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The effect of ions on the motion of an oil slug through a charged capillary

Published online by Cambridge University Press:  21 February 2018

Z. M. Wilmott*
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
C. J. W. Breward
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
S. J. Chapman
Affiliation:
Mathematical Institute, University of Oxford, Radcliffe Observatory Quarter, Woodstock Road, Oxford OX2 6GG, UK
*
†Email address for correspondence: wilmott@maths.ox.ac.uk

Abstract

Numerous experimental studies have documented that injecting low-salinity water into an oil reservoir can increase the amount of oil recovered. However, owing to the complexity of the chemical interactions involved in this process, there has been much debate over the dominant mechanism causing this effect. In order to further understand one proposed mechanism, multicomponent ionic exchange, we study the motion of an oil slug through a clay pore throat filled with saline water. The pore throat is modelled as a capillary tube connecting two bulk regions of water. We assume that the surfaces of the oil and the capillary are negatively charged and that, due to repulsion between these surfaces, the oil slug is separated from the capillary surface by a thin film of water. Ion interactions at the oil–water and clay–water interfaces are modelled using the law of mass action. By using lubrication theory to describe the thin-film flow in the water layer separating the oil from the clay surface, and the macroscopic flow through the capillary, we derive expressions for the thickness of the wetting film, and the velocity of the oil slug, given a pressure difference across the ends of the capillary. Numerical results show that the thickness of the water layer and the velocity of the oil slug increase as the salinity of the water is reduced, suggesting that this mechanism contributes to the low-salinity effect. An analytical solution is presented in the limit in which the applied pressure is small.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Figure 1.Schematic diagram of the multicomponent ionic exchange (MIE) mechanism.

Figure 1

Figure 2.Schematic diagram of the macroscopic motion of an oil slug through a capillary between two bulk phases of water.

Figure 2

Figure 3.Schematic diagram of the capillary problem. The thickness of the water layer below the oil slug has been exaggerated for illustrative purposes.

Figure 3

Table 1.Dimensionless parameters defined in §§ 4.1, 3.3 and 2.3.

Figure 4

Table 2.Dimensional parameters.

Figure 5

Figure 4.Schematic diagram of region IV. For $|x-x_{c}^{\ast }|\gg \unicode[STIX]{x1D716}_{1}\unicode[STIX]{x1D716}_{2}^{1/2}$ the bulk water solution is valid, as $H\gg 1$. For $|x-x_{c}^{\ast }|\ll \unicode[STIX]{x1D716}_{1}$ the thin-film solution is valid, as $H_{x}\gg \unicode[STIX]{x1D716}_{1}^{-1}\unicode[STIX]{x1D716}_{2}^{-1}$.

Figure 6

Figure 5.Graphs showing the surface charge densities of the oil–water and clay–water interfaces as a function of the salinity. In (a), the salinity varies between the high-salinity ($\unicode[STIX]{x1D70F}\approx 0$) and low-salinity ($\unicode[STIX]{x1D70F}\approx -6$) regimes used for low-salinity water-flooding experiments. In (b), the salinity ratio is kept constant, and the dimensionless concentration is defined to be $c:=c^{\pm ,2\pm }$. The values of the dimensionless parameters, given in table 1, are $\bar{c}^{1}=100$, $\bar{c}^{2}=18$, ${\mathcal{K}}_{c}^{1}=1.7\times 10^{-2}$, ${\mathcal{K}}_{c}^{2}=0.99$, ${\mathcal{K}}_{o}^{1}=0.01$ and ${\mathcal{K}}_{o}^{2}=1.5\times 10^{-3}$.

Figure 7

Figure 6.Schematic diagram of the three regions at the front meniscus.

Figure 8

Figure 7.Plots of the rear (a) and front (b) transition region profiles, $h(x)$, in the low-salinity ($\unicode[STIX]{x1D70F}=-6$) and high-salinity ($\unicode[STIX]{x1D70F}=0$) regimes, for $P^{\ast }V=9\times 10^{-6}$.

Figure 9

Figure 8.Schematic diagram of the circular solution the oil–water interface approaches.

Figure 10

Figure 9.Schematic diagram of the macroscopic flow problem.

Figure 11

Figure 10.(a) Plot of the film thickness, $h^{\ast }$, as a function of the salinity, $\unicode[STIX]{x1D70F}$. (b) Plots of the corrections to the menisci radii, $r_{1}^{\pm }$, and the difference between the front and rear menisci, $|r_{1}^{+}-r_{1}^{-}|$, as functions of the salinity, $\unicode[STIX]{x1D70F}$. The low-salinity and high-salinity regimes correspond to $\unicode[STIX]{x1D70F}\approx -6$, and $\unicode[STIX]{x1D70F}\approx 0$, respectively.

Figure 12

Figure 11.Plots of the velocity of the oil slug, given by (4.43), as functions of the salinity, $\unicode[STIX]{x1D70F}$, where $\unicode[STIX]{x1D70F}\approx -6$ corresponds to the low-salinity regime, and $\unicode[STIX]{x1D70F}\approx 0$ corresponds to the high-salinity regime: (a) the total velocity, and (b) the two corrections to the velocity. The latter are $V_{1}^{(1)}=(\unicode[STIX]{x1D716}_{2}\unicode[STIX]{x1D6E4}/6P^{\ast })(r_{1}^{-}-r_{1}^{+})$ and $V_{1}^{(2)}=(\unicode[STIX]{x1D716}_{2}\unicode[STIX]{x1D707}^{\ast }L_{o}^{\ast }/(1+(\unicode[STIX]{x1D707}^{\ast }-1)L_{o}^{\ast }))(\unicode[STIX]{x1D707}^{\ast }-1)H^{\ast }$.

Figure 13

Figure 12.(a) Film thickness as a function of the salinity, comparing the numerical solution for $P^{\ast }=9\times 10^{-6}$ with the asymptotic solution in the limit $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }\rightarrow 0$. (b) Film thickness as a function of the dimensionless pressure, $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }$, in the low-salinity regime, comparing the numerical solution with the analytic solution in the limit $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }\rightarrow 0$.

Figure 14

Figure 13.(a) Velocity of the oil slug as a function of the salinity, comparing the numerical solution for $P^{\ast }=9\times 10^{-6}$ with the asymptotic solution in the limit $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }\rightarrow 0$. (b) Velocity as a function of the dimensionless pressure, $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }$, in the low-salinity regime, comparing the numerical solution with the analytic solution in the limit $\unicode[STIX]{x1D716}_{2}^{-3/2}P^{\ast }\rightarrow 0$.

Figure 15

Figure 14.Plots of the rear and front oil–water interface profiles, $h(x)$, in the low-salinity regime, $\unicode[STIX]{x1D70F}=-6$, for $P^{\ast }=10^{-5},10^{-2},10^{-1.5},10^{-1}$.

Figure 16

Figure 15.Velocity of the oil slug, $V$, as a function of the salinity, for $P^{\ast }=10^{-2},10^{-1.5},10^{-1}$.

Figure 17

Figure 16.Plot of the real parts of the roots of (A 5) as $a/b^{2/3}$ varies.