Flow in a multiaquifer porous system can be simulated by the so-called "quasi three-dimensional" models. When heterogeneous and/or aquitards with nonlinear hydrogeologic behavior are considered, a fully numerical approach is required for the model solution. If the finite element method is used to in
Parallel non-iterative methods for evolutionary semilinear flow problems
✍ Scribed by A. Arrarás; L. Portero; J. C. Jorge
- Publisher
- John Wiley and Sons
- Year
- 2008
- Tongue
- English
- Weight
- 253 KB
- Volume
- 56
- Category
- Article
- ISSN
- 0271-2091
- DOI
- 10.1002/fld.1693
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