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Pollutant dispersion through an obstacle array: numerical modelling and experimental investigation Soulhac L., Rios I., Garbero V., Farges B., Salizzoni P., Scaccianoce L., Perkins R., F.-X. Cierco Work funded by CEA/DAM Ecole Centrale de Lyon Laboratoire de Mécanique des Fluides et d'Acoustique 11th Harmonisation Conference Cambridge 2007

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Page 1: Pollutant dispersion through an obstacle array: …€¦ · Pollutant dispersion through an obstacle array: numerical modelling and experimental investigation Soulhac L., Rios I.,

Pollutant dispersion through an obstacle array: numerical modelling

and experimental investigation Soulhac L., Rios I., Garbero V., Farges B., Salizzoni P., Scaccianoce L., Perkins R.,

F.-X. Cierco Work funded by CEA/DAM

Ecole Centrale de LyonLaboratoire de Mécanique des Fluides et d'Acoustique

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LMFA/ECL - 2007 Harmo 11 - Cambridge - 04/07/2007 2

1. Introduction

• Context of prevention from short accidental releases

– Accidental releases due to urban industrial facilities– Transport of toxic materials

• Need of model tools in order to– Simulate different scenarios in preparation and training

for an eventual release– Predict the dispersion for emergency response– Evaluate precisely the impact of a release in post-

accident analysis

Dispersion of hazardous material in urban area

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1. Introduction

Some orders of magnitude

Capacity of reaction

Population affected(density ~ 10 000 inhbts/km²)

Concentration values

Concerned area (U ~ 1m/s)

Time100 s ~ 1 min. 30 1000 s ~ 15 min. 10 000s ~ 3h

100 m

10 km

1 km

100 inhbts

1 million inhbts

10000inhbts

100 m 1 km 10 km100

inhbts10000 inhbts

1 millioninhbts

District scaleStreet scale Agglomeration scale

Instantaneous release

• High concentrations

• Few people• Low concentrations• Very large number

of people concerned• No time to react• Enough time for

emergency services to react

Focus ondistrict scale

• Still high concentrations

• Already many people concerned

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• Which processes/parameters control dispersion at district scale?

• How to model a district of thousands street segments?

• How to predict one or two days of dispersion in a few minutes on a PC?Find an alternative to CFD codes (Fluent, Mercure, …) Need to develop simplified models for operational applicationsSome approaches exist : MicroSwiftSpray, UDM, …We will develop an alternative approach for very fast emergency response

1. Introduction

Some modelling issues at district scale

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1. Introduction

2. Wind tunnel experiments on urban district

3. SIRANERISK dispersion model

4. Preliminary comparison SIRANERISK / measurements

5. Conclusions and perspectives

1. Introduction

Plan of the presentation

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Dimensions of the test section: 14m x 2.5 m x 3.7m

2. Wind tunnel experiments on urban district

Experimental setting

Atmospheric wind tunnel of the Ecole Centrale de Lyon

Study of turbulent dispersion from a continuous point source in an urban districtInfluence of wind direction

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2. Wind tunnel experiments on urban district

Experimental setting

y

x

z

x

Lx

Ly

Sx

Sy

H

Model :H = 50 mmLx = Ly = 5HSx = Sy = H

Establishment of the urban boundary layer

District studied

7 m

Model scale 1:400

Reality :H = 20 mLx = Ly = 100 mSx = Sy = 20 m

Building geometry

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Concentration measurements with Flame Ionisation Detector:

• Lateral profiles (y-direction) at different distance from the source• Variation of the wind direction

XX

x

y

2. Wind tunnel experiments on urban district

Experimental setting

15°

30°45°

• Continuous release

• Point source located in an intersection

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24 12 0

-12

-24

y/H

K

012

2436

48

x/H

04

80

24

01

20

0.5

1

2. Wind tunnel experiments on urban district

Experimental results Wind direction = 0°

• The plume is channelled by the main street

• Small transverse dispersion in perpendicular streets

RANS CFD calculationsWind tunnel concentration profiles (z = 0)

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K

012

2436

48x/

H

06

04

01

00.

35

36 24 12 0

-12

y/H

2. Wind tunnel experiments on urban district

Experimental resultsWind direction = 15°

• The plume spreads more rapidly than in the 0° case

• The plume centreline is shifted due to a channelling mechanism

Analogy with plume behaviour in this CFD simulation of the MUST experiment (Carissimo, 2001)

Wind directionPlume centreline

Wind tunnel concentration profiles (z = 0)

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K

0

12

24

36

48

x/H

0

60

10

0.250

0.15

36 24 12 0 -12y/H

2. Wind tunnel experiments on urban district

Experimental resultsWind direction = 30°

• The plume spreads even more rapidly

• The steps in the concentration profiles correspond to the presence of the streets

• The concentration is almost homogeneous in each street

Wind directionPlume centreline

Wind tunnel concentration profiles (z = 0)

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2. Wind tunnel experiments on urban district

Experimental results

K

012

2436

48x/

H

01

00.

30

0.2

48 36 24 12 0

y/H

Wind direction = 45°

• The plume centreline deflection disappears in the symmetric case

• The concentration is almost constant in each street but varies from one street to the other

Wind tunnel concentration profiles (z = 0)

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2. Wind tunnel experiments on urban district

Experimental results

K

012

2436

48x/

H

01

00.

30

0.2

48 36 24 12 0

y/H

Wind direction = 45°RANS CFD calculations

Importance of the exchange mechanism at the intersections

Wind tunnel concentration profiles (z = 0)

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2. Wind tunnel experiments on urban district

Experimental resultsWind direction = 45°

Two mechanisms control the dispersion in a district :

1. Exchanges at each intersection

2. Exchange with the external flow and dispersion over the roof level

RANS CFD calculations(roof level z = H)

Importance of the transport over the roof level

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• SIRANERISK is an evolution of the SIRANE model, used for air quality modelling in urban area (application on Lyon, Paris, Grenoble, Torino, Milano, …)

• SIRANE is a steady state model SIRANERISK is an unsteady model

3. SIRANERISK dispersion model

Introduction

SIRANE model – Agglomeration of Lyon – 2003Example of hourly NOX concentrations

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Urban geometry is complex at different scalesneed to simplify in an operational model

Scale of the reliefScale of the detail on buildings

Scale of buildings

3. SIRANERISK dispersion model

Geometrical description of a district

Taken into account by aRoughness length

Taken into account by auser-provided external wind field

coupled with a puff model

Resolved explicitly bya street network approach

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Representation of urban canopy

Simplification of building geometry

3. SIRANERISK dispersion model

Geometrical description of a district

Pollutant budget in each street Exchange at intersections

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• Turbulent exchange at the interface

• Budget of pollutant mass in the street

QI,out

QI,in

QH,turb

Qpart,ground

QS

Qpart,HQwet depos.( )wH,turb street street,ext

WLQ C C2

σ= −

π

Emission of a new rectangular puff over the street

( )S I,in part,H H,turb I,out part,ground wet depos.

In fluxes Out fluxes

streetd HWL.Cdt

Q Q Q Q Q Q Q= + + − + + +144424443 14444444244444443

3. SIRANERISK dispersion model

Concentration model in each street• Analytical model for the average velocity in each street

(Soulhac et al., 2007, submitted to Boundary Layer Meteorology)

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Calculation of exchange fluxes as a function of wind direction :

Pi,j (θ)

3. SIRANERISK dispersion model

Exchange model for an intersection15° 45°30°

RANS CFDcalculations

Averaging fluxes over wind direction fluctuations :

( ) ( ) ( )

( )

i,j 0 0 i,j

2

00

P f P d

1 1with f exp22 θθ

θ = θ − θ θ θ

⎡ ⎤⎛ ⎞θ − θ⎢ ⎥θ − θ = − ⎜ ⎟σσ π ⎢ ⎥⎝ ⎠⎣ ⎦

∫11th Harmonisation Conference

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3. SIRANERISK dispersion model

Puff dispersion model over the roof level

Each vertical flux of pollutant is modelled by a source of puffs

• Each puff is advected by the wind field

• Each puff spreads to model turbulent dispersion11th Harmonisation Conference

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4. Preliminary comparison SIRANERISK / measur.

Wind direction = 30°

Ground level Roof level

• The model seams to represent the main features of the concentration field• Need to parameterize the different exchange coefficients to compare more precisely

Concentration profilesWind tunnel

– SIRANERISK

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4. Preliminary comparison SIRANERISK / measur.

Wind direction = 15°

Ground level Roof level

Concentration profilesWind tunnel

– SIRANERISK

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4. Preliminary comparison SIRANERISK / measur.

Wind direction = 0°

Ground level Roof level

• Difficulty to describe the lateral diffusion in this case Pietro Salizzoni's presentation

Concentration profilesWind tunnel

– SIRANERISK

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5. Conclusions and perspectives

• Wind tunnel experimental studyIdentification of main dispersion mechanisms

• Development of an unsteady puff-canopy dispersion model, SIRANERISK, for operational purposes

Need to validate SIRANERISK model

• A preliminary comparison between model and experiments shows that SIRANERISK describes the main characteristics of the plume

• PerspectivesNeed to parameterize the different exchange coefficientsValidation on unsteady dispersion cases

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