Dynamics of dense sheared granular flows. Part 1. Structure and diffusion

被引:30
|
作者
Kumaran, V. [1 ]
机构
[1] Indian Inst Sci, Dept Chem Engn, Bangalore 560012, Karnataka, India
关键词
INELASTIC COLLAPSE; SELF-DIFFUSION; KINETIC-THEORY; SUSPENSIONS; GAS; MICROSTRUCTURE; PARTICLES; RHEOLOGY; SPHERES; DECAY;
D O I
10.1017/S0022112009006776
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Shear flows of inelastic spheres in three dimensions in the Volume fraction range 0.4-0.64 are analysed using event-driven simulations. Particle interactions are considered to be due to instantaneous binary collisions, and the collision model has a normal coefficient of restitution e(n) (negative of the ratio of the post- and pre-collisional relative velocities of the particles along the line joining the centres) and a tangential coefficient of restitution e(t) (negative of the ratio of post- and pre-collisional velocities perpendicular to the line Joining the centres). Here, we have considered both e(t) = +1 and e(t) = e(n) (rough particles) and e(t) = -1 (smooth particles), and the normal coefficient of restitution e(n) was varied in the range 0.6-0.98. Care was taken to avoid inelastic collapse and ensure there are no particle overlaps during the simulation. First, we studied the ordering in the system by examining the icosahedral order parameter Q(6) in three dimensions and the planar order parameter q(6) in the plane perpendicular to the gradient direction. It was found that for shear flows of sufficiently large size, the system Continues to be in the random state, with Q(6) and q(6) close to 0, even for volume fractions between phi = 0.5 and phi = 0.6; in contrast, for a system of elastic particles in the absence of shear, the system orders (crystallizes) at phi = 0.49. This indicates that the shear flow prevents ordering in a system of sufficiently large size. In a shear flow of inelastic particles, the strain rate and the temperature are related through the energy balance equation, and all time scales can be non-dimensionalized by the inverse of the strain rate. Therefore, the dynamics of the system are determined only by the volume fraction and the coefficients of restitution. The variation of the collision frequency with volume fraction and coefficient of restitution was examined. It was found, by plotting the inverse of the collision frequency as a function of volume fraction, that the collision frequency at constant strain rate diverges at a volume fraction phi(ad) (volume fraction for arrested dynamics) which is lower than the random close-packing Volume fraction 0.64 in the absence of shear. The volume fraction phi(ad) decreases as the coefficient of restitution is decreased from e(n) = 1; phi(ad) has a minimum of about 0.585 for coefficient of restitution e(n) in the range 0.6-0.8 for rough particles and is slightly larger for smooth particles. It is found that the dissipation rate and all components of the stress diverge proportional to the collision frequency in the close-packing limit. The qualitative behaviour of the increase in the stress and dissipation rate are well Captured by results derived from kinetic theory, but the quantitative agreement is lacking even if the collision frequency obtained from simulations is used to calculate the pair correlation function used In the theory.
引用
收藏
页码:109 / 144
页数:36
相关论文
共 50 条
  • [2] Rheology of dense sheared granular flows
    Kumaran, V.
    XVTH INTERNATIONAL CONGRESS ON RHEOLOGY - THE SOCIETY OF RHEOLOGY 80TH ANNUAL MEETING, PTS 1 AND 2, 2008, 1027 : 920 - 922
  • [3] Structure and dynamics of two-dimensional sheared granular flows
    Reddy, K. Anki
    Kumaran, V.
    PHYSICAL REVIEW E, 2009, 79 (06):
  • [4] On the Velocity Gradient in Stably Stratified Sheared Flows. Part 1: Asymptotic Analysis and Applications
    Zilitinkevich, S. S.
    Esau, I.
    Kleeorin, N.
    Rogachevskii, I.
    Kouznetsov, R. D.
    BOUNDARY-LAYER METEOROLOGY, 2010, 135 (03) : 505 - 511
  • [5] On the Velocity Gradient in Stably Stratified Sheared Flows. Part 1: Asymptotic Analysis and Applications
    S. S. Zilitinkevich
    I. Esau
    N. Kleeorin
    I. Rogachevskii
    R. D. Kouznetsov
    Boundary-Layer Meteorology, 2010, 135 : 505 - 511
  • [6] Scaling laws for segregation forces in dense sheared granular flows
    Guillard, Francois
    Forterre, Yoel
    Pouliquen, Olivier
    JOURNAL OF FLUID MECHANICS, 2016, 807 : R1
  • [7] Complex flow dynamics in dense granular flows Part II: Simulations
    Zamankhan, Piroz
    PROCEEDINGS OF THE ASME FLUIDS ENGINEERING DIVISION SUMMER CONFERENCE - 2005, VOL 1, PTS A AND B, 2005, : 551 - 570
  • [8] Complex flow dynamics in dense granular flows - Part II: Simulations
    Zamankhan, Piroz
    Jun, Huang
    Journal of Applied Mechanics, Transactions ASME, 2007, 74 (04): : 691 - 702
  • [9] Complex flow dynamics in dense granular flows Part I: Experimentation
    Zamankhan, Piroz
    PROCEEDINGS OF THE ASME FLUIDS ENGINEERING DIVISION SUMMER CONFERENCE - 2005, VOL 1, PTS A AND B, 2005, : 539 - 550
  • [10] Complex flow dynamics in dense granular flows - Part I: Experimentation
    Zamankhan, Piroz
    Bordbar, Mohammad Hadi
    JOURNAL OF APPLIED MECHANICS-TRANSACTIONS OF THE ASME, 2006, 73 (04): : 648 - 657