Atmospheric CFD modelling
for environmental applications
at local scale
B. Carissimo, S. Lacour, H. Foudhil, L. Musson-Genon, E. Dupont, D. Wendum,
M. Milliez, B. Albriet, E. Demael, L. Laporte,
Outline
•
Objectives
•
Focus : concentration fluctuations
•
Overview : other activities
Animation Wind tunnel
Objectives
Develop an integrated modelling tool for studies of the
atmospheric environment at local scale
Dispersion of pollutants and its impact on population and
environment in urban and around industrial areas.
Other impact studies : reactive pollutants, particle
formation and dispersion, noise propagation …
Accidental releases,
Population comfort (wind and turbulence prediction),
The model: Mercure_Saturne
Developed by CEREA
3-D model adapted to atmospheric flow and dispersion
simulation
Core of the model: CFD model Code_Saturne (EDF) which
can handle complex geometry and complex physics
Unstructured grid, finite volumes Simulations:
•
• Full scale, fine resolution, complex terrainFull scale, fine resolution, complex terrain
•
• Large scale Large scale meteometeo. conditions taken into account. conditions taken into account
•
• kk--
ε
ε
turbulence closure modelturbulence closure model•
• neutral neutral gazgaz releases, point source, continuous releasesreleases, point source, continuous releases
•
Concentration time series (wind tunnel measurements) 0 200 400 600 800 1000 Tsite en seconde 0 200 400 600 800 1000 Ci -C BF en ppm 0 200 400 600 800 1000 Tsite en seconde 0 100 200 300 400 Ci -C BF en pp m Ci Concentration moyenne At 1000 m High fluctuations near the source
Focus : concentration
fluctuations
•
Two approaches
:
•
•
Hybrid
Hybrid
RANS / PDF
RANS / PDF
(
(
PhD Thesis
PhD Thesis
A.
A.
Radicchi
Radicchi
)
)
•
•
Pure RANS
Pure RANS
(
Hybrid approach
RANS/PDF
RANS (k-ε) PDF (SLM¹) ui , P k ,f
(PDF Eulérienne de la concentration)[ RANS / PDF ]
a Résolution des EDS pour la trajectoire d'un
échantillon de particules de fluide,
dx
p,iu
p,idt
du
p,i1
P
x
idt
u
p,iu
iT
Ldt
C
0dW
i ui , P , xp,i,up,i Wi, TLChamps moyens (RANS) Champs instantanés (EDS) Proccessus de Wiener,
Temp characterisitique de la turbulence
[ RANS / PDF ]
b Résolution de l'equation pour le melange de la
concentration transportée par chaque particule de fluide,
d
p p mdt S
dt
p m Conc. moyenneConc. instantanée particule p Temp de mélange
Pure RANS approach :
Concentration mean: j j j i j j x c u x C D x x C U t C ∂ ∂ − ∂ ∂ ∂ ∂ = ∂ ∂ + ∂ ∂ ( ' ') ) ( ) ( ρ ρ ) ( ' ' j t t j x C Sc c u ∂ ∂ = − ρ µ µt t Sc turbulent viscosity ε ρ µt = Cµ k2 Schmidt number Concentration variance: j j j j j j j i j j x c x c D x C c u x c u x c D x x c U t c ∂ ∂ ∂ ∂ − ∂ ∂ − ∂ ∂ − ∂ ∂ ∂ ∂ = ∂ ∂ + ∂ ∂ ' ' 2 ' ' 2 ) ' ' ( ) ' ( ) ' ' ( 2 2 2 2 ρ ρ ρ ) ' ( ' ' 2 2 j t t j x c Sc c u ∂ ∂ = − ρ µ k c R x c x c D f c j j ε ρ ε ρ '2 ' ' 2 = = ∂ ∂ ∂ ∂The Mock Urban Setting Test
(MUST)
Biltoft (2001).
Yee and Biltoft (2004).
Near full scale experiment
in the U.S. Army Dugway Proving Ground (Utah), conducted for the DTRA (Defense Threat
Simulations with
Mercure
~4 m ~2 m 0.6 to 1m ~0.3 m ~4 m Mesh: ~800 000 hexahedral elements Dimensions: 240 m x 233 m x 32mHorizontal grid : lower levels Stretched vertical grid
MUST: 20 selected cases
Detailed study of dynamics and mean concentration with
Simulations with
Mercure
Root mean square of concentration fluctuations (ppm)
Simulations with
Mercure
Simulations with
Mercure
20 simulated cases:
•
• MG = exp (|MG = exp (|lnln Co| Co| –– ||lnln Cp|)Cp|)
•
• VG = exp [|(VG = exp [|(lnln CoCo--lnln Cp) Cp) 22 |]|]
•
• FAC2 = fraction of data that FAC2 = fraction of data that satisfy 0.5<Cp/Co<2
satisfy 0.5<Cp/Co<2
Co = MUST observations Co = MUST observations Cp =
Cp = MercureMercure predictions predictions |x| = average over the data set |x| = average over the data set
53.8 % 2.56 0.66 Masts A, B, C, D 50.3 % 2.70 0.51 Tower T 66.4 % 2.22 1.05 All horizontal 60.1 % 2.40 0.82 All 52.6 % 2.61 0.61 All vertical 67.0 % 1.368 1.156 Line4 69.2 % 1.341 0.980 Line3 67.2 % 1.437 1.028 Line2 63.5 % 3.31 0.94 Line1 FAC2 VG MG
Root mean square of concentration fluctuations
Simulations with
Mercure
Root mean square of concentration fluctuations (ppm)
10 simulated cases:
FAC2 (neutral) = 46.9 % FAC2 (stable) = 53.3 %
+ 6 %
Simulations with
Mercure
c’(source) = 1% C(source)
Root mean square of concentration fluctuations (ppm)
Cloud modeling : plume + fog
Impact of building and complex terrain on
dispersion
Chemistry of reactive plumes
Aerosols formation (local scale)
Wind energy
Radiative effects
operational ABL prediction (SIRTA)
Traffic and tunnel
Overview : other activities
}
Following presentationsCalcul code Mercure iso-concentration
eau liquide Panache Bugey
Fig. 2 Comparison of the in-situ spectra measured by the aircraft with the simulated ones. a) Horizontal slice at z=1320m above the ground for case B ( -- -- : iso-LWC and —— : iso-N: c). The symbol ∗ shows the maximum of LWC, and the circles o are part of the same arc whose center is ∗. b) shows the measured spectra (black) 660m far from the ∗ and the log-normal curves (blue) obtained from the LWC and Nc values given by the code at the position of the shaded circles (located 660m far from the ∗).
a)
Stage C. Samba
Évolution de la visibilité
( )0.88 0 7 . 144 ) 02 . 0 ln( l q avec VIS β ρ β = − =Nouveau paramètre d’étude : la visibilité
Te mps (heure ) A lti tu de ( m ) vis ibilite 1 2 3 4 5 6 7 8 9 0 20 40 60 80 100 120 140 160 180 200 220 10 20 30 40 50 60 70 80 90 Mesures CAILLOU MERCURE Variations spatio-temporelles de la visibilité
3 phases dans l’évolution du brouillard :
La formation, le développement vertical et la dissipation de la couche de brouillard
IV. Résultats
Spectre des gouttelettes à 2m
Diamètre moyen de l’ordre de 10 µm et 20 µm Nc de l’ordre de quelques centaines de gouttelettes par cm³
Distribution des gouttelettes de nuages (cm-3/µm) à 2m en fonction du diamètre des gouttelettes (µm)
Overview : other activities
Cloud modeling : plume + fog
Impact of building and complex terrain on
dispersion
Chemistry of reactive plumes
Aerosols formation (local scale)
Wind energy
Local ABL prediction (SIRTA)
Traffic and tunnel
Résultats pour la situation de vent de Sud (Mercure_Saturne 1.1.3)
Overview : other activities
Cloud modeling : plume + fog
Impact of building and complex terrain on
dispersion
Chemistry of reactive plumes
Aerosols formation (local scale)
Wind energy
Local ABL prediction (SIRTA)
Traffic and tunnel
Overview : other activities
Cloud modeling : plume + fog
Impact of building and complex terrain on
dispersion
Chemistry of reactive plumes
Aerosols formation (local scale)
Wind energy
Local ABL prediction (SIRTA)
Traffic and tunnel
Overview : other activities
Cloud modeling : plume + fog
Impact of building and complex terrain on
dispersion
Chemistry of reactive plumes
Aerosols formation (local scale)
Wind energy
Local ABL prediction (SIRTA)
Traffic and tunnel
Wind energy : turbulence in complex terrain
and mask effect for large parks (Thesis L. Laporte)