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Two‐Phase Fluid Flow Properties of Rough Fractures With Heterogeneous Wettability: Analysis With Lattice Boltzmann Simulations
Author(s) -
Guiltinan Eric J.,
Santos J. E.,
Cardenas M. Bayani,
Espinoza D. Nicolas,
Kang Qinjun
Publication year - 2021
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2020wr027943
Subject(s) - capillary pressure , relative permeability , wetting , lattice boltzmann methods , materials science , permeability (electromagnetism) , multiphase flow , microscale chemistry , mechanics , geotechnical engineering , surface finish , capillary action , saturation (graph theory) , fluid dynamics , capillary number , geology , composite material , porous medium , chemistry , porosity , biochemistry , physics , mathematics education , mathematics , combinatorics , membrane
Fractures are conduits for fluid flow in low‐permeability geological formations. Multiphase flow properties of fractures are important in natural processes and in engineering applications such as the evaluation of the sealing capacity of caprocks and productivity of hydrocarbon‐bearing tight rocks. Investigations of flow and transport through fractures typically focus on the effects of fracture geometric and mechanical factors such as aperture, roughness, and compressibility. The wettability of the fracture surfaces and its influence on microscale interfacial phenomena and macroscale effective transport properties are seldom studied. Here, we investigated the effect of heterogeneous wetting properties on the displacement of water by supercritical CO 2 through a series of lattice Boltzmann method simulations. The results show the evolution of the CO 2 plume within a fracture is controlled by both the roughness of the aperture field and the wetting distribution. We combined these factors into a capillary pressure map that can be related to the macroscopic flow behavior of the fracture. We observed that heterogeneous wetting distributions promote the residual trapping of water where lower capillary pressures allowed for isolated water pockets in higher capillary pressure zones. Analysis of fracture unsteady relative permeability shows the effect of wetting on permeability evolution and provides support for the viscous‐coupling relative permeability model. Finally, analysis of the steady‐state relative permeability and saturation demonstrates a strong correlation between permeability and the standard deviation of the capillary pressure field. Thus, characterizing the distribution of wetting properties of fractures is crucial to understanding multiphase fracture flow and transport properties.