[CIG-SHORT] Griffith Crack Theory Implementation
Brad Aagaard
baagaard at usgs.gov
Tue Jan 28 14:22:22 PST 2014
Jared,
PyLith's currently has two fault implementations. One is for prescribing
slip time histories on the fault, and the other uses a friction model as
a constitutive model for sliding/opening on the fault surface. In
setting up the fault constitutive model implementation, I explicitly
formulated it in terms of a friction model,
T_s = C + mu_f * T_n,
where T_s is the shear traction, C is cohesion, mu_f is the coefficient
of friction, and T_n is the normal traction. Adding difference friction
models is designed to be very easy and there is a template for doing so.
The fault constitutive implementation could be rewritten to be more
general and modular and would involve only a small piece of the code if
you are inclined to get your hands dirty. We have much high priority and
bigger issues on our plate right now related to expanding the
capabilities of the code for higher order discretizations and multiphysics.
Regards,
Brad
On 01/28/2014 12:06 PM, Jared William Graham Atkinson wrote:
> Hello all,
>
> I am currently working with Dr. Brad Hager at MIT and am looking at attempting to implement Griffith crack theory as a faulting/fracturing mechanism in Pylith.
>
> I have spoken with Lucas Willemsen about his previous work on Rate-State Ageing, and he suggested I contact this mailing list to see if the current Pylith iteration would be capable of handling a new constitutive law.
>
> Any insight into this issue and its viability is greatly appreciated!
>
> Thank you for your time.
> Jared Atkinson
>
>
>
> _______________________________________________
> CIG-SHORT mailing list
> CIG-SHORT at geodynamics.org
> http://geodynamics.org/cgi-bin/mailman/listinfo/cig-short
>
More information about the CIG-SHORT
mailing list