[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
>
>
>
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