scholarly journals Discussion: Fully Developed Plastic Shear Flow of Granular Materials

Géotechnique ◽  
1971 ◽  
Vol 21 (2) ◽  
pp. 190-192 ◽  
Author(s):  
A. J. M. Spencer
Géotechnique ◽  
1970 ◽  
Vol 20 (3) ◽  
pp. 277-307 ◽  
Author(s):  
G. Mandl ◽  
R. Fernández Luque

1983 ◽  
Vol 29 (102) ◽  
pp. 283-285 ◽  
Author(s):  
Thomas Scheiwiller ◽  
Kolumban Hutter

Abstract The paper of which this is an extended abstract reviews theoretical formulations for flow and airborne powder-snow avalanches. First powder-snow avalanches are considered as plane turbulent gravity currents. Then we propose a two-phase model describing powder-snow avalanches as turbulent binary mixtures of snow granules and air. An analogy is postulated between flow avalanches and the rapid shear flow of granular materials which leads to a non-polar continuum with microstructure taking into account the fluctuation energy of the snow granules.


1999 ◽  
Vol 397 ◽  
pp. 203-229 ◽  
Author(s):  
P. R. NOTT ◽  
M. ALAM ◽  
K. AGRAWAL ◽  
R. JACKSON ◽  
S. SUNDARESAN

The tendency of granular materials in rapid shear ow to form non-uniform structures is well documented in the literature. Through a linear stability analysis of the solution of continuum equations for rapid shear flow of a uniform granular material, performed by Savage (1992) and others subsequently, it has been shown that an infinite plane shearing motion may be unstable in the Lyapunov sense, provided the mean volume fraction of particles is above a critical value. This instability leads to the formation of alternating layers of high and low particle concentrations oriented parallel to the plane of shear. Computer simulations, on the other hand, reveal that non-uniform structures are possible even when the mean volume fraction of particles is small. In the present study, we have examined the structure of fully developed layered solutions, by making use of numerical continuation techniques and bifurcation theory. It is shown that the continuum equations do predict the existence of layered solutions of high amplitude even when the uniform state is linearly stable. An analysis of the effect of bounding walls on the bifurcation structure reveals that the nature of the wall boundary conditions plays a pivotal role in selecting that branch of non-uniform solutions which emerges as the primary branch. This demonstrates unequivocally that the results on the stability of bounded shear flow of granular materials presented previously by Wang et al. (1996) are, in general, based on erroneous base states.


2006 ◽  
Vol 169 (1) ◽  
pp. 10-21 ◽  
Author(s):  
Lee Aarons ◽  
Sankaran Sundaresan

Author(s):  
V. N. Dolgunin ◽  
O. O. Ivanov ◽  
S. A. Akopyan

Phenomenological approaches to describing the rheological behavior of granular materials under conditions of rapid and quasi-plastic shear deformations are considered. A unified approach to the phenomenological-logical description of the physical parameter, called the temperature of the granular medium, and the mechanisms of shear stress generation is proposed. A description is given of the mechanism for generating shear stresses under the action of a flow of pulses directed along the shear rate gradient and caused by transverse quasi-diffusion of particles. This mechanism is taken into account in the rheological model in addition to the traditional mechanism of generating kinetic shear stresses under the action of tangential shock pulses.


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