A quasi steady state method for solving transient Darcy flow in complex 3D fractured networks accounting for matrix to fracture flow

DOI10.1016/j.jcp.2014.11.038zbMath1351.76280OpenAlexW2009813363MaRDI QIDQ728929

Benoit Noetinger

Publication date: 20 December 2016

Published in: Journal of Computational Physics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.jcp.2014.11.038

zbMATH Keywords

Laplace transformtransfer functiondiscrete fracture networkdual porosityfractured reservoirsquasi steady statelow permeability matrixtransport in fractured media

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Finite volume methods applied to problems in fluid mechanics (76M12) Finite element methods applied to problems in fluid mechanics (76M10) Finite element, Rayleigh-Ritz and Galerkin methods for initial value and initial-boundary value problems involving PDEs (65M60) Finite volume methods for initial value and initial-boundary value problems involving PDEs (65M08)

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Uses Software

• Algorithm 368

Cites Work

• Unnamed Item
• A quasi steady state method for solving transient Darcy flow in complex 3D fractured networks
• Multiscale finite element methods for high-contrast problems using local spectral basis functions
• A parallelizable method for two-phase flows in naturally-fractured reservoirs
• Homogenization and porous media
• A Generalized Mixed Hybrid Mortar Method for Solving Flow in Stochastic Discrete Fracture Networks
• Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks [strata]
• Derivation of the Double Porosity Model of Single Phase Flow via Homogenization Theory

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