University of Debrecen

Department of Theoretical Physics


H-4010 Debrecen, P.O.Box 5, Hungary

E-mail: ferenc.kun@science.unideb.hu

Phone: +36 52 417266 ext. 1388

Web: http://dtp.atomki.hu/~feri

Fax: +36 52 346758

Profile on Google Scholar

Ferenc Kun is professor at the Department of Theoretical Physics (UD). He received his PhD in 1997 and became doctor of the Hungarian Academy of Sciences (DSc) in 2010. As a PhD Student he studied at the Ecole Superieur de la Physique et Chimie Industrielle in Paris, and later on he was postdoc at the Institute of Computational Physics of the University of Stuttgart. His major research field is the physics of complex systems and the statistical physics of fracture and fragmentation phenomena.

Rupture cascades in a discrete element model of porous sedimentary rocks


Understanding the processes that lead up to catastrophic failure in porous granular media is an important problem in a wide variety of applications, notably in Earth sciences and engineering. In natural catastrophes such as landslides and earthquakes, as well as in controlled laboratory tests on rock samples, the available data are incomplete, and provide only a limited insight into the complexity of the key microscopic processes at work prior to failure.


On the other hand computer models can simulate all of the processes at work, right down to the minutest detail. Motivated by this potential, we developed a new computer model of the compressive failure of porous rocks. First we reconstruct a model rock of discrete elements by sedimenting spherical particles, wathing them fall and settle under gravity. Then we 'cement' them together at the points of contact with breakable beams.


Final reassembled samples of the simulations

A cylindrical sample of model sand stone was subject to uniaxial compression until it completely failed. In the final state we reassembled the sample by placing the particles back to their original position inside the body. In the left figure particles are colored according to the size of the fragment they belong to. The formation of a damage band can be observed. In the right figure only the two biggest fragments are presented so that the damage band appeares as an empty region.

As stress is applied the local contacts break, increasingly as cascades of correlated micro-fractures. The model overcomes some problems associated with simpler computational models and spontaneously reproduces the observed scaling laws of rupture cascades in natural and experimental data remarkably well. The new understanding of the relationship between microscopic processes and properties that can be observed at a bigger scale hold out the potential for developing better predictive models for catastrophic failure.



References

1. F. Kun, I. Varga, S. Lennartz-Sassinek, and I. G. MainRupture Cascades in a Discrete Element Model of a Porous Sedimentary Rock , Physical Review Letters 112, 065501 (2014). Highlighted in Physics Focus
b>2. F. Kun, I. Varga, S. Lennartz-Sassinek, and I. G. MainApproach to failure in porous granular materials under compression , Physical Review E 88, 062207 (2013). Highlighted in Physics Focus


In collaboration with

Ian G. Main and Sabine Lenartz-Sassinek, University of Edinburg, UK


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