NANAFeb 23, 2017

Coupling of multiscale and multi-continuum approaches

arXiv:1702.0709558 citationsh-index: 47
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For researchers in computational geoscience, this work provides a theoretical and practical framework to combine two popular model reduction techniques, though the improvements are incremental.

This paper establishes a relation between multi-continuum approaches and the Generalized Multiscale Finite Element Method (GMsFEM) for simulating flow in fractured media, and proposes coupling these methods to handle both resolved and unresolved fractures. Numerical results demonstrate that GMsFEM can automatically detect fracture networks and that a simplified basis construction achieves similar accuracy to spectral basis functions.

Simulating complex processes in fractured media requires some type of model reduction. Well-known approaches include multi-continuum techniques, which have been commonly used in approximating subgrid effects for flow and transport in fractured media. Our goal in this paper is to (1) show a relation between multi-continuum approaches and Generalized Multiscale Finite Element Method (GMsFEM) and (2) to discuss coupling these approaches for solving problems in complex multiscale fractured media. The GMsFEM, a systematic approach, constructs multiscale basis functions via local spectral decomposition in pre-computed snapshot spaces. We show that GMsFEM can automatically identify separate fracture networks via local spectral problems. We discuss the relation between these basis functions and continuums in multi-continuum methods. The GMsFEM can automatically detect each continuum and represent the interaction between the continuum and its surrounding (matrix). For problems with simplified fracture networks, we propose a simplified basis construction with the GMsFEM. This simplified approach is effective when the fracture networks are known and have simplified geometries. We show that this approach can achieve a similar result compared to the results using the GMsFEM with spectral basis functions. Further, we discuss the coupling between the GMsFEM and multi-continuum approaches. In this case, many fractures are resolved while for unresolved fractures, we use a multi-continuum approach with local Representative Volume Element (RVE) information. As a result, the method deals with a system of equations on a coarse grid, where each equation represents one of the continua on the fine grid. We present various basis construction mechanisms and numerical results.

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