods and Design

1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION 1.5 STRESS-PATH METHOD OF SETTLEMENT CALCULATION

Discrete Element Modelling of a Reinforced Concrete Structure

Using the Timoshenko Beam Bond Model: Example Problem

Finite Element analysis of Laterally Loaded Piles on Sloping Ground

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

Numerical Simulation of Unsaturated Infilled Joints in Shear

Strength of Material. Shear Strain. Dr. Attaullah Shah

Cementing Material on Mechanical Property of Calcareous Sand

Laboratory Testing Total & Effective Stress Analysis

VORONOI APPLIED ELEMENT METHOD FOR STRUCTURAL ANALYSIS: THEORY AND APPLICATION FOR LINEAR AND NON-LINEAR MATERIALS

Failure Mechanism and Evolution Law of Fractured-Rocks based on Moment Tensor Inversion

Pressure Vessels Stresses Under Combined Loads Yield Criteria for Ductile Materials and Fracture Criteria for Brittle Materials

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

Technical Note 16 Equivalent Static Method

Chapter (12) Instructor : Dr. Jehad Hamad

General method for simulating laboratory tests with constitutive models for geomechanics

A FAILURE CRITERION FOR POLYMERS AND SOFT BIOLOGICAL MATERIALS

Transcription:

THEORETICAL & APPLIED MECHANICS LETTERS 3, 22 (23) Stress and fabric in granular material Ching S. Chang,, a) and Yang Liu 2 ) Department of Civil Engineering, University of Massachusetts Amherst, Massachusetts 3, USA 2) Department of Civil Engineering, University of Science and Technology, Beijing 83, China (Received 6 December 22; accepted 7 January 23; published online March 23) Abstract It has been well recognized that, due to anisotropic packing structure of granular material, the true stress in a specimen is different from the applied stress. However, very few research efforts have been focused on quantifying the relationship between the true stress and applied stress. In this paper, we derive an explicit relationship among applied stress tensor, material-fabric tensor, and force-fabric tensor; and we propose a relationship between the true stress tensor and the applied stress tensor. The validity of this derived relationship is examined by using the discrete element simulation results for granular material under biaxial and triaxial loading conditions. c 23 The Chinese Society of Theoretical and Applied Mechanics. [doi:.63/2.322 Keywords stress tensor, force fabric tensor, material fabric tensor, granular material, discrete element method For granular material, as a discrete system, the applied stress transmits to the material in a form of force-chains through the particles of an assembly. The patterns of force-chains (force-fabric) vary with packing structures (material-fabric), and are important factors that govern the deformation behavior of the granular material. To account for the effect of material-fabric, a concept of true stress can be utilized, which is a continuum analog of the force chains. Different from the applied stress, the true stress depends on the packing structure and directly governs the deformation and strength of the material. Therefore, the relationships among applied stress, true stress, material-fabric, and force-fabric are very useful for the development of a stress strain model for granular material. In the literature, there are many studies on the material-fabric and the force-fabric of a granular material. 2 The concept of true stress has also been used for many years in the analysis of damaged brittle material. 2 4 However, very few efforts have been devoted to the use of true stress in modeling of granular material. In this paper, we derive an explicit form that relates stress, force-fabric and material-fabric under triaxial loading conditions, and suggest a formula for estimating true stress in granular material. The formula is then examined through discrete element simulation results for both biaxial and triaxial tests. The material-fabric of a packing is characterized by the distribution of inter-particle contact orientations, which can be expressed by a harmonic Fourier expansion in a spherical coordinate system. The commonly used formula is a simplified form by truncating the Fourier expansion to include only up to second order terms ξ(θ, β) = [ + a (3 cos 2θ + ) + 4π 4 a) Corresponding author. Email: chang@ecs.umass.edu. 3b sin 2 θ cos 2β, () in which the angles θ and β are defined in Fig., a and b are two constants of the material-fabric. The distribution function is a probability density function, given by ξ(θ, β) sin θ d θ d β =. (2) The auxiliary local coordinate system at each contact consists of three orthogonal vectors n, s, t, which are defined as n = cos θi + sin θ cos βj + sin θ sin βk, s = sin θi cos θ cos βj sin β cos θk, t = sin βj cos βk. (3) Equation () can be written alternatively as a Cartesian tensor equation ξ(n) = 4π D ijn i n j, (4) where D ij is termed as contact density vector component, defined as + a D = a/2 + 3b. (5) a/2 3b Aside from the contact density tensor, another commonly used measure for material-fabric is termed fabric vector component, and defined as F ij = n c N in c j. (6) c In terms of integrate form, we can rewrite Eq. (6) as F ij = ξ(θ, β) n i n j sin θ d θ d β. (7)

22-2 C. S. Chang, and Y. Liu Theor. Appl. Mech. Lett. 3, 22 (23) x f(θ) = f ( + a n cos 2θ), f t (θ) = fa t sin 2θ. (3) y β θ s n t n z The contact density tensor, force-fabric tensor, and material-fabric tensor are [ + a D =, a [ + a n A =, a n [ F = 2 + a. (4) 2 2 a Fig.. Local coordinate system at an inter-particle contact. Using the density function defined in Eq. (), the following expression can be derived F = 5 + 2a 5 a + 6b. (8) 5 5 a 6b The pattern of contact force (or force-fabric) is characterized by the orientation distribution of the contact forces. There are three components of contact forces in the n, s, t directions. Distributions for the three force components, observed from the results of discrete element simulation, can be defined as follows f n = fa ij n i n j, f s = a s faij n i s j, f t = a t faij n i t j, (9) where the mean force and the force-fabric tensor respectively are f = 4π A = s t f n sin θ d θ d β, () + a n a n 2 + 3b n a n 2 3b n. () The constants a n, b n, a s and a t define the distributions of force-fabric. For a two-dimensional condition, the distribution function for material-fabric and force-fabric can be reduced to the following form ξ(θ) = ( + a cos 2θ), (2) 2π The Cauchy stress tensor for granular material with volume V can be expressed as a summation of the dyadic product of force and branch vector components over all contacts in the volume σ ij = li c fj c. (5) V c The branch vector component li c is defined as the vector joining the centroids of two contact particles. By assuming spherical particles with average length of branch vector, expressing the force vector in terms of its three components, and substituting the forces with the force-fabric tensor expressions in Eq. (9), the following form can be obtained where σ ij = A pq D mn T ijpqmn, (6) T ijpqmn = m v l f a t n p t q t i n j )n m n n sin θ d θ d β, (n p n q n i n j + a s n p s q s i n j + where m v is the total number of contacts per volume. This relationship among stress tensor, material-fabric tensor and force-fabric tensor is applicable to any types of external leading conditions. The main assumptions are that the distribution of material-fabric and forcefabric can be approximated by the second order harmonic Fourier expansion as given in Eqs. () and (3), and the correlations between branch vector and force vector are neglected. Equation (6) is examined by discrete element simulation results for biaxial tests and triaxial tests. For a three-dimensional axisymmetric condition, b = in the material-fabric tensor and b n = in the force-fabric tensor. Using Eq. (6), the stress ratio can be expressed by the material-fabric and force-fabric constants, given by σ a σ r = σ a + 2σ r 5 a + 5 a n + 2 5 a t + 5 aa n + 6 5 aa t + 2 5 aa n 5 a + 5 a n + 2 5 a t. (7)

22-3 Stress and fabric in granular material Theor. Appl. Mech. Lett. 3, 22 (23) For biaxial test conditions, using Eq. (6), the stress ratio can be expressed by the material-fabric and forcefabric constants, given by σ x σ y = (a + a n + a t )/2 σ x + σ y + aa n /2 2 (a + a n + a t ), (8) this equation has the same form as that given in Rothenburg and Bathurst. 4 A series of biaxial tests were performed on assemblage of discs using particle flow code in 2 dimensions (PFC2D). Dense sample consists of 4 6 frictional discs and loose sample 3 797 particles, both with uniform size distribution (.75. m particle radii). The porosity in loose and dense sample is chosen as.7 and.3, respectively. The density of discs is chosen to be 2 63 kg/m 3, normal and tangential contact stiffness are both MN/m, and the coefficient of friction is.5. Biaxial compression tests were carried out by isotropically compressing the specimen to. MPa, then keeping horizontal stress constant and applying a strain rate in the vertical direction. The results for the initial isotropic stress state (see point A in Fig. 2) are plotted in Fig. 3(a). The materialfabric is shown in Fig. 3(a), the normal contact force distribution is shown in Fig. 3(a2), and the tangential contact force distribution is in Fig. 3(a3). The results for the peak stress state (see point B in Fig. 2) are plotted in Fig. 3(b). The material-fabric is shown in Fig. 3(b), the normal contact force distribution is in Fig. 3(b2), and the tangential contact force distribution is in Fig. 3(b3). The evolution of material-fabric constants and force-fabric constants during the loading is shown in Fig. 4 for both dense and loose samples. The symbols represent the fabric constants at different loading states. The comparison of Eq. (8) with that obtained from the discrete element simulation is shown in Fig. 2, which indicates a good agreement. For triaxial test, the spherical particles were generated within a cylinder, consisting of 2 2 frictional spheres, with uniform size distribution of.75. m sphere radii. The density is 2 63 kg/m 3, normal and tangential contact stiffness are both MN/m and the coefficient of friction is.5. Triaxial compression tests were carried out by keeping radial stress constant and applying a strain rate in the other direction after isotropic compression of the specimen under. MPa. The fabric plots for the peak stress state (see point A in Fig. 5) are shown in Fig. 6. The material-fabric is in Fig. 6(a), the normal contact force distribution is in Fig. 6(a2), and the tangential contact force distribution is in Fig. 6(a3). The evolution of the material-fabric and the forcefabric constants during loading are shown in Fig. 7. The comparison of Eq. (7) and that obtained from discrete element simulation results is shown in Fig. 5, which indicates that Eq. (7) is applicable to the triaxial loading conditions. (σ σ2)/(σ+σ2).6.4.2 B Dense sample Loose sample A (a+a n +a t )/2 4 8 2 Axial strain Fig. 2. Biaxial stress strain curves obtained from discrete element simulations. The analyses discussed above demonstrate that the applied stress is partly carried by the anisotropic packing structure and partly carried by the frictional resistance capacity of the material. The second part of the stress is termed as true stress, which mobilize the frictional resistance of the material. Thus, the true stress governs the deformation and strength of the material. For Coulomb friction material, the mobilized friction angle by the true stress is given by = + sin φ m sin φ. (9) m As the mobilized friction angle exceeds the friction capacity of the material, the material fails. The concept of true stress has been used for many years in the field of damage mechanics to model brittle materials with fractural damage. 2 4 However, very few efforts have been devoted to the use of true stress concept for modeling of granular material. Here, we propose a formula that shows the relationship between the true stress and the applied stress in the following form σ ij = 3F ik σ kj, (2) where F ik is the material-fabric tensor component shown in Eq. (8) or in Eq. (4). Using Eq. (2), the true stress ratio, the applied stress ratio, and the materialfabric ratio can be related by = F 33 F. (2) Using Eq. (9), Eq. (2) can be rearranged to the following form F F 33 = κ, κ = sin φ m + sin φ m =. (22) Triaxial or biaxial test results from discrete element simulation can be plotted as a curve in a plane of material-fabric ratio versus stress ratio. Any point on the curve corresponds to a stress state during the test. The slope of the line, connecting a point on the curve and the origin of the coordinate, is denoted as κ,

22-4 C. S. Chang, and Y. Liu Theor. Appl. Mech. Lett. 3, 22 (23).2.2.3.5 -.5 -.2 -.2 -.2.2 -.2.2 -.3 -.5.5 (a) a= (a2) a n = (a3) a t =.3 (a) Isotropic stress state.3.2.2.5 -.5 -.2 -.2 -.3 -.2.2 -.2.2 -.5.5 (b) a=.25 (b2) a n =.45 (b3) a t =.6 (b) Peak stress state Fig. 3. Fabric plots for material, normal contact force and tangential contact force. a an at a an at.4 a a n a t.3.2. 2 4 6 8 (a) Loose sample.6 a a n a t.4.2 2 4 6 8 2 (b) Dense sample Fig. 4. Evolution of material-fabric constants and forcefabric constants for loose and dense samples. (σa σr)/(σa+2σr).6.4.2 (a+a n +a t )/5 2 4 6 8 Fig. 5. Stress strain curve obtained from discrete element simulation for triaxial test. which is related to the mobilized friction angle and true stress ratio. For example, the results of biaxial tests in Fig. 2 are plotted in Fig. 8. For the dense sample case, at peak stress point, the stress ratio is 2.5 (corresponding to a peak friction angle of 26 ). The line connecting the peak point and the origin point has a slope κ, which gives the true stress ratio.9 (corresponding to a mobilized friction angle of 2 ). Thus, for the peak friction angle of 26, 2 is carried by the material friction resistance, and 6 is carried by the anisotropic packing structure. At the residual stress state, the applied stress ratio is.95 (corresponding to a friction angle of 2 ). The true stress ratio at the residual state is.4 (corresponding to a mobilized friction angle of ). It is noted from A

22-5 Stress and fabric in granular material Theor. Appl. Mech. Lett. 3, 22 (23).2.2.5 -.2 -.2.2 a a=.69 -.2 -.2.2 a2 a n =.7 -.5 -.2.2 a3 a t =.65 Fig. 6. Fabric plots for material, contact normal and tangential forces at peak stress state. a an at 2.4.6.8 a a n a t 2 4 6 8 Fig. 7. Evolution of material-fabric and force-fabric constants for triaxial test. F/F22 2 Dense sample Loose sample A: ϕ m ' =Ο κ.5..5 2. 2.5 / κ 2 B: ϕ' m =25Ο Fig. 8. Stress ratio versus material-fabric ratio for loose and dense samples in biaxial test. F/F33 2 Triaxial sample A: ϕ m ' =2Ο κ 2 3 / κ 2 B: ϕ' m =25Ο Fig. 9. Stress ratio versus material-fabric ratio for the sample in triaxial test. Fig. 8 that, while the stress ratio decreases from peak to the residual stress state, the material-fabric ratio continues to increase slightly. Thus, the friction capacity due to the support of anisotropic packing structure is not decreased. On the other hand, the friction capacity due to the friction resistance of the material decreases from 2 to caused by the process of dilation related reduction of granular interlocking. The overall friction angle reduces from 26 (peak state) to 2 (residual state). Similar behavior is also shown in the discrete element simulation results for triaxial case as given in Fig. 9, the value of peak friction angle is 33, and the value of mobilized peak friction angle due to true stress is 25. This 8 difference is supported by the anisotropic packing structure. At the residual state, the friction angle is about 3, and the mobilized friction angle due to true stress is 2. The reduction of material friction resistance from 25 to 2 is due to the reduction of granular interlocking. An explicit expression is derived for the relationship among stress tensor, material-fabric tensor and forcefabric tensor in a triaxial test condition. The comparisons between the derived expression and the discrete element simulation results show a good agreement, which indicates that, the second-order approximations for the distributions of material-fabric and force-fabric are good assumptions. The proposed relationship between true stress and applied stress is examined using the discrete element simulation results to illustrate the influence of anisotropic packing structure on the overall friction capacity. The proposed relationship is potentially useful for further development in modeling of stress strain behavior for granular material. The second author appreciates the financial support of the National Natural Science Foundation of China (57844) and Program for New Century Excellent Talents in University (NCET--579).. M. Oda, I. Koishikawa, and T. Higuchi, Soils and Foundation 8, 25 (978). 2. M. Oda, and H. Nakayama, Journal of Engineering Mechanics, ASCE 5, 89 (989).

22-6 C. S. Chang, and Y. Liu Theor. Appl. Mech. Lett. 3, 22 (23) 3. K. Kanatani, International Journal of Engineering Science 22, 49 (984). 4. L. Rothenburg, and R. J. Bathurst, Geotechnique 39, 6 (989). 5. C. S. Chang, and A. Misra, Journal of Engineering Mechanics 6, 77 (99). 6. C. S. Chang, S. C. Chao, and Y. Chang, International Journal of Solids and Structures 32, 989 (995). 7. L. Rothenburg, and N. P. Kruyt, Journal of the Mechanics and Physics of Solids 57, 634 (29). 8. Y. Yunus, E. Vincensand, and B. Cambou, International Journal for Numerical and Analytical Methods in Geomechanics 34, (2). 9. M. R. Kuhn, Mechanics of Materials 42, 827 (2).. C. Thornton, and L. Zhang, Geotechnique 6, 333 (2).. N. P. Kruyt, Mechanics of Materials 44, 2 (22). 2. V. A. Lubarda, and D. Krajcinovic, Int. J. Solids Structures 3, 2859 (993). 3. C. L. Chow, Y. J. Liu, and A. Asundi, International Journal of Fracture 64, 299 (993). 4. I. Carol, and Z. P. Bazant, International Journal of Solids Structures 34, 387 (997).