Abstract
A generic model is introduced for brittle fragmentation in 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 . Data from laboratory-scale experiments and large-scale quarry blastings of granitic gneiss confirm its validity for . 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.
- Received 10 November 2003
DOI:https://doi.org/10.1103/PhysRevLett.92.245506
©2004 American Physical Society