This paper describes a series of experiments designed to investigate the fall of granular columns in a quasi-static regime. Columns made of alternatively green and red sand layers were initially laid out in a box and then released when a retaining wall was set in slow motion with constant speed. The dependence of the dynamics of the fall on the initial aspect ratio of the columns, the velocity of the wall, and the material properties was investigated within the quasi-static regime. A change in the behavior of the columns was identified to be a function of the aspect ratio (height/length) of the initial sand column. Columns of high aspect ratio first subsided before sliding along failure planes, while columns of small aspect ratio were only observed to slide along failure planes. The transition between these two characteristic falls occurred regardless of the material and the velocity of the wall in the context of the quasi-static regime. When the final height and length of the piles were analyzed, we found power-law relations of the ratio of initial to final height and final run-out to initial length with the aspect ratio of the column. The dissipation of energy is also shown to increase with the run-out length of the pile until it reaches a plateau. Finally, we find that the structure of the slip planes that develop in our experiments are not well described by the failure of Coulomb’s wedges for twin retaining rough walls.
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September 2006
Research Article|
September 05 2006
Two dimensional fall of granular columns controlled by slow horizontal withdrawal of a retaining wall
Catherine Mériaux
Catherine Mériaux
Epsilon Laboratory, School of Mathematical Sciences and MC2,
Monash University
, 3800 Victoria, Australia
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Physics of Fluids 18, 093301 (2006)
Article history
Received:
April 21 2006
Accepted:
July 10 2006
Citation
Catherine Mériaux; Two dimensional fall of granular columns controlled by slow horizontal withdrawal of a retaining wall. Physics of Fluids 1 September 2006; 18 (9): 093301. https://doi.org/10.1063/1.2335477
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