4.7 Article

Discontinuous and continuous Galerkin methods for compressible single-phase and two-phase flow in fractured porous media

期刊

ADVANCES IN WATER RESOURCES
卷 156, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.advwatres.2021.104039

关键词

Fractured porous media; Discontinuous Galerkin; Compressible flow; Discrete fractured model

资金

  1. National Natural Science Foundation of China [42002255, 41902310]
  2. Jiangsu Province Natural Science Foundation [BK20180636]
  3. Chinese Geological Survey [DD20201165]

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The study presents DG and CG approximations for single- and two-phase flow in fractured porous media. The proposed method accurately captures pressure continuity and jumps across the matrix-fracture interface. Simulation results demonstrate reliable prediction of flow behaviors in fractured porous media using the developed approach.
Accurate simulation of flow behaviors in fractured porous media is challenging. We present a discontinuous Galerkin (DG) approximation and continuous Galerkin (CG) approximation for compressible single- and twophase flow in porous media with conducting (high permeable) and blocking (low permeable) fractures using a mixed-dimensional approach in which the fracture is described as a reduced-dimensional interface coupled with linear transmission conditions. The proposed DG/CG method was first verified with single-phase fractured flow benchmark cases and then applied to time-dependent single-phase flow cases. The simulated results demonstrate that the DG/CG method is capable of capturing the continuity as well as the jump in pressure between the two sides of the matrix-fracture interface. For the two-phase flow cases, we verify the DG/CG method with a reference case involving a complex fracture configuration. Subsequently, we analyze several cases to study two-phase flow through a single fracture and a discrete fracture network in two dimensions. Overall, the simulation results show that the developed DG/CG approach can reliably predict the flow behaviors for single- and two-phase flow in fractured porous media.

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