Viscous Fingering and Preferential Flow Paths in Heterogeneous Porous Media. Issue 3 (21st March 2020)

• Record Type: Journal Article
• Authors: Tang, Y. B.; Li, M.; Bernabé, Y.; Zhao, J. Z.
• Is Part Of: Journal of geophysical research. Volume 125:Issue 3(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-03-21
• Subjects: flow channeling -- immiscible displacements -- viscous fingering -- pore‐scale heterogeneity -- pore connectivity -- network simulation; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1029/2019JB019306
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: Preferential flow channeling and viscous fingering are widely observed phenomena in heterogeneous porous media from the pore scale to the core and reservoir scales. The transition from capillary to viscous fingering with increasing injection rate is also a well‐known phenomenon. Based on the previously observed visual similarity of viscous fingers and preferential single‐phase flow paths in 2‐D simulations, we postulate that these single‐ and two‐phase flow patterns should also be interrelated in 3‐D porous media. Capillary fingering is a manifestation of invasion percolation, a process restricted to the subnetwork of pores obtained from the critical path analysis. We investigated single‐phase flow channeling by applying a method similar to critical path analysis to the flow rate field and compared the subnetwork thus determined to the set of invaded pipes in drainage simulations. Our aim is to quantify the relation between preferential flow paths and viscous fingering, its dependence on pore‐scale heterogeneity and pore connectivity, and ultimately to upscale the network observations to the field scale appropriate for the engineering applications involving drainage in heterogeneous media. Key Points: The single‐phase flow channeling is investigated by applying a method similar to CPA to the flow rate field The relation between flow channeling and viscous fingering and its dependence on pore‐scale heterogeneity are quantified