Approach to failure in porous granular materials under compression.
We investigate the approach to catastrophic failure in a model porous granular material undergoing uniaxial compression. A discrete element computational model is used to simulate both the microstructure of the material and the complex dynamics and feedbacks involved in local fracturing and the production of crackling noise. Under strain-controlled loading, microcracks initially nucleate in an uncorrelated way all over the sample. As loading proceeds the damage localizes into a narrow damage band inclined at 30°-45° to the load direction. Inside the damage band the material is crushed into a poorly sorted mixture of mainly fine powder hosting some larger fragments. The mass probability density distribution of particles in the damage zone is a power law of exponent 2.1, similar to a value of 1.87 inferred from observations of the length distribution of wear products (gouge) in natural and laboratory faults. Dynamic bursts of radiated energy, analogous to acoustic emissions observed in laboratory experiments on porous sedimentary rocks, are identified as correlated trails or cascades of local ruptures that emerge from the stress redistribution process. As the system approaches macroscopic failure consecutive bursts become progressively more correlated. Their size distribution is also a power law, with an equivalent Gutenberg-Richter b value of 1.22 averaged over the whole test, ranging from 3 to 0.5 at the time of failure, all similar to those observed in laboratory tests on granular sandstone samples. The formation of the damage band itself is marked by a decrease in the average distance between consecutive bursts and an emergent power-law correlation integral of event locations with a correlation dimension of 2.55, also similar to those observed in the laboratory (between 2.75 and 2.25).
Department of Theoretical Physics, University of Debrecen, P. O. Box 5, H-4010 Debrecen, Hungary.
Ferenc
F
Kun
Department of Informatics Systems and Networks, University of Debrecen, P. O. Box 12, H-4010 Debrecen, Hungary.
Imre
I
Varga
School of Geosciences, University of Edinburgh, EH9 3JL Edinburgh, United Kingdom and Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany.
Sabine
S
Lennartz-Sassinek
School of Geosciences, University of Edinburgh, EH9 3JL Edinburgh, United Kingdom.
Ian G
IG
Main