We numerically model two-dimensional systems of granular aggregates confined between two rough walls and demonstrate that at a critical grain volume fraction nu(c) an abrupt rigidity transition occurs. The transition has first-order characteristics, although the elastic constants undergo a second-order transition. Densely packed grains, with a volume fraction nu>nu(c), display an elastic-plastic rheology. Loose packings, with nu<nu(c), display gas-like characteristics. It is shown that when the volume fraction is allowed to change freely (applying a constant normal stress to the walls), it evolves spontaneously to nu(c) under a wide range of boundary stress values, demonstrating that the phase boundary is an attractive critical state.
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Aharonov et al. (1999) studied this question.
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