2016
DOI: 10.1016/j.cageo.2016.01.011
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SediFoam: A general-purpose, open-source CFD–DEM solver for particle-laden flow with emphasis on sediment transport

Abstract: With the growth of available computational resource, CFD-DEM (computational fluid dynamics-discrete element method) becomes an increasingly promising and feasible approach for the study of sediment transport. Several existing CFD-DEM solvers are applied in chemical engineering and mining industry. However, a robust CFD-DEM solver for the simulation of sediment transport is still desirable. In this work, the development of a threedimensional, massively parallel, and open-source CFD-DEM solver SediFoam is detail… Show more

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Cited by 120 publications
(81 citation statements)
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References 42 publications
(66 reference statements)
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“…In contrast, when Θ r t < Θ < Θ e t , particles entrained by turbulent events continuously rebound for comparably longer periods before they deposit again, giving rise to intermittent bulk transport and significant transport autocorrelations, as often observed in aeolian (Bauer & Davidson-Arnott, 2014;Baas & Sherman, 2005;Carneiro et al, 2015;Dupont et al, 2013;Ellis et al, 2012;Lee, 1987;Martin et al, 2013;Pfeifer & Schönfeldt, 2012;Rasmussen & Sørensen, 1999;Sherman et al, 2018;Spies et al, 2000;Stout & Zobeck, 1997) and fluvial systems (Ancey et al, 2006(Ancey et al, , 2008Dinehart, 1999;Drake et al, 1988;Heathershaw & Thorne, 1985;Heyman et al, 2013;Lee & Jerolmack, 2018). The closer Θ comes to the impact entrainment threshold Θ e t , the more such continuously rebounding particles the flow can carry, which increases the probability of impact entrainment events (section 4.2) and thus further enhances transport autocorrelation.…”
Section: Intermittent Bulk Transport ( R T < < E T )mentioning
confidence: 99%
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“…In contrast, when Θ r t < Θ < Θ e t , particles entrained by turbulent events continuously rebound for comparably longer periods before they deposit again, giving rise to intermittent bulk transport and significant transport autocorrelations, as often observed in aeolian (Bauer & Davidson-Arnott, 2014;Baas & Sherman, 2005;Carneiro et al, 2015;Dupont et al, 2013;Ellis et al, 2012;Lee, 1987;Martin et al, 2013;Pfeifer & Schönfeldt, 2012;Rasmussen & Sørensen, 1999;Sherman et al, 2018;Spies et al, 2000;Stout & Zobeck, 1997) and fluvial systems (Ancey et al, 2006(Ancey et al, , 2008Dinehart, 1999;Drake et al, 1988;Heathershaw & Thorne, 1985;Heyman et al, 2013;Lee & Jerolmack, 2018). The closer Θ comes to the impact entrainment threshold Θ e t , the more such continuously rebounding particles the flow can carry, which increases the probability of impact entrainment events (section 4.2) and thus further enhances transport autocorrelation.…”
Section: Intermittent Bulk Transport ( R T < < E T )mentioning
confidence: 99%
“…The numerical model of sediment transport in a Newtonian fluid by Durán et al () belongs to a new generation of sophisticated grain‐scale models of sediment transport (Arolla & Desjardins, ; Carneiro et al, , , ; Clark et al, , ; Derksen, ; Durán et al, , ; Durán et al, ; Durán et al, ; Elghannay & Tafti, , ; Finn & Li, ; Finn et al, ; González et al, ; Ji et al, ; Kidanemariam & Uhlmann, , , ; Maurin et al, , , ; Pähtz & Durán, ; Pähtz, Durán, et al, ; Pähtz, Omeradžić, et al, ; Schmeeckle, ; Seil et al, ; Sun & Xiao, ; Vowinckel et al, , ). It couples a discrete element method for the particle motion with a continuum Reynolds‐averaged description of hydrodynamics, which means that it neglects turbulent fluctuations around the mean turbulent flow.…”
Section: Numerical Model Descriptionmentioning
confidence: 99%
“…The coupled solver is developed by Sun and Xiao [21], and the source code is available at https://github.com/xiaoh/sediFoam. The detailed algorithms of this solver are published in [22,23] and it has been rigorously verified and validated in a wide range of application areas, such as the fluidized bed [24], sediment transport [21] and sand dune migration [25]. Here, a block flow diagram of sediFoam is shown in Fig.…”
Section: Coupled Cfd-dem Approachmentioning
confidence: 99%
“…The averaging process was introduced in [21,22]. The right terms of the momentum conservation equation are the pressure gradient ∇ , the divergence of the stress tensor , gravity g, and fluid-particle interaction forces , which is the averaged interaction force from every individual particle in a fluid cell.…”
Section: Fig 1 the Block Flow Diagram Of Sedifoammentioning
confidence: 99%
“…Block diagram of CFD-DEM coupling. Diagram adopted from [36]. Fluid dynamics is solved in the CFD module and particle motion is solved in the DEM module.…”
mentioning
confidence: 99%