On the Convergence and Capability of the Large-Eddy Simulation of Concentration Fluctuations in Passive Plumes for a Neutral Boundary Layer at Infinite Reynolds Number.
Concentration moments
Large-eddy simulation grid resolution
Plume dispersion
Probability density function
Turbulence
Journal
Boundary-layer meteorology
ISSN: 0006-8314
Titre abrégé: Boundary Layer Meteorol
Pays: Netherlands
ID NLM: 101622294
Informations de publication
Date de publication:
2020
2020
Historique:
received:
09
10
2019
accepted:
26
05
2020
entrez:
18
8
2020
pubmed:
18
8
2020
medline:
18
8
2020
Statut:
ppublish
Résumé
Large-eddy simulation (LES) experiments have been performed using the Parallelized LES Model (PALM). A methodology for validating and understanding LES results for plume dispersion and concentration fluctuations in an atmospheric-like flow is presented. A wide range of grid resolutions is shown to be necessary for investigating the convergence of statistical characteristics of velocity and scalar fields. For the scalar, the statistical moments up to the fourth order and the shape of the concentration probability density function (p.d.f.) are examined. The mean concentration is influenced by grid resolution, with the highest resolution simulation showing a lower mean concentration, linked to larger turbulent structures. However, a clear tendency to convergence of the concentration variance is observed at the two higher resolutions. This behaviour is explained by showing that the mechanisms driving the mean and the variance are differently influenced by the grid resolution. The analysis of skewness and kurtosis allows also the obtaining of general results on plume concentration fluctuations. Irrespective of grid resolution, a family of Gamma p.d.f.s well represents the shape of the concentration p.d.f. but only beyond the peak of the concentration fluctuation intensity. In the early plume dispersion phases, the moments of the p.d.f. are in good agreement with those generated by a fluctuating plume model. To the best of our knowledge, our study demonstrates for the first time that, if resolution and averaging time are adequate, atmospheric LES provides a trustworthy representation of the high order moments of the concentration field, up to the fourth order, for a dispersing plume.
Identifiants
pubmed: 32801384
doi: 10.1007/s10546-020-00537-6
pii: 537
pmc: PMC7392951
doi:
Types de publication
Journal Article
Langues
eng
Pagination
291-327Informations de copyright
© The Author(s) 2020.
Références
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