2019
DOI: 10.1007/s00703-019-00689-2
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CFD simulation of dense gas dispersion in neutral atmospheric boundary layer with OpenFOAM

Abstract: In this study, MOST (Monin-Obukhov Similarity Theory) is used to specify the profiles of velocity, turbulent kinetic energy (k) and eddy dissipation rate (ǫ) in ABL (Atmospheric Boundary Layer) flow. The OpenFOAM standard solver buoyantSimpleF oam is modified to simulate neutrally stratified ABL. The solver is able to obtain equilibrium ABL. For gas dispersion simulation, buoyantN onReactingF oam is developed to take into accounts fluid properties change due to temperature, buoyancy effect and variable turbule… Show more

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Cited by 10 publications
(4 citation statements)
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“…The simulation of the atmospheric boundary layer poses a challenge for CFD. The main problem lies in the inherently turbulent nature of the atmospheric flow and cloud formation, further complicated by the orography of the terrain and the buildings [22,23]. A realistic wind flow requires taking into account many details like changes in transport properties with temperature and pressure, as well as the boundary conditions in contact with the terrain or in the top of the simulation domain.…”
Section: Resultsmentioning
confidence: 99%
“…The simulation of the atmospheric boundary layer poses a challenge for CFD. The main problem lies in the inherently turbulent nature of the atmospheric flow and cloud formation, further complicated by the orography of the terrain and the buildings [22,23]. A realistic wind flow requires taking into account many details like changes in transport properties with temperature and pressure, as well as the boundary conditions in contact with the terrain or in the top of the simulation domain.…”
Section: Resultsmentioning
confidence: 99%
“…The simulation of the atmospheric boundary layer possess a challenge for CFD. The main problem lies in the inherently turbulent nature of the atmospheric flow and the cloud formation, further complicated by the orography of the terrain and the buildings [19,20]. A realistic wind flow requires taking into account many details like the changes of the transport properties with temperature and pressure, as well as the boundary conditions in contact with the terrain or in the top of the simulation domain.…”
Section: Resultsmentioning
confidence: 99%
“…This model is equivalent to Equations ( 20)- (22). Although the use of this model on the mesoscale is not the common choice, there exist several applications of corresponding models [55][56][57][58][59]. One possibility for hybridizing this model is to consider a variable α * (instead of a constant α) combined with an appropriate calculation of α * .…”
Section: Stratified Flowsmentioning
confidence: 99%