Role of heterogeneous surface wettability on dynamic immiscible displacement, capillary pressure, and relative permeability in a CO2-water-rock system. (July 2022)

• Record Type: Journal Article
• Authors: Guo, Ruichang; Dalton, Laura; Crandall, Dustin; McClure, James; Wang, Hongsheng; Li, Zhe; Chen, Cheng
• Is Part Of: Advances in water resources. Volume 165(2022)
• Publication Date: 2022-07
• Subjects: Geological CO2 sequestration -- Immiscible displacement -- Wettability heterogeneity -- Pc-Sw curve -- Relative permeability; Hydrology -- Periodicals; Hydrodynamics -- Periodicals; Hydraulic engineering -- Periodicals; 551.48
• DOI: 10.1016/j.advwatres.2022.104226
• Languages: English
• ISSNs: 0309-1708

Abstract

Highlights: This study investigates the impact of pore-scale surface wettability heterogeneity on immiscible two-fluid displacement in porous media. Rock surface wettability fields are generated based on in-situ X-ray micro-computed tomography measurements of contact angles. Heterogeneous surface wettability leads to a negative entry pressure of the primary drainage stage under the intermediate-wet condition. Abstract: Surface wettability is one of the major factors that regulate immiscible fluid displacement in porous media. However, the role of pore-scale wettability heterogeneity on dynamic immiscible displacement is rarely investigated. This study investigated the impact of pore-scale wettability heterogeneity on immiscible two-fluid displacement and the resulting macroscopic constitutive relations, including the capillary pressure-water saturation ( P c -S w ) and relative permeability curves. A digital Bentheimer sandstone model was obtained from X-ray micro-computed tomography (micro-CT) scanning and the rock surface wettability fields were generated based on in-situ measurements of contact angles. A graphics processing unit-accelerated lattice Boltzmann model was employed to simulate the immiscible displacement processes through the primary drainage, imbibition, and second drainage stages in a CO2 -water-rock system. We found that pore-scale surface wettability heterogeneity caused noticeable local supercritical CO2 (scCO2 ) and water redistribution under less water-wet conditions. At the continuum scale, the P c -S w curves under the heterogeneous wetting condition were overall similar to those under the homogeneous wetting condition. This is because the impact of local wettability heterogeneity on the large-scale Pc -Sw curve was statistically averaged out at the entire-sample scale. The only difference was that heterogeneous wettability led to a negative entry pressure at the primary drainage stage under the intermediate-wet condition, which was caused by local, scCO2 -wet surfaces. The impact of pore-scale wettability heterogeneity was more noticeable on the relative permeability curves. Particularly, the variation of the scCO2 relative permeability curve in the heterogeneous wettability scenario was more significant than that in the homogenous wettability scenario. This suggests that pore-scale wettability heterogeneity enhances the coalescence and snap-off behaviors of scCO2 blobs. This is the first study that systematically investigated the role of pore-scale wettability heterogeneity on dynamic immiscible displacement and associated P c -S w curves in complicated, three-dimensional porous media.