Geofluids
Volume 2020 (2020), Article ID 5759023, 10 pages
https://doi.org/10.1155/2020/5759023

Research Article

Impact of Pore-Scale Characteristics on Immiscible Fluid Displacement

Nariman Mahabadi,¹ Leon van Paassen,² Ilenia Battiato,³ Tae Sup Yun,⁴ Hyunwook Choo,⁵ and Jaewon Jang⁶

¹Department of Civil Engineering, University of Akron, Akron, Ohio, USA
²School of Sustainable Engineering and the Built Environment, Arizona State University, Tempe, Arizona, USA
³Department of Energy Resources Engineering, Stanford University, Stanford, California, USA
⁴Department of Civil and Environmental Engineering, Yonsei University, Seoul, Republic of Korea
⁵Department of Civil Engineering, Kyung Hee University, Yongin, Republic of Korea
⁶Department of Civil and Environmental Engineering, Hanyang University, Seoul, Republic of Korea

Correspondence should be addressed to Jaewon Jang; jwj@hanyang.ac.kr

Received 9 January 2020; Accepted 2 May 2020; Published 15 May 2020

Academic Editor: Reza Rezaee

Copyright © 2020 Nariman Mahabadi et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract.

Immiscible fluid flows (drainage displacement) where nonwetting fluid invades porous media filled with wetting fluid are frequently observed. Numerous studies have confirmed the existence of three different displacement patterns which depend on the viscosity ratio and capillary number: stable displacement, viscous fingering, and capillary fingering. However, the phase boundary and displacement efficiency of each displacement pattern can vary significantly depending on the characteristics of the experimental and numerical tools employed. In this study, a three-dimensional (3D) tube network model was extracted from 3D X-ray computed tomography images of natural sand. The extracted network model was used to quantitatively outline the phase boundary of the displacement pattern and to examine the displacement efficiency for wide ranges of viscosity ratios and capillary numbers. Moreover, the effects of the tube size distribution and tube connectivity on the displacement characteristics were investigated. A transition regime between the viscous fingering and capillary fingering zones with regard to the displacement efficiency was observed for the first time. As the tube size distribution became uniform, the viscosity effect increased. As the tube connectivity decreased to ~4.6, the phase boundary became similar to that of a two-dimensional network. The characteristic changes of the phase boundary and displacement efficiency were highlighted through local gradient diagrams.

1. Introduction

Immiscible fluid flow is frequently observed in various engineering applications, such as enhanced oil and gas recovery, geological CO₂ sequestration, and soil remediation. While the invading fluid is injected into porous media through an injection well, the defending fluid in the pore space is displaced until the invading fluid reaches a drainage well. Consequently, multiple preferential flow channels are formed. When a nonwetting invading fluid displaces a wetting defending fluid, called drainage displacement, the pattern of fluid invasion and displacement depends on several parameters, such as the viscosity ratio, interfacial tension, injection rate, and wettability, as well as the characteristics of the porous media [1].

The viscosity ratio is defined as the ratio of the viscosity of the invading fluid () to that of the defending fluid (). The capillary number is defined as the ratio of the viscous force to the capillary force:

Here, (m³/s) represents the flow rate of the invading fluid, (m²) represents the cross-sectional area normal to the fluid direction, (N/m) represents the interfacial tension between the invading and defending fluids, and represents the contact angle at the interface between the invading and defending fluids on the pore surface.

Previous studies have indicated that three displacement patterns can be distinguished, which are illustrated in the plot shown in Figure 1 [1–3]. The boundaries for each displacement zone proposed by Lenormand et al. [1], Zhang et al. [2], and Liu et al. [3] are superimposed on Figure 1. Viscous fingering occurs when a less viscous invading fluid displaces a more viscous defending fluid in porous media (i.e., negative value). The displacement pattern is characterized by the formation of tree-like fingers with no loops. The principal force is the viscosity of the defending fluid, because capillary effects in the invading fluid are negligible. Capillary fingering prevails at low capillary numbers where viscous forces in both fluids are negligible compared with capillary force. During displacement, an invading fluid forms fingers, which grow in all directions and eventually form loops that trap the clusters of a defending fluid. Stable displacement occurs at relatively high capillary numbers and viscosity ratios, where the dynamics are primarily controlled by the viscous forces of the fluid invading at a relatively high flow rate. A straight invading front perpendicular to the invading direction is formed, and few trapped clusters of the defending fluid are observed.

Figure 1: Boundaries of three displacement patterns with respect to and : stable displacement (upper right), viscous fingering (left), and capillary fingering (lower right). The symbols (circle, triangle, and square) represent the values of and used for the microfluidic chip experiment and the pore-network model or a lattice Boltzmann simulation in the literature. The lines indicate the phase boundaries identified in previous studies. The values of and used in previous studies have a very limited range, particularly in the transition zone. A wide range of and values (represented by grey dots) was used in the present study.

After the invading fluid reaches the drainage well and displacement no longer occurs, the final saturation of the invading fluid is known as the displacement efficiency, which is the highest in stable displacement and the lowest in viscous fingering [4].

Numerous methods have been used to study immiscible fluid flows, including numerical simulations, e.g., tube network models, or lattice Boltzmann simulations [1, 3, 5, 6] and laboratory displacement experiments using microfluidic chips [2, 4, 7, 8]. The invasion pattern is affected by several parameters, such as the pore morphology (e.g., pore size distribution and connectivity), fluid property (e.g., viscosity and density), fluid-wall interaction (e.g., wettability), and flow rate. This complexity makes both experiments and numerical simulations challenging [1]. In experiments, it is difficult to control various parameters and observe three-dimensional (3D) pore-scale phenomena. In numerical simulations, solving the Navier-Stokes equation under multiphase flow conditions is computationally demanding. Alternative approaches, such as lattice Boltzmann simulations, have a limited capability to properly model all the fluid properties and implement boundary conditions. Owing to these difficulties, few experimental and numerical studies considering various pore-scale characteristics and fluid properties have been performed in the 3D domain [9]. Tube network models are simple yet effective for simulating fluid invasion and displacement by applying the various parameters. Therefore, the objectives of this study were to provide the displacement efficiency values in the 3D domain and to investigate the effects of the pore-scale characteristics and fluid properties on the displacement pattern.

In this study, we used 3D tube networks to simulate the drainage displacement for wide ranges of capillary numbers and viscosity ratios. We also examined the effects of the tube size distribution and connectivity on the phase boundary, displacement pattern, and displacement efficiency.

2. Numerical Method and Procedure

2.1. Tube Network Extraction

A sandy sediment recovered from the Mallik 5L-38 site (gas hydrate reservoir) at a depth of 1091 m was selected for X-ray computed tomography (CT) scanning and tube network extraction. Detailed information regarding X-ray CT scanning was presented by Mahabadi et al. [10]. In the present study, the volume of the CT image was 8 mm³ () (Figure 2(a), left). A 3D tube network was extracted from the CT images using the maximal ball algorithm developed by Silin and Patzek [11] (Figure 2(a), right). The maximal ball algorithm searches for all possible spheres that can be inscribed within a pore. After the search, the big spheres located at the centers of the pore spaces become the pores of the pore-network model, and the small spheres inscribed in pore throats become tubes connecting adjacent pores. A detailed description of the method was presented by Dong and Blunt [12]. The 3D tube network model extracted from the X-ray image of in situ sediment represents the real pore structure well, because the pore-scale characteristics, such as the connectivity, pore size, and pore length, are used to generate the tube networks. In this study, a network model consisting of only tubes, called tube network or bond-network model, was used. Thus, no pore volume was considered, and the tube length was the distance between the centers of two neighboring pores. The obtained 3D tube network model consisted of 5775 tubes, with a mean tube-coordination number (connectivity) of , a mean tube size of , and a standard deviation of the logarithmic tube size of .

(a)

(b)

Figure 2: Tube network model extraction and modification. (a) X-ray CT image of a specimen (left) and the extracted tube network model (right). The dimensions of the network model were , and the model comprised 5775 tubes with a coordination number of . (b) Four tube size distributions used to modify the extracted tube network model. Three additional tube size distributions with different standard deviations (, , and ) were generated. The average tube size was kept constant, along with the tube-size rank order of the individual tubes.

2.2. Tube Size Distributions

Four tube size distributions were used in this study. The average value in the tube size distribution and the rank of the individual tubes were kept constant, and the standard deviations were , , , and , where represents the standard deviation of the original tube network model extracted from the CT images. Lower values correspond to more uniform tube size distributions. Figure 2(b) shows the four tube size distributions used in this study. The other parameters of the tube size distribution, such as the coordination number, tube location and direction, and tube length, were kept constant.

2.3. Coordination Numbers

Several studies have used two-dimensional (2D) tube networks with a homogeneously distributed pore space and a fixed coordination number, e.g., [1–3]. The degree of heterogeneity and the coordination numbers typically tend to be higher for in situ sediments, compared with the regular 2D tube network model. The coordination number of the original tube network extracted from the CT image is . In this study, the effect of the connectivity was investigated using tube networks with four different coordination numbers (, 6.2, 5.1, and 4.6), which are similar to the values employed in other studies [13–16].

The coordination number is reduced by randomly selecting tubes and removing them from the original tube network to generate tube network models with a lower coordination number while keeping the tube size distribution constant.

2.4. Simulation Algorithm for Fluid Invasion

The algorithm developed by Aker et al. [17] was used in this study. This algorithm considers the dynamics of the temporal evolution of the fluid flow and the time dependency of the interface between the invading and defending fluids. Initially, the tube network model is fully saturated with the defending fluid with viscosity . Then, the invading fluid with viscosity is injected through an inlet boundary at a constant injection rate. Here, we study the drainage displacement; therefore, the invading fluid is nonwetting and the defending fluid is in the wetting phase. It is assumed that the two fluids are immiscible; thus, an explicit interface exists between the defending and invading fluids.

Consider a cylindrical tube containing both invading and defending fluids. The capillary pressure at the interface between the two fluids is given by the Young-Laplace equation:

where (N/m) represents the interfacial tension, (m) represents the tube radius, and (°) represents the contact angle. Aker et al. [17] modified the Young-Laplace equation to consider the capillary pressure in hour glass-shaped tubes where the capillary pressure depends on the position of the meniscus inside the tubes. Accordingly, the capillary pressure can be expressed as a function of the meniscus position inside the tube:

where represents the relative position of the meniscus, which ranges from 0 to 1 (0 at the beginning of the tube and 1 at the end of the tube). In this study, the contact angle was set as zero () for a perfect wetting condition. The proposed modification in Young-Laplace equation allows the model to simulate the burst drainage displacement dynamics of a multiphase flow system: nonwetting fluid advances to the narrower part of a tube with increasing capillary pressure. After the meniscus passes the pore throat, the invading fluid abruptly occupies some parts of connected tubes.

The volume flux through a cylindrical tube is calculated using the Washburn equation:

where represents the effective viscosity and represents the pressure difference between the two sides of a capillary tube. For a cylindrical tube without a meniscus, Equation (6) reduces to a Hagen-Poiseuille equation with or .

For an incompressible fluid, the mass-balance equation is

i.e., the sum of all fluxes into and out of a given node should be zero. Application of Equation (7) to every internal node in the tube network enables the calculation of the pressures at every internal node via the conjugate gradient method. Thus, the pressure difference across the network can be determined. Because the pressure gradient at a constant flow rate must be obtained, one must determine the nodal pressures at a constant injection rate. The flow rate in the tube network model is given as

where and are parameters that depend on the properties of the fluid and the geometry of the porous medium and represents the pressure difference between the inlet and the outlet of the network model. These parameters and can be calculated by solving the nodal pressures for two differential pressures and and corresponding flow rates and . After determining the coefficients and , is calculated for the desired constant flow rate. Then, all the nodal pressures are computed by solving Equation (7) for a given pressure difference . A detailed explanation was presented by Aker et al. [17].

The timestep is selected such that only one meniscus among the menisci in all tubes in the network model can reach the other end of the tube in each timestep during invasion:

Here, represents the distance between the meniscus and the end of the tube, and represents the flow velocity in the tube, which can be calculated using the flow rate and the tube radius: . At each timestep, the minimum is calculated and is used for the next timestep. The new position of the meniscus is calculated and is updated using a second-order Runge-Kutta scheme.

3. Typical Characteristics of Invasion Simulation

Typical displacement patterns for selected capillary numbers and viscosity ratios are shown in Figure 3. The simulation results clearly indicate that the displacement patterns were affected by the values of and . At a low viscosity ratio (, Figure 3(a)), tree-like displacement patterns and a clear single preferential flow path developed. In this case, the saturation of the invading fluid at the end of the invasion increased slightly, from 0.066 to 0.074, as the capillary number decreased from to . At a low capillary number (, bottom row of Figure 3), the displacement pattern changed from viscous fingering to capillary fingering as the viscosity ratio increased from to . Patterns of stable displacement were observed for a high viscosity ratio () and high capillary number (). The final saturation for stable displacement was approximately 0.7 for and .

Figure 3: Typical invasion patterns for selected and conditions. The fluid invaded from the left boundary to the right boundary.

After the invasion process was completed, the tube network model with dimensions of was divided equally into five sections along the flow direction. The “local” saturation of the invading fluid in each internal section was calculated for nine values of and (Figure 4(a)). Depending on the specific phase boundary proposed in the literature, the points (, ) in the phase diagram were categorized into either one of the three displacement zones (viscous fingering, capillary fingering, and stable displacement zone) or the transition zone (between the three displacement-pattern zones). Here, the noticeable observation is that in the intermediate zone at , the displacement efficiency decreases as the capillary number increases, not like at the condition of .

(a)

(b)

Figure 4: Local saturation of the invading fluid in the tube network model (with and ) for different and conditions. (a) Nine sets of and values used to calculate the saturation of the invading fluid, superimposed on phase boundaries suggested by other researchers. Each symbol represents and conditions used for the local saturation plot in (b). (b) Local saturation of the invading fluid with respect to the distance from an input boundary.

As shown in Figure 4(b), the local saturations for the nine investigated cases were spatially inhomogeneous and decreased from the inlet to the outlet. For the three cases with (which correspond to capillary fingering when , the transition zone for , and stable displacement when ), the saturations of the 1st and 2nd internal sections were almost and then decreased to approximately 0.5% in the last section near the outlet boundary. As the log capillary number increased from –5 to 0 and 5, the local saturations in the 3rd and 4th internal sections increased, resulting in an overall increase in the “global” saturation, because the displacement pattern changed from capillary fingering to stable displacement, through the transition zone. However, for the three cases of (in the transition zone), the “local” saturation for a given internal section decreased as the capillary number increased from –5 to 5. This effect was most pronounced for the 1st, 2nd, and 3rd internal sections, because the displacement pattern changed from capillary fingering to the transition zone in the proximity of the viscous fingering zone. As shown in Figure 5, the saturation was higher in the capillary fingering zone than in the transition zone, particularly near the viscous fingering zone. For the three cases of , the “local” saturation started decreasing in the first section and remained almost constant between the second and last sections for a given value. Note that the saturation averaged for the five internal sections was the same as the “global” saturation in Figure 5.

Figure 5: Effects of the viscosity ratio and capillary number on the displacement efficiency for the original tube network model ( and ).

4. Effects of Viscosity Ratio and Capillary Number on Displacement Efficiency

The viscosity ratios and capillary numbers used in this study ranged from to 10 and from to 10, respectively. A total of 441 simulation runs were performed using 21 viscosity ratios and 21 capillary numbers, with the original tube network model.

The obtained displacement efficiency with respect to the viscosity ratio and capillary number is shown in a contour plot (Figure 5). Three displacement zones, i.e., stable displacement (denoted by S), viscous fingering (V), and capillary fingering (C), are identified with regard to the displacement efficiency. A fourth zone (denoted by “V-C,” lower left in the phase diagram) is separated from the conventional capillary fingering zone, because the displacement efficiency in the “V-C” zone is significantly lower than that in the capillary fingering zone. The “V-C” zone has an intermediate displacement efficiency between those of the viscous fingering and capillary fingering zones. The displacement efficiency values in the zones divided by the dashed lines in Figure 5 were used to calculate the average value of saturation (displacement efficiency). The displacement efficiencies in the transition zones and near these boundaries were excluded from the calculation. The average value of the displacement efficiency was 0.68 for the stable displacement zone, 0.53 for the capillary fingering zone, and 0.07 for the viscous fingering zone. The average displacement efficiency in the “V-C” zone was . In the three displacement-pattern zones, i.e., stable displacement, capillary fingering, and viscous fingering, the coefficient of variation for the displacement efficiency values for nine neighboring points (obtained for three consecutive values on each and axis) was <0.1. However, the “V-C” zone exhibited an increasing trend in the displacement efficiency from the viscous fingering zone to the capillary fingering zone. Furthermore, the boundary between the stable displacement and capillary fingering zones could not be clearly identified according to the displacement efficiency only.

5. Impact of Pore-Scale Characteristics on Displacement

Additional simulations were performed using three different tube size distributions and three different coordination numbers () to investigate the effects of the pore-scale characteristics on the displacement patterns. Figures 6(a) and 7(a) show contour maps of the displacement efficiency for four different tube size distributions and coordination numbers, respectively. Results for the original tube network model are also presented.

(a)

(b)

Figure 6: Effect of the tube size distribution on the displacement efficiency for the tube network model with a coordination number of . The tube size distribution changes from to σ = 0.1σ₀. (a) Saturation of the invading fluid. The average saturation is shown for each zone. (b) Gradient in the displacement efficiency distribution.

(a)

(b)

Figure 7: Effect of the coordination number on the displacement efficiency for the tube network model with a given tube size distribution (). (a) Saturation of the invading fluid. The coordination number is reduced from to by removing randomly chosen tubes from the original tube network model. (b) Gradient in the displacement efficiency distribution.

5.1. Effect of Tube Size Distribution on Displacement Efficiency

In Figure 6(a), each contour map contains the results of 441 simulation runs for 21 viscous ratios and 21 capillary numbers. For stable displacement and viscous fingering, the displacement efficiency decreased as the standard deviation of the tube size distribution decreased. However, this trend was not observed in the capillary zone; the tube network with the original standard deviation () exhibited a saturation of , whereas the values of were 0.57, 0.58, and 0.59 for , , and , respectively. Thus, the difference in the displacement efficiency between the “C” and the “S” zones decreased.

For these simulations using different tube size distributions (Figure 6), the rank of tube size in the tube network model was maintained constant even though the tube size distribution varies. As the tube size distribution increases, there occur more numbers of larger- and smaller-sized tubes. Due to the same rank of tube size, the number of tubes invaded at the end of the invasion might be similar or the same for the tube network models with different tube size distributions, which results in higher saturation (or displacement efficiency) for the condition of higher tube size distribution. In order words, the same number of tubes is invaded, but they might be larger tubes. However, this phenomenon is not pronounced in the capillary fingering zone. The possible reason might be that multiple tubes with the similar capillary pressures could be invaded simultaneously, which results in higher displacement efficiency for lower tube size distribution condition.

Moreover, as the standard deviation of the tube size distribution decreased, the vertical boundaries separating the viscous fingering and stable displacement zones moved to higher values of (from –5 to –2) in the plot. Furthermore, the displacement efficiency in the “V-C” zone decreased and approached saturation value in the “V” zone. Thus, when the tube network model had a uniform tube size distribution, the displacement pattern was determined predominantly by the viscosity of both fluids, rather than by capillarity effects in the tube network. The boundary between the stable displacement and capillary fingering zones became unclear as the difference in the average displacement efficiency between stable displacement and capillary fingering decreased, for a uniform tube size distribution. This trend is highlighted in Figure 6(b), which shows the gradient of the displacement efficiency. High gradients (i.e., large changes in the displacement efficiency) are observed in the transition zone, which is shown in red. For , high gradients between four displacement-pattern zones (S, V, C, and V-C) are observed, and the boundary between stable displacement and capillary fingering is clearly identifiable. As the standard deviation of the tube size distribution decreases, the boundary between the “S” and “C” zones becomes unclear, and viscosity effects increase.

5.2. Effect of Coordination Number on Displacement Efficiency

Contour maps of the displacement efficiency are shown in Figure 7(a). The simulation results indicate that the displacement efficiency for each displacement pattern (V, S, and C) decreased as the coordination number decreased. However, the displacement efficiency in the “V-C” zone exhibited the opposite trend. As the coordination number decreased, the difference in the displacement efficiencies between the “V-C” and “C” zones decreased. Additionally, the boundary between the viscous fingering and capillary fingering zones became clearer. The shape and location of the boundaries for the lowest coordination number, i.e., (Figure 7(a), right), were very similar to those of the boundaries suggested by Lenormand et al. [1], Liu et al. [3], and Zhang et al. [2], where . This trend is also observed in Figure 7(b). For a given standard deviation , the gradient of the displacement efficiency clearly exhibited a change in the phase boundaries as the coordination number decreased.

5.3. Limitations

The results of this study are applicable to several immiscible fluid flow conditions, such as those in CO₂ sequestration, soil contamination and remediation, fluid control using Pickering emulsions, enhanced oil and gas recovery, and gas hydrate production [4, 18–21]. However, a few assumptions and limitations must be considered for applications. (1) The tube network is millimeter-scale, in contrast to kilometer-scale in situ applications. This limitation may be resolved by obtaining constant local saturation values using a longer tube network. For field application, as long as the and values are accurately identified depending on the distance from the input well, the corresponding displacement efficiency can be predicted using the constant local saturation values obtained from the network model simulation. (2) Even in the small tube network, the local saturation varies significantly owing to the capillary end effect. This phenomenon can be minimized by using a longer network or controlled outflow boundary [22]. (3) The shape of real pore spaces is not perfectly cylindrical. The capillary pressure for irregularly shaped pores found in in situ conditions differs from that for perfectly circular pores [23]. (4) The contact angle and interfacial tension vary depending on the in situ conditions [24]. (5) The invading fluid with a high flow rate may affect the configuration of sediment particles (e.g., the redistribution of sediment particles) [25, 26]; however, in this study, it was assumed that the pore shape did not change during the invasion. (6) A constant flow rate condition was selected in this study to evaluate the displacement efficiency for a given condition, and the results might be different if other boundary conditions are used. Moreover, in in situ applications, the invasion rate may decrease as the invading fluid spreads in the radial direction from an injection well.

6. Conclusions

The displacement efficiency values of an immiscible fluid flow were obtained for a wide range of and values in the 3D domain, using tube networks. The effects of the pore-scale characteristics, such as the tube size distribution and tube connectivity, on the displacement efficiency were investigated. The main findings of this study are presented below:

(i)The dynamic invasion process resulted in saturation gradients inside the tube network. After invasion is complete, the saturation of the invading fluid is higher near the inlet and decreases toward the outlet(ii)Three displacement patterns were observed, similar to previous studies. Additionally, a fourth “V-C” zone that was previously part of the capillary fingering zone was defined by the displacement efficiency gradually increasing from the viscous fingering zone to the capillary fingering zone(iii)The displacement efficiency obtained via a 3D tube network simulation was for the stable displacement zone, for the viscous fingering zone, for the capillary fingering zone, and for the “V-C” zone(iv)As the tube size distribution became narrower distribution, the boundaries between the stable displacement and capillary fingering zones and between the viscous fingering and “V-C” zones became unclear. Additionally, the boundary between the viscous fingering and stable displacement zones moved to a higher value. The displacement efficiency is affected dominantly by the viscosity ratio in the tube network especially when the tube size distribution becomes uniform. The displacement efficiency decreased with the increasing uniformity of the tube size distribution for stable displacement and viscous fingering(v)As the coordination number (indicating the tube connectivity) decreased from 8.0 to 4.6, the boundary between the viscous fingering and “V-C” zones became clear. This is similar to the phase boundary reported in the literature. The displacement efficiency decreased with the decreasing coordination number for the stable displacement, viscous fingering, and capillary fingering zones

Data Availability

The data presented in this study are available at http://jwjang1977.wixsite.com/mysite/data.

Conflicts of Interest

The authors declare that there is no conflict of interest regarding the publication of this paper.

Acknowledgments

This work was supported by a research fund provided by the Korea Agency for Infrastructure Technology Advancement (19CTAP-C142849-02) and National Research Foundation of Korea (NRF-2018R1D1A1B07042530).

References

R. Lenormand, E. Touboul, and C. Zarcone, “Numerical models and experiments on immiscible displacements in porous media,” Journal of Fluid Mechanics, vol. 189, pp. 165–187, 1988.

C. Zhang, M. Oostrom, T. W. Wietsma, J. W. Grate, and M. G. Warner, “Influence of viscous and capillary forces on immiscible fluid displacement: pore-scale experimental study in a water-wet micromodel demonstrating viscous and capillary fingering,” Energy & Fuels, vol. 25, no. 8, pp. 3493–3505, 2011.

H. Liu, A. J. Valocchi, Q. Kang, and C. Werth, “Pore-Scale Simulations of Gas Displacing Liquid in a Homogeneous Pore Network Using the Lattice Boltzmann Method,” Transport in Porous Media, vol. 99, no. 3, pp. 555–580, 2013.

X. Zheng, N. Mahabadi, T. S. Yun, and J. Jang, “Effect of capillary and viscous force on CO2 saturation and invasion pattern in the microfluidic chip,” Journal of Geophysical Research, vol. 122, pp. 1634–1647, 2017.

E. Aker, K. J. Måløy, and A. Hansen, “Simulating temporal evolution of pressure in two-phase flow in porous media,” Physical Review E, vol. 58, no. 2, pp. 2217–2226, 1998.

S. H. Lee, L. Padmanabhan, and H. A. Al-Sunaidi, “Simulation of linear displacement experiments on massively parallel computers,” SPE Journal, vol. 1, no. 3, pp. 327–340, 2013.

I. Razmavar, F. M. Alami, M. R. Rasaei, and M. Nadafpour, “Microscopic fractal-dimension study of rate and viscosity changes on displacement pattern by use of 2D glass micromodel,” SPE Reservoir Evaluation & Engineering, vol. 20, no. 1, pp. 8–18, 2017.

J. Sharma, S. B. Inwood, and A. Kovscek, “Experiments and analysis of multiscale viscous fingering during forced imbibition,” SPE Journal, vol. 17, no. 4, pp. 1142–1159, 2013.

S. Bakhshian, S. A. Hosseini, and N. Shokri, “Pore-scale characteristics of multiphase flow in heterogeneous porous media using the lattice Boltzmann method,” Scientific Reports, vol. 9, no. 1, p. 3377, 2019.

N. Mahabadi, X. Zheng, T. S. Yun, L. van Paassen, and J. Jang, “Gas bubble migration and Trapping in porous media: pore-scale simulation,” Journal of Geophysical Research - Solid Earth, vol. 123, no. 2, pp. 1060–1071, 2018.

D. Silin and T. Patzek, “Pore space morphology analysis using maximal inscribed spheres,” Physica A: Statistical Mechanics and its Applications, vol. 371, no. 2, pp. 336–360, 2006.

H. Dong and M. J. Blunt, “Pore-network extraction from micro-computerized-tomography images,” Physical Review E, vol. 80, no. 3, 2009.

R. I. Al-Raoush and C. S. Willson, “Extraction of physically realistic pore network properties from three- dimensional synchrotron X-ray microtomography images of unconsolidated porous media systems,” Journal of Hydrology, vol. 300, no. 1-4, pp. 44–64, 2005.

M. Yanuka, F. A. L. Dullien, and D. E. Elrick, “Percolation processes and porous media: I. Geometrical and topological model of porous media using a three-dimensional joint pore size distribution,” Journal of Colloid and Interface Science, vol. 112, no. 1, pp. 24–41, 1986.

R. M. Sok, M. A. Knackstedt, A. P. Sheppard et al., “Direct and stochastic generation of network models from tomographic images; effect of topology on residual saturations,” Transport in Porous Media, vol. 46, no. 2/3, pp. 345–371, 2002.

W. B. Lindquist and A. Venkatarangan, “Pore and throat size distributions measured from synchrotron X-ray tomographic images of Fontainebleau sandstones,” Journal of Geophysical Research, vol. 105, no. B9, pp. 21509–21527, 2000.

E. Aker, K. J. Måløy, A. Hansen, and G. G. Batrouni, “A two-dimensional network simulator for two-phase flow in porous media,” Transport in Porous Media, vol. 32, no. 2, pp. 163–186, 1998.

N. Mahabadi, S. Dai, Y. Seol, and J. Jang, “Impact of hydrate saturation on water permeability in hydrate-bearing sediments,” Journal of Petroleum Science and Engineering, vol. 174, pp. 696–703, 2019.

J. Jang and J. C. Santamarina, “Hydrate bearing clayey sediments: Formation and gas production concepts,” Marine and Petroleum Geology, vol. 77, pp. 235–246, 2016.

X. Zheng and J. Jang, “Hydraulic properties of porous media saturated with nanoparticle-stabilized air-water foam,” Sustainability, vol. 8, no. 12, p. 1317, 2016.

R. J. Glass, S. H. Conrad, and W. Peplinski, “Gravity-destabilized nonwetting phase invasion in macroheterogeneous porous media: Experimental observations of invasion dynamics and scale analysis,” Water Resources Research, vol. 36, no. 11, pp. 3121–3137, 2000.

D. H. Kang and T. S. Yun, “Minimized capillary end effect during CO2 displacement in 2-D micromodel by manipulating capillary pressure at the outlet boundary in lattice Boltzmann method,” Water Resources Research, vol. 54, no. 2, pp. 895–915, 2018.

H. S. Suh, D. H. Kang, J. Jang, K. Y. Kim, and T. S. Yun, “Capillary pressure at irregularly shaped pore throats: Implications for water retention characteristics,” Advances in Water Resources, vol. 110, pp. 51–58, 2017.

X. Zheng, A. C. Barrios, F. Perreault, T. S. Yun, and J. Jang, “Interfacial tension and contact angle in CO2-water/nanofluid-quartz system,” Greenhouse Gases: Science and Technology, vol. 8, no. 4, pp. 734–746, 2018.

N. Mahabadi and J. Jang, “The impact of fluid flow on force chains in granular media,” Applied Physics Letters, vol. 110, no. 4, article 041907, 2017.

X. Zheng, F. Perreault, and J. Jang, “Fines adsorption on nanoparticle-coated surface,” Acta Geotechnica, vol. 13, no. 1, pp. 219–226, 2018.