Effects of Pore-Scale Disorder on Fluid Displacement in Partially-Wettable Porous Media
arXiv:1608.00900 · doi:10.1038/srep36221
Abstract
We present a systematic, quantitative assessment of the impact of pore size disorder and its interplay with flow rates and wettability on immiscible displacement of a viscous fluid. Pore-scale simulations and micromodel experiments show that reducing disorder increases the displacement efficiency and compactness, minimizing the fluid-fluid interfacial area, through (i) trapping at low rates and (ii) viscous fingering at high rates. Increasing the wetting angle suppresses both trapping and fingering, hence reducing the sensitivity of the displacement to the underlying disorder. A modified capillary number that includes the impact of disorder on viscous forces (through pore connectivity) is direct related to , in par with previous works. Our findings bear important consequences on sweep efficiency and fluid mixing and reactions, which are key in applications such as microfluidics to carbon geosequestration, energy recovery, and soil aeration and remediation.
References in corpus (5)
- Wettability stabilizes fluid invasion into porous media via nonlocal, cooperative pore filling
- Fluid Mixing from Viscous Fingering
- Growth activity during fingering in a porous Hele Shaw cell
- Influence of pore-scale disorder on viscous fingering during drainage
- Wetting heterogeneity in mixed-wet porous media controls flow dissipation
Cited by in corpus (8)
- Impact of spatially correlated pore-scale heterogeneity on drying porous media
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- Immiscible fluid displacement in porous media with spatially correlated particle sizes
- Tuning capillary flow in porous media with hierarchical structures
- Vortices of Electro-osmotic Flow in Heterogeneous Porous Media
- Characteristics of fluid-fluid displacement in model mixed-wet porous media: patterns, pressures, and scalings
- X-ray Tomographic Micro-Particle Velocimetry in Porous Media
- Pore-scale Modelling of Gravity-driven Drainage in Disordered Porous Media