2018
DOI: 10.1016/j.advwatres.2018.01.030
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Pore-level influence of micro-fracture parameters on visco-capillary behavior of two-phase displacements in porous media

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Cited by 40 publications
(13 citation statements)
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“…Then, the model is verified under the condition of two‐phase flow, where the solute advection is active. The inaccurate modeling of solute advection can cause the artificial (unphysical) mass transfer near the interface (Maes & Soulaine, 2018, 2020). The artificial mass transfer is induced when the solute advection is not consistent with fluids motion.…”
Section: Numerical Methods and Detailsmentioning
confidence: 99%
See 1 more Smart Citation
“…Then, the model is verified under the condition of two‐phase flow, where the solute advection is active. The inaccurate modeling of solute advection can cause the artificial (unphysical) mass transfer near the interface (Maes & Soulaine, 2018, 2020). The artificial mass transfer is induced when the solute advection is not consistent with fluids motion.…”
Section: Numerical Methods and Detailsmentioning
confidence: 99%
“…The PFM, solving the coupled Cahn‐Hilliard and Navier‐Stokes equations, is already well developed and numerous simulation studies were performed addressing the two‐phase flow system (Akhlaghi Amiri & Hamouda, 2013; Alpak et al., 2016; Jacqmin, 1999; Yue et al., 2004, 2006). In addition, numerous recent studies have applied PFM to study various subsurface flow problems related to fluid viscosity, capillarity, temperature, wettability, heterogeneity, and fractures (Akhlaghi Amiri & Hamouda, 2013, 2014; Basirat et al., 2017; Rokhforouz & Akhlaghi Amiri, 2017, 2018). To our knowledge, PFM has not yet been applied to study reactive transport for two phase flow in porous media.…”
Section: Introductionmentioning
confidence: 99%
“…Because pore‐scale events in spontaneous imbibition, particularly cocurrent spontaneous imbibition, are so quick that current imaging techniques may not capture them, the pore‐scale modeling will be tremendously beneficial. Previous pore‐scale modeling of spontaneous imbibition have been limited to synthetic 2‐D porous media or a porous domain smaller than the REV size (Bakhshian, Rabbani, et al., 2020; Diao et al., 2021; Liu et al., 2020; Rokhforouz & Akhlaghi Amiri, 2018; Zheng et al., 2021). As a result, the obtained pore‐scale information was not upscaled to Darcy‐scale capillary pressure and relative permeability.…”
Section: Introductionmentioning
confidence: 99%
“…Two-phase flow in fractured rocks is relevant to various application, ranging from geothermal energy (Babaei and Nick 2019;Erfani et al 2019), groundwater contamination (Gleeson et al 2009;Sebben et al 2015;Aminnaji et al 2019;Aljuboori et al 2019;Dejam 2019), carbon capturing and storage (Emami-Meybodi et al 2015;Babaei and Islam 2018;Erfani Gahrooei and Joonaki 2018;Dejam and Hassanzadeh 2018;Erfani et al 2020;An et al 2020b;Ershadnia et al 2020), and soil salinization (Weisbrod and Dragila 2006) to enhanced hydrocarbon recovery (Farajzadeh et al 2012;Rokhforouz and Akhlaghi Amiri 2017;Rokhforouz and Amiri 2018;Bakhshi et al 2018;Rabbani et al 2020a;Chen et al 2020;An et al 2020a). The complexity of the fluid flow in highly heterogeneous rocks is caused by the notion that the fluid flows in two different media, matrix block and fracture, which separates the fluids into flowing and stagnant regions due to property contrast (Erfani et al 2019;Hasan et al 2019;Soltanian et al 2019;An et al 2020c;Aziz et al 2020;Rabbani et al 2020b;Hasan et al 2020).…”
Section: Introductionmentioning
confidence: 99%