Periodic Reporting for period 1 - MiDiROM (Deep learning enhanced numerical simulations of mixed-dimensional models for subsurface flow)
Reporting period: 2022-01-16 to 2024-01-15
Two main objectives were targeted by the project. First, we developed numerical methods known as reduced order models for flows in fractured rock. Such models can capture the changes in flow due to different material properties and can therefore be used to rapidly simulate multiple scenarios. The second objective was to construct and analyze models for flow systems by using deep learning algorithms. The main challenge in this context was to ensure that the trained neural networks provide flow fields that satisfy physical laws, such as the law of mass conservation. We reached this objective by proposing a solution technique that exploits the underlying mathematical structure of the problem.
In parallel with the mathematical aspects of the project, we contributed to an open-source software package where all numerical experiments from the project can be easily reproduced. This code base, called PyGeoN, is designed to construct discretization methods and solvers for mixed-dimensional problems by providing access to the block matrix structure of the problem. The code availability allows for its usage by the scientific community and further developments.
In total, the project has generated seven scientific articles that have been submitted to peer-reviewed journals. Our findings were presented at seven international conferences, including the SIAM Conference on Mathematical and Computational Issues in the Geosciences and Computational Methods in Water Resources. Moreover, we discussed the results with experts in the field at six academic workshops such as SuPreNum: Structure Preserving Numerical Methods and FRAME: Fractured media; numerical methods for fluid flow and mechanics.
Secondly, we constructed and analyzed a new mixed finite element method for Stokes flow with only one degree of freedom per facet and cell of the mesh. The same approach was then used to model the displacement and pressure in Biot poroelasticity. Linear convergence was shown theoretically and numerically in both cases, and the methods produce satisfactory results for well-known benchmark problems. Third, we developed domain decomposition methods using MPFA finite volume schemes for Darcy flows and the MAC-scheme for Stokes flow. These schemes, based on flux-mortar methods, were shown to satisfy a priori error estimates and proved efficient in practice on realistic model problems. Finally, we made a new connection between a class of coupled problems and the Čech-de-Rham complex. This perspective provides a new insight into the structure of these problems which helps in their analysis.