A. Bizzarri et al., Solving the dynamic rupture problem with different numerical approaches and constitutive laws, GEOPHYS J I, 144(3), 2001, pp. 656-678
We study the dynamic initiation, propagation and arrest of a 2-D in-plane s
hear rupture by solving the elastodynamic equation by using both a boundary
integral equation method and a finite difference approach. For both method
s we adopt different constitutive laws: a slip-weakening (SW) law, with con
stant weakening rate, and rate- and state-dependent friction laws (Dieteric
h-Ruina). Our numerical procedures allow the use of heterogeneous distribut
ions of constitutive parameters along the fault for both formulations. We f
irst compare the two solution methods with an SW law, emphasizing the requi
red stability conditions to achieve a good resolution of the cohesive zone
and to avoid artificial complexity in the solutions. Our modelling results
show that the two methods provide very similar time histories of dynamic so
urce parameters. We paint out that, if a careful control of resolution and
stability is performed, the two methods yield identical solutions. We have
also compared the rupture evolution resulting from an SW and a rate- and st
ate-dependent friction law. This comparison shows that despite the differen
t constitutive formulations, a similar behaviour is simulated during the ru
pture propagation and arrest. We also observe a crack tip bifurcation and a
jump in rupture velocity (approaching the P-wave speed) with the Dieterich
-Ruina (DR) law. The rupture arrest at a barrier thigh strength zone) and t
he barrier-healing mechanism are also reproduced by this law. However, this
constitutive formulation allows the simulation of a more general and compl
ex variety of rupture behaviours. By assuming different heterogeneous distr
ibutions of the initial constitutive parameters, we are able to model a bar
rier-healing as well as a self-healing process. This result suggests that i
f the heterogeneity of the constitutive parameters is taken into account, t
he different healing mechanisms can be simulated. We also study the nucleat
ion phase duration T-n, defined as the time necessary for the crack to reac
h the half-length l(c). We compare the T-n values resulting from distinct s
imulations calculated using different constitutive laws and different sets
of constitutive parameters. Our results confirm that the DR law provides a
different description of the nucleation process than the SW law adopted in
this study. We emphasize that the DR law yields a complete description of t
he rupture process, which includes the most prominent features of SW.