2019
DOI: 10.1016/j.advwatres.2018.12.008
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Effects of grain size and shape distribution on pore-scale numerical simulation of two-phase flow in a heterogeneous porous medium

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Cited by 46 publications
(18 citation statements)
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“…The local Péclet number can be calculated as Pel=u×Lc/D, where u is the velocity, Lc is the characteristic length equal to the average throat width Lc = 8 μm (Rokhforouz & Akhlaghi Amiri, 2019), and D is diffusivity. The mobile zones are generally defined as zones with Pe >> 1 (Chhabra & Shankar, 2018; Smedt & Wierenga, 1984).…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The local Péclet number can be calculated as Pel=u×Lc/D, where u is the velocity, Lc is the characteristic length equal to the average throat width Lc = 8 μm (Rokhforouz & Akhlaghi Amiri, 2019), and D is diffusivity. The mobile zones are generally defined as zones with Pe >> 1 (Chhabra & Shankar, 2018; Smedt & Wierenga, 1984).…”
Section: Resultsmentioning
confidence: 99%
“…We assumed a 2D porous medium from a thin slice of Berea sandstone, first presented by Keller et al (1997) for a micro-model experiment. The geometry has already been used as the computational domain in Basirat et al (2017) and Rokhforouz and Akhlaghi Amiri (2019). The domain measures 660 × 320 μm in size.…”
Section: Model Application For Flow In Porous Mediamentioning
confidence: 99%
“…They aimed to investigate the adequacy of COMSOL in the modelling of unconventional reservoirs and showed that many important areas of EOR methods can be investigated using this package. Finally, they concluded that, although the computational cost and performance of the commercial packages, like CMG, is still better than COMSOL, due to the high variability and flexibility, COMSOL can be used for phenomenological investigation of new EOR methods in pore to core scale (Bogdanov et al 2007;Rokhforouz and Amiri 2019). Bjørnarå and Aker (2008) implemented two-phase flow equations of porous media in COMSOL, which can be very complex depending on the introduced assumptions.…”
Section: Numerical Simulation Backgroundsmentioning
confidence: 99%
“…, where u is the velocity, Lc is the characteristic length equal to the average throat width Lc = 8 μm (Rokhforouz & Akhlaghi Amiri, 2019), and D is diffusivity. The mobile zones are generally defined as zones with Pe >> 1 (Chhabra & Shankar, 2018;Smedt & Wierenga, 1984).…”
Section: Identification Of the Mobile And Immobile Zonesmentioning
confidence: 99%