2017
DOI: 10.1063/1.4976195
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Fluid flows of mixed regimes in porous media

Abstract: In porous media, there are three known regimes of fluid flows, namely, pre-Darcy, Darcy and post-Darcy. Because of their different natures, these are usually treated separately in literature. To study complex flows when all three regimes may be present in different portions of a same domain, we use a single equation of motion to unify them. Several scenarios and models are then considered for slightly compressible fluids. A nonlinear parabolic equation for the pressure is derived, which is degenerate when the … Show more

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Cited by 12 publications
(5 citation statements)
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“…(1978) classified flow in porous media into three regimes: pre‐Darcy flow, Darcy flow, and post‐Darcy flow (Figure 1a). Pre‐Darcy flow occurs mainly in low‐velocity seepage in low‐permeability media at low pressure gradients (Celik et al., 2017; Neuzil, 1986; Siddiqui et al., 2016; Zeng et al., 2011). Based on many experimental and simulation studies, most current scholars agree that the cause of this phenomenon is the formation of a liquid film by the adsorption of fluid on the pore wall (Afsharpoor & Javadpour, 2016; Cai, 2014; Tokunaga, 2009; S. Yang & Yu, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…(1978) classified flow in porous media into three regimes: pre‐Darcy flow, Darcy flow, and post‐Darcy flow (Figure 1a). Pre‐Darcy flow occurs mainly in low‐velocity seepage in low‐permeability media at low pressure gradients (Celik et al., 2017; Neuzil, 1986; Siddiqui et al., 2016; Zeng et al., 2011). Based on many experimental and simulation studies, most current scholars agree that the cause of this phenomenon is the formation of a liquid film by the adsorption of fluid on the pore wall (Afsharpoor & Javadpour, 2016; Cai, 2014; Tokunaga, 2009; S. Yang & Yu, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…Interestingly, there are also physics and engineering problems in which the diffusivity can also vanish when the gradient of the dependent variable vanishes. One example is pre-Darcy flow in saturated porous media [12]. Another example is the spreading of confined layers of non-Newtonian fluids [13,14], for which the complex rheology of the fluid leads to a degenerating gradient-dependent diffusivity (unlike the Newtonian case [8]); see also the review by Ghodgaonkar and Christov [15].…”
Section: Introductionmentioning
confidence: 99%
“…Transport equations for theoretical treatments of porous media flows exist in all of these fields (e.g. see Bear 1972;Celik et al 2017;Fourar et al 2004;Maier et al 2003), but it is difficult to theoretically calculate the boundary conditions for a particular porous matrix based on the geometry of the pores-although some of such attempts have been undertaken, as evident from Freund et al (2003) and Zeiser et al (2003). The publications show that correct flow boundary conditions are needed to solve the available transport equations.…”
Section: Introduction and Objectivesmentioning
confidence: 99%