2016
DOI: 10.1016/j.enganabound.2016.04.001
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Modeling free-surface flow in porous media with modified incompressible SPH

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Cited by 47 publications
(14 citation statements)
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“…A constraint similar to Constraint 1 is not required to be imposed on the size of the support of the kernel function r Υ , since in the macroscopic description of the porous media, the domain is considered as a single phase continuum. Equations (8) and (9) are called the SPH-averaged macroscopic (SPHAM) equations of mass and momentum, respectively, and G * is called the porosity and will be replaced with in the following equations. These equations are defined in a unified framework, ie, they describe the fluid motion over the entire computational domain including both the porous and free-flow regions.…”
Section: The Spham Equationsmentioning
confidence: 99%
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“…A constraint similar to Constraint 1 is not required to be imposed on the size of the support of the kernel function r Υ , since in the macroscopic description of the porous media, the domain is considered as a single phase continuum. Equations (8) and (9) are called the SPH-averaged macroscopic (SPHAM) equations of mass and momentum, respectively, and G * is called the porosity and will be replaced with in the following equations. These equations are defined in a unified framework, ie, they describe the fluid motion over the entire computational domain including both the porous and free-flow regions.…”
Section: The Spham Equationsmentioning
confidence: 99%
“…Regarding the interfacial boundary treatment, they applied a transitional interface layer that is similar to the treatment of Akbari and Namin but with the thickness of the layer being set to one mean diameter of the solid particles of porous medium. Pahar and Dhar developed ISPH models to simulate the interaction of flows with porous media. The interfacial boundary conditions were implicitly implemented by representing the Darcy velocity in the governing equations and incorporating the porosity parameter into the pressure Poisson equation (PPE).…”
Section: Introductionmentioning
confidence: 99%
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“…Earlier research indicated that Darcy's equation is empirically derived to describe the macroscopic characteristics of flow in porous medium (Alazmi & Vafai, 2001;Lage, 1998;Pokrajac, Manes, & McEwan, 2007;Whitaker, 1986;Zeng & Grigg, 2006), which established a relationship between mean porous flow velocity and the pressure gradient in the porous medium. There are several researches using a mesh-free particle method to include the Darcy velocity in the source term in the flow equation to study the interface of fluid and porous structures using SPH model (Gui, Dong, Shao, & Chen, 2015;Pahar & Dhar, 2016) and describe the wetting phenomena on the pore scale (Kunz et al, 2016). As the velocity increases, Darcy's law will overestimate the porous velocity (Chan et al, 2007;Ochoa-Tapia & Whitaker, 1995;Pedras & de Lemos, 2001).…”
Section: Introductionmentioning
confidence: 99%