13–16 May 2024
Asia/Shanghai timezone

Impact of corner-bridge flow on capillary pressure curve

13 May 2024, 17:45
15m
Oral Presentation (MS03) Flow, transport and mechanics in fractured porous media MS03

Speaker

Dr Tian Lan (Wuhan university)

Description

The capillary pressure curve is essential for predicting multiphase flow processes in geological systems. At low saturations, wetting films form and become important, but how wetting films control this curve remains inadequately understood. In this study, we combine microfluidic experiments with pore-network modeling to investigate the impact of corner-bridge flow on the capillary pressure curve in porous media. Using a CMOS camera and a confocal laser scanning microscopy, we directly observe the corner-bridge flow under quasi-static drainage displacement, revealing that corner-bridge flow serves as an additional flow path to drain trapped water. Consequently, the capillary pressure curve shifts towards lower saturations, resulting in a reduced water residual saturation. We establish a theoretical criterion for the occurrence of corner-bridge flow and develop a pore-network model to simulate quasi-static drainage, taking into account this additional flow path. Pore-network modeling results agree well with our experimental observation. On this basis, we employ our pore-network model to systematically analyze the impact of corner-bridge flow on capillary pressure curve across varying porosity, pore-scale disorder, and system size. Results indicate that the impact of corner-bridge flow becomes more pronounced as porosity decreases and shape factor increases. Our findings demonstrate that the maximum decrease of water residual saturation is 0.19 when porosity is at its minimum, and the shape factor is at its maximum. This work bridges the gap between the pore-scale mechanism and capillary pressure behavior and has significant implications for estimating the amount of extractable water and the CO2 storage capacity.

References Bakhshian, S., Rabbani, H. S., Hosseini, S. A., & Shokri, N. (2020). New insights into complex interactions between heterogeneity and wettability influencing two-phase flow in porous media. Geophysical Research Letters, 47(14), e2020GL088187. https://doi.org/10.1029/2020GL088187 Borgman, O., Fantinel, P., Luhder, W., Goehring, L., Holtzman, R. (2017). Impact of spatially correlated pore-scale heterogeneity on drying porous media. Water Resources Research, 53(7), 5645–5658. https://doi.org/10.1002/2016WR020260 Cejas, C. M., Hough, L. A., Fretigny, C., & Dreyfus, R. (2018). Effect of geometry on the dewetting of granular chains by evaporation. Soft Matter, 14(34), 6994-7002. https://doi.org/10.1039/c8sm01179f Cieplak, M., & Robbins, M. O. (1988). Dynamical transition in quasi-static fluid invasion in porous-media. Physical Review Letters, 60(20), 2042–2045. https://doi.org/10.1103/PhysRevLett.60.2042 Cieplak, M., & Robbins, M. O. (1990). Influence of contact-angle on quasi-static fluid invasion of porous-media.
Country China
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Primary authors

Guan-Xiong Wang (Wuhan university) Ran Hu (Wuhan University) Dr Tian Lan (Wuhan university) Yi-Feng Chen (Wuhan University) Zhibing Yang (Wuhan University)

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