TY - JOUR
T1 - Basic mechanical properties of wet granular materials
T2 - A DEM study
AU - Than, Vinh Du
AU - Khamseh, Saeed
AU - Tang, Anh Minh
AU - Pereira, Jean Michel
AU - Chevoir, François
AU - Roux, Jean Noël
N1 - Publisher Copyright:
© 2016 American Society of Civil Engineers.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - Numerical simulations, by the discrete element method (DEM), of a model granular assembly, made of spherical balls, are used to investigate the influence of a small amount of an interstitial wetting liquid, forming capillary bridges between adjacent particles, on two basic aspects of granular material rheology: (1) the plastic response in isotropic compression, and (2) the critical state under monotonic shear strain, and its generalization to steady, inertial flow. Tensile strength F0 = φGa, in contacts between beads of diameter a joined by a small meniscus of a liquid with surface tension G, introduces a new force scale and a new dimensionless control parameter, P* = a2P/F0, for grains of diameter a under confining stress P. Under low P*, as cohesion dominates, capillary cohesion may stabilize very loose structures. Upon increasing pressure P in isotropic compression, such structures gradually collapse. The resulting irreversible compaction is well described by the classical linear relation between log P* and void ratio in some range, until a dense structure forms that retains its stability without cohesion as confinement dominates for large P*. In steady shear flow, with uniform velocity gradient γ ˙ = ∂v1/∂x2 under normal stress P = σ22, the apparent internal friction coefficient, which is defined as μ* = σ12/σ22, depends on P* and inertial number (reduced shear rate) I = γ ˙ √m/aP p , and so does solid fraction Φ. The material exhibits, as P* decreases, a strongly enhanced resistance to shear (larger μ*). In the quasistatic limit, for I → 0, it is roughly predicted by a simple effective pressure assumption by which the capillary forces are deemed equivalent to an isotropic pressure increase applied to the dry material as long as P* ≥ 1, while the yield criterion approximately assumes the Mohr-Coulomb form. At lower P*, such models tend to break down as liquid bonding, causing connected clusters to survive over significant strain intervals, strongly influences the microstructure. Systematic shear banding is observed at very small P*.
AB - Numerical simulations, by the discrete element method (DEM), of a model granular assembly, made of spherical balls, are used to investigate the influence of a small amount of an interstitial wetting liquid, forming capillary bridges between adjacent particles, on two basic aspects of granular material rheology: (1) the plastic response in isotropic compression, and (2) the critical state under monotonic shear strain, and its generalization to steady, inertial flow. Tensile strength F0 = φGa, in contacts between beads of diameter a joined by a small meniscus of a liquid with surface tension G, introduces a new force scale and a new dimensionless control parameter, P* = a2P/F0, for grains of diameter a under confining stress P. Under low P*, as cohesion dominates, capillary cohesion may stabilize very loose structures. Upon increasing pressure P in isotropic compression, such structures gradually collapse. The resulting irreversible compaction is well described by the classical linear relation between log P* and void ratio in some range, until a dense structure forms that retains its stability without cohesion as confinement dominates for large P*. In steady shear flow, with uniform velocity gradient γ ˙ = ∂v1/∂x2 under normal stress P = σ22, the apparent internal friction coefficient, which is defined as μ* = σ12/σ22, depends on P* and inertial number (reduced shear rate) I = γ ˙ √m/aP p , and so does solid fraction Φ. The material exhibits, as P* decreases, a strongly enhanced resistance to shear (larger μ*). In the quasistatic limit, for I → 0, it is roughly predicted by a simple effective pressure assumption by which the capillary forces are deemed equivalent to an isotropic pressure increase applied to the dry material as long as P* ≥ 1, while the yield criterion approximately assumes the Mohr-Coulomb form. At lower P*, such models tend to break down as liquid bonding, causing connected clusters to survive over significant strain intervals, strongly influences the microstructure. Systematic shear banding is observed at very small P*.
KW - Capillary forces
KW - Cohesion
KW - Effective pressure
KW - Granular materials
KW - Mohr-Coulomb
KW - discrete element method (DEM)
UR - https://www.scopus.com/pages/publications/85007173278
U2 - 10.1061/(ASCE)EM.1943-7889.0001043
DO - 10.1061/(ASCE)EM.1943-7889.0001043
M3 - Article
AN - SCOPUS:85007173278
SN - 0733-9399
VL - 143
JO - Journal of Engineering Mechanics
JF - Journal of Engineering Mechanics
IS - 1
M1 - C4016001
ER -