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By Yingxin Zhou; Jian Zhao

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Static simulation is also available when the velocity is ignored. ii) PMM is a fully implicit model. All unknowns are solved by a global mathematical equation. The contact behaviours are described by the penalty method and the open-close iteration is inherited from manifold method to make contact state convergent. iii) PMM extends NMM to micro scale simulation. By importing proper failure mechanisms, PMM could simulate explicit processes with implicit modelling. iv) PMM is capable of presenting material nonlinearity and inhomogeneity.

Proceedings of the 1st Congress of International Society of Rock Mechanics, Lisbon, 1966, 439–442. R. : Transmission of seismic waves across single natural fractures. 8617–8638. R. : Anisotropy in seismic velocities and amplitudes from multiple parallel fractures. 11345–11358. , Wang, M. : Strain-rate effects on the strength and fragmentation size of rocks. 1355–1364. : High rates and impact experiments. N. 929–960. Ravichandran, G. : A micromechanical model for high strain rate behavior of ceramics.

4 The momentum-trap system: (a) photograph and (b) x-t diagram showing its working principle.

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