Pattern Formation Dynamics in Tapped Granular Media

2003 ◽  
Author(s):  
Y. K. Goh
2017 ◽  
Vol 3 (1) ◽  
Author(s):  
Eric Opsomer ◽  
Martial Noirhomme ◽  
Nicolas Vandewalle ◽  
Eric Falcon ◽  
Simon Merminod

Fractals ◽  
1993 ◽  
Vol 01 (04) ◽  
pp. 968-976 ◽  
Author(s):  
E. LEMAIRE ◽  
Y. OULD MOHAMED ABDELHAYE ◽  
J. LARUE ◽  
R. BENOIT ◽  
P. LEVITZ ◽  
...  

We studied pattern formation in granular media in two distinct states: in the dry and non-cohesive (powder) state, on the one hand, and in the wet and cohesive (paste) state, on the other. In the first case, we have shown that gas injection in a thin layer of powder within a Hele Shaw cell leads to fractal patterns remarkably similar to viscous fingering patterns obtained with complex fluids. In the second case, we have shown that the tensile cohesive viscoplastic fracture of a layer of paste leads to self-affine rough surfaces with a Hurst exponent close to 0.88, very close to the value obtained for fragile fracture by other authors.18 Our observations reinforce the universality of two fractal growth processes and add a new element to the ambivalent nature of the granular state of matter.


Soft Matter ◽  
2014 ◽  
Vol 10 (38) ◽  
pp. 7459-7467 ◽  
Author(s):  
Pedro H. A. Anjos ◽  
José A. Miranda

We study the pattern formation dynamics related to the displacement of a viscous wetting fluid by a less viscous nonwetting fluid in a lifting Hele-Shaw cell.


Author(s):  
Alison Ord ◽  
Bruce E. Hobbs

Naturally, deformed rocks commonly contain crack arrays (joints) forming patterns with systematic relationships to the large-scale deformation. Kinematically, joints can be mode-1, -2 or -3 or combinations of these, but there is no overarching theory for the development of the patterns. We develop a model motivated by dislocation pattern formation in metals. The problem is formulated in one dimension in terms of coupled reaction–diffusion equations, based on computer simulations of crack development in deformed granular media with cohesion. The cracks are treated as interacting defects, and the densities of defects diffuse through the rock mass. Of particular importance is the formation of cracks at high stresses associated with force-chain buckling and variants of this configuration; these cracks play the role of ‘inhibitors’ in reaction–diffusion relationships. Cracks forming at lower stresses act as relatively mobile defects. Patterns of localized deformation result from (i) competition between the growth of the density of ‘mobile’ defects and the inhibition of these defects by crack configurations forming at high stress and (ii) the diffusion of damage arising from these two populations each characterized by a different diffusion coefficient. The extension of this work to two and three dimensions is discussed.


1994 ◽  
pp. 563-571
Author(s):  
E. LEMAIRE ◽  
Y. OULD MOHAMED ABDELHAYE ◽  
J. LARUE ◽  
R. BENOIT ◽  
P. LEVITZ ◽  
...  

1996 ◽  
Vol 36 (4) ◽  
pp. 247-252 ◽  
Author(s):  
S Luding ◽  
E Clément ◽  
J Rajchenbach ◽  
J Duran

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