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The quasistatic, Prandtl-Reuss perfect plasticity at small strains is combined with a gradient, reversible (i.e.
admitting healing) harm which influences both the elastic moduli and the yield stress. An vital facet of the model is that not solely the conservative part but also the dissipative half is subjected to damage, i.e. not only the elastic moduli but also the yield stress might be considered as damageable.
Much less literature addresses various combination of plasticity and harm, cf. Also a lot of geophysical models combine reversible harm (referred to as slightly ageing) with some sort of plasticity (typically modelled as not solely impartial of damage, however), cf.
A slender so-known as core of the fault could be modelled by the perfect plasticity whereas. POSTSUBSCRIPT in order to calculate threat measures, a step we loosely name "forecasting", may be performed as soon as an applicable model for the innovations has been decided.
POSTSUBSCRIPT by way of (2.14h) under. POSTSUBSCRIPT inactive. Note that at any step, if there isn't a lively node, the exploration process terminates.

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