Influence of vibration amplitude on dynamic triggering of slip in sheared granular layers

M. Griffa, B. Ferdowsi, R. A. Guyer, E. G. Daub, P. A. Johnson, C. Marone, and J. Carmeliet
Phys. Rev. E 87, 012205 – Published 24 January 2013

Abstract

We perform a systematic statistical investigation of the effect of harmonic boundary vibrations on a sheared granular layer undergoing repetitive, fully dynamic stick-slip motion. The investigation is performed using two-dimensional discrete element method simulations. The main objective consists of improving the understanding of dynamic triggering of slip events in the granular layer. Here we focus on how the vibration amplitude affects the statistical properties of the triggered slip events. The results provide insight into the granular physical controls of dynamic triggering of failure in sheared granular layers.

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  • Received 26 September 2012

DOI:https://doi.org/10.1103/PhysRevE.87.012205

©2013 American Physical Society

Authors & Affiliations

M. Griffa1,*, B. Ferdowsi1,2, R. A. Guyer3,4, E. G. Daub3,5, P. A. Johnson3, C. Marone6,7, and J. Carmeliet1,2

  • 1Swiss Federal Laboratories for Materials Science and Technology (EMPA), Überlandstrasse 129, CH-8600, Dübendorf, Switzerland
  • 2Swiss Federal Institute of Technology in Zürich (ETHZ), CH-8093, Zürich, Switzerland
  • 3Solid Earth Geophysics Group, MS D443, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
  • 4Department of Physics, University of Nevada, Reno, Nevada 89557, USA
  • 5Center for Nonlinear Studies, MS D443, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
  • 6Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA
  • 7G3 Center and Energy Institute, Pennsylvania State University, University Park, Pennsylvania 16802, USA

  • *michele.griffa@empa.ch

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Vol. 87, Iss. 1 — January 2013

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