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(1)

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,

(2)

Outline

Objectives

Focus : concentration fluctuations

Overview : other activities

(3)

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),

(4)

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

(5)

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

(6)

Focus : concentration

fluctuations

Two approaches

:

Hybrid

Hybrid

RANS / PDF

RANS / PDF

(

(

PhD Thesis

PhD Thesis

A.

A.

Radicchi

Radicchi

)

)

Pure RANS

Pure RANS

(

(7)

Hybrid approach

RANS/PDF

RANS (k-ε) PDF (SLM¹) ui , P k ,

f

(PDF Eulérienne de la concentration)
(8)

[ RANS / PDF ]

a

„ Résolution des EDS pour la trajectoire d'un

échantillon de particules de fluide,

dx

p,i

u

p,i

dt

du

p,i

1

P

x

i

dt

u

p,i

u

i

T

L

dt

C

0

dW

i ui , P , xp,i,up,i Wi, TL

Champs moyens (RANS) Champs instantanés (EDS) Proccessus de Wiener,

Temp characterisitique de la turbulence

(9)

[ RANS / PDF ]

b

„ Résolution de l'equation pour le melange de la

concentration transportée par chaque particule de fluide,

d

p p m

dt S

dt

p m Conc. moyenne

Conc. instantanée particule p Temp de mélange

(10)
(11)

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 = = ∂ ∂ ∂ ∂
(12)

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

(13)

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 32m

Horizontal grid : lower levels Stretched vertical grid

„ MUST: 20 selected cases

„ Detailed study of dynamics and mean concentration with

(14)

Simulations with

Mercure

Root mean square of concentration fluctuations (ppm)

(15)

Simulations with

Mercure

(16)

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

(17)

Simulations with

Mercure

Root mean square of concentration fluctuations (ppm)

„ 10 simulated cases:

FAC2 (neutral) = 46.9 % FAC2 (stable) = 53.3 %

+ 6 %

(18)

Simulations with

Mercure

c’(source) = 1% C(source)

Root mean square of concentration fluctuations (ppm)

(19)

„

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 presentations
(20)

Calcul code Mercure iso-concentration

eau liquide Panache Bugey

(21)

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)

(22)

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

(23)

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)

(24)

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

(25)
(26)

Résultats pour la situation de vent de Sud (Mercure_Saturne 1.1.3)

(27)
(28)

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

(29)
(30)
(31)

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

(32)
(33)

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

(34)

Wind energy : turbulence in complex terrain

and mask effect for large parks (Thesis L. Laporte)

Figure

Fig. 2 Comparison of the in-situ spectra measured by the aircraft with the simulated ones

References

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