4.7 Article

An adaptive lattice Boltzmann scheme for modeling two-fluid-phase flow in porous medium systems

Journal

WATER RESOURCES RESEARCH
Volume 52, Issue 4, Pages 2601-2617

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015WR018279

Keywords

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Funding

  1. Army Research Office [W911NF-14-1-0287]
  2. National Science Foundation [0941235]
  3. Department of Energy [DE-SC0002163]
  4. Division Of Earth Sciences
  5. Directorate For Geosciences [1619767] Funding Source: National Science Foundation
  6. Division Of Earth Sciences
  7. Directorate For Geosciences [0941235] Funding Source: National Science Foundation

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We formulate a multiple-relaxation-time (MRT) lattice-Boltzmann method (LBM) to simulate two-fluid-phase flow in porous medium systems. The MRT LBM is applied to simulate the displacement of a wetting fluid by a nonwetting fluid in a system corresponding to a microfluidic cell. Analysis of the simulation shows widely varying time scales for the dynamics of fluid pressures, fluid saturations, and interfacial curvatures that are typical characteristics of such systems. Displacement phenomena include Haines jumps, which are relatively short duration isolated events of rapid fluid displacement driven by capillary instability. An adaptive algorithm is advanced using a level-set method to locate interfaces and estimate their rate of advancement. Because the displacement dynamics are confined to the interfacial regions for a majority of the relaxation time, the computational effort is focused on these regions. The proposed algorithm is shown to reduce computational effort by an order of magnitude, while yielding essentially identical solutions to a conventional fully coupled approach. The challenges posed by Haines jumps are also resolved by the adaptive algorithm. Possible extensions to the advanced method are discussed.

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