| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8915752 | Physics of the Earth and Planetary Interiors | 2018 | 42 Pages |
Abstract
The computational framework we devise is immediately applicable to modelling high melt fraction phenomena in Earth and planetary science research. Furthermore, it provides a template for solving similar non-linear diffusion equations that arise in other science and engineering disciplines, particularly for non-linear functional forms of the diffusion coefficient.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
Dan J. Bower, Patrick Sanan, Aaron S. Wolf,