Universal Dynamic Fragmentation in D Dimensions

J. A. Åström, F. Ouchterlony, R. P. Linna, and J. Timonen
Phys. Rev. Lett. 92, 245506 – Published 18 June 2004

Abstract

A generic model is introduced for brittle fragmentation in D dimensions, and this model is shown to lead to a fragment-size distribution with two distinct components. In the small fragment-size limit a scale-invariant size distribution results from a crack branching-merging process. At larger sizes the distribution becomes exponential as a result of a Poisson process, which introduces a large-scale cutoff. Numerical simulations are used to demonstrate the validity of the distribution for D=2. Data from laboratory-scale experiments and large-scale quarry blastings of granitic gneiss confirm its validity for D=3. In the experiments the nonzero grain size of rock causes deviation from the ideal model distribution in the small-size limit. The size of the cutoff seems to diverge at the minimum energy sufficient for fragmentation to occur, but the scaling exponent is not universal.

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  • Received 10 November 2003

DOI:https://doi.org/10.1103/PhysRevLett.92.245506

©2004 American Physical Society

Authors & Affiliations

J. A. Åström1, F. Ouchterlony2, R. P. Linna3, and J. Timonen3

  • 1Centre for Scientific Computing, P.O. Box 405, FIN-02101 Esbo, Finland
  • 2Swedish Blasting Research Centre at LTU, Box 47047, S-10074 Stockholm, Sweden
  • 3Department of Physics, University of Jyväskylä, P.O. Box 35, FIN-40014 Jyväskylä, Finland

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Vol. 92, Iss. 24 — 18 June 2004

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