  We investigate the scaling properties of the sources of crackling noise in a
fully-dynamic numerical model of sedimentary rocks subject to uniaxial
compression. The model is initiated by filling a cylindrical container with
randomly-sized spherical particles which are then connected by breakable beams.
Loading at a constant strain rate the cohesive elements fail and the resulting
stress transfer produces sudden bursts of correlated failures, directly
analogous to the sources of acoustic emissions in real experiments. The source
size, energy, and duration can all be quantified for an individual event, and
the population analyzed for their scaling properties, including the
distribution of waiting times between consecutive events. Despite the
non-stationary loading, the results are all characterized by power law
distributions over a broad range of scales in agreement with experiments. As
failure is approached temporal correlation of events emerge accompanied by
spatial clustering.
