Novel technique for solving advection-dominated fluid flow in anisotropic and heterogeneous porous media
In our recent publication (https://doi.org/10.1016/j.cma.2023.116285), we introduced a novel numerical approach that constructs solutions across multiple scales, achieving both a stable solution and an on-the-fly adaptive refinement. We demonstrate the effectiveness and reliability of our method through various numerical experiments, which include high heterogeneity, pronounced anisotropic diffusion tensors, and convection-dominated diffusion.
By employing this method, we can obtain more precise numerical approximations to predict mineral flow deposition in complex permeability porous media, all while reducing the computational cost.
![](https://i0.wp.com/research.csiro.au/earth-process-models/wp-content/uploads/sites/479/2023/08/multiscale1.png?resize=380%2C465&ssl=1)
Representation of the multi-scale solution and the transition from error estimation to the fine scale using an inter-scale operator.
![](https://i0.wp.com/research.csiro.au/earth-process-models/wp-content/uploads/sites/479/2023/08/figure-ani-burgers.png?resize=551%2C460&ssl=1)
Results for a shock wave problem: Full-scale stabilised solution (left), refined mesh after several levels of adaptive refinement (middle). Fine-scale solution (right).