2019
DOI: 10.1051/e3sconf/20198904002
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Impact of injection rate on transient oil recovery under mixed-wet conditions: a microfluidic study

Abstract: Lab-on-a-chip methods were used to visualize the pore-scale distribution of oil within a mixed-wet, quasi-monolayer of marble grains packed in a microfluidic channel as the oil was displaced by water. Water injection rates corresponding to microscopic capillary numbers between Ca = 5 × 10-8 and 2 × 10-4 (Darcy velocities between 0.3 and 1100 ft/d) were considered. As expected, early-time water invasion transitions from stable displacement to capillary fingering with decreasing Ca, with capillary fingering obse… Show more

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Cited by 3 publications
(3 citation statements)
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“…Displacement of one fluid by another within a porous medium is relevant to many processes such as oil and gas recovery from hydrocarbon reservoirs, CO 2 storage in deep saline aquifers, gas transport in fuel cells, nonaqueous phase liquid contaminant transport in groundwater aquifers, and water infiltration into soils. Immiscible displacement encountered in these applications is influenced, at the pore scale, by the properties of the grains (size distribution, roughness, mineralogy) and how they are arranged (pore topology and geometry) [e.g., [1][2][3][4][5], the properties of the fluids (chemical and physical constituents, which in turn alter fluid-fluid-grain contact angle, fluid-fluid interfacial tension, viscosity, and density) [e.g., [6][7][8], the fractional volumes of the fluids initially occupying the pores [e.g., 6,9,10], and the velocity of the fluids [e.g., 11,12].…”
Section: Introductionmentioning
confidence: 99%
“…Displacement of one fluid by another within a porous medium is relevant to many processes such as oil and gas recovery from hydrocarbon reservoirs, CO 2 storage in deep saline aquifers, gas transport in fuel cells, nonaqueous phase liquid contaminant transport in groundwater aquifers, and water infiltration into soils. Immiscible displacement encountered in these applications is influenced, at the pore scale, by the properties of the grains (size distribution, roughness, mineralogy) and how they are arranged (pore topology and geometry) [e.g., [1][2][3][4][5], the properties of the fluids (chemical and physical constituents, which in turn alter fluid-fluid-grain contact angle, fluid-fluid interfacial tension, viscosity, and density) [e.g., [6][7][8], the fractional volumes of the fluids initially occupying the pores [e.g., 6,9,10], and the velocity of the fluids [e.g., 11,12].…”
Section: Introductionmentioning
confidence: 99%
“…In addition to capillary number and viscosity ratio, wettability effects on fingering patterns were recently investigated as a third dimension for a phase diagram in 2D flow cells (Zhao et al, 2016). The investigated pore-scale geometries have generally been 2D (Lenormand et al, 1988), 2.5D (Christensen et al, 2019), or 3D homogeneous porous matrices (Islam et al, 2014) or a single planar rough fracture (Chen et al, 2017). Whether and to what extent the existence of microfractures, connected or dead-end, can affect unstable flow is not yet well-known.…”
Section: Introductionmentioning
confidence: 99%
“…If the Ca is small, the invading fluid propagates as thick fingers that follow a tortuous path through the porous medium ("capillary fingering"). The exact (Ca, M) at which the flow transitions from one regime to the other is difficult to predict, as it is a function of many factors, including the pore geometry [11] and hydrophilicity [12,13] of the porous medium. Notwithstanding this, regime boundaries proposed [8] for staggered cylinder arrays are presented in Figure 1 as a guide.…”
Section: Introductionmentioning
confidence: 99%