Dry friction avalanches: Experiment and theory

Sergey V. Buldyrev, John Ferrante, and Fredy R. Zypman
Phys. Rev. E 74, 066110 – Published 19 December 2006

Abstract

Experimental evidence and theoretical models are presented supporting the conjecture that dry friction stick-slip is described by self-organized criticality. We use the data, obtained with a pin-on-disk tribometer set to measure lateral force, to examine the variation of the friction force as a function of time. We study nominally flat surfaces of matching aluminum and steel. The probability distribution of force drops follows a negative power law with exponents μ in the range 3.2–3.5. The frequency power spectrum follows a 1fα pattern with α in the range 1–1.8. We first compare these experimental results with the well-known Robin Hood model of self-organized criticality. We find good agreement between theory and experiment for the force-drop distribution but not for the power spectrum. We explain this on a physical basis and propose a model which takes explicitly into account the stiffness and inertia of the tribometer. Specifically, we numerically solve the equation of motion of a block on a friction surface pulled by a spring and show that for certain spring constants the motion is characterized by the same power law spectrum as in experiments. We propose a physical picture relating the fluctuations of the force drops to the microscopic geometry of the surface.

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  • Received 8 September 2005

DOI:https://doi.org/10.1103/PhysRevE.74.066110

©2006 American Physical Society

Authors & Affiliations

Sergey V. Buldyrev1, John Ferrante2, and Fredy R. Zypman1

  • 1Department of Physics, Yeshiva University, 2495 Amsterdam Avenue, New York, New York 10033, USA
  • 2NASA-Glenn Research Center, 21000 Brookpark Road, Cleveland, Ohio 44135, USA

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Issue

Vol. 74, Iss. 6 — December 2006

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