Effect of Wettability and Permeability on Pore-Scale of CH4–Water Two-Phase Displacement Behavior in the Phase Field Model
Hydraulic measures such as hydraulic slotting and hydraulic fracturing are commonly used in coal seam pressure relief and permeability enhancement. Two-phase flow patterns of CH4–water in pore-sized coal seams after hydraulic measures are critical to improve gas extraction efficiency. The phase field module in COMSOL Multiphysics™ 5.4 and the classical ordered porous media model were used in this paper. The characteristics of CH4–water two-phase immiscible displacement in coal seams under different capillary numbers (Ca) and viscosity ratios (M) were simulated and quantitatively analyzed. By changing the contact angle of the porous media, the flow patterns of CH4–water two-phase in coal with different wettability were simulated. Results show that wettability significantly affects the displacement efficiency of CH4. Additionally, by constructing a dual-permeability model to simulate the varying local permeability of the coal, the flow patterns of different Ca and M in dual-permeability media were further investigated. It is found that CH4 preferentially invades high-permeability regions, and the displacement efficiency in low-permeability regions increases with higher Ca and M, providing a reference for gas extraction from coal seams after hydraulic measures.
Authors
- Nan Liu (ORCID: https://orcid.org/0000-0002-9717-2137)
- Chang Guo (ORCID: https://orcid.org/0000-0001-6527-6989)
- Kai Fan (ORCID: https://orcid.org/0000-0001-6870-6657)
- Ting Liu (ORCID: https://orcid.org/0000-0002-1636-5990)
- Xiangliang Zhang (ORCID: https://orcid.org/0000-0003-0718-1783)
- Zedong Wang
Institutions
- China University of Mining and Technology (CN)
- China Jiliang University (CN)
Publication Details
- Journal
- Applied Sciences
- Published
- 2024-08-05
- DOI
- https://doi.org/10.3390/app14156815
- Citations
- 5
- Primary Topic
- Enhanced Oil Recovery Techniques
- Type
- article
- Field-Weighted Citation Impact
- 1.68