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The "problem" is that the factor A_diff depends on temperature (and R*T). It is unclear how to implement this flow law. Can we readily use abstract flow laws to account for this or is more engineering needed?
Below screenshots from the paper:
The text was updated successfully, but these errors were encountered:
This cannot be done with the existing DiffusionCreep structure, but instead you would have to create a new one (say DiffusionCreep_ice).
Much of what is required can be seen here, and you could add a data table for this as well (see this example), which would allow you to predefine multiple ice rheologies.
Once implemented, it should work with all composite rheologies, plotting and computational routines in GeoParams (and can be combined with elasticity, plasticity).
Adding ice flow composite rheology requires to incorporate following diffusion creep law from Goldsby and Kohlstedt (2001), eq.4 + Table 6:
The "problem" is that the factor
A_diff
depends on temperature (andR*T
). It is unclear how to implement this flow law. Can we readily use abstract flow laws to account for this or is more engineering needed?Below screenshots from the paper:
![Screenshot 2022-10-06 at 23 28 14](https://user-images.githubusercontent.com/61313342/194421977-711ca57d-ef62-4ab0-b686-71396fa6061e.png)
![Screenshot 2022-10-06 at 23 28 31](https://user-images.githubusercontent.com/61313342/194422006-8a7dd7c3-b0c9-4d6f-bde8-1d1f5c191db7.png)
The text was updated successfully, but these errors were encountered: