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ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
1
MODELLING OF ATMOSPHERIC FLOW AND DISPERSION IN THE WAKE OF A
CYLINDRICAL OBSTACLE
S. Andronopoulos1, I. Mavroidis2, A. Venetsanos1, J.G. Bartzis3
1Environmental Research Laboratory, Institute of Nuclear Technology and Radiation Protection, National Centre for Scientific Research “Demokritos”, 15310 Aghia Paraskevi Attikis, Greece, e-mail:
[email protected] Open University, Patras, Greece
3Department of Energy Resources Management Engineering, University of Western Macedonia, Greece
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
2
Aim of the paper
• Computational study of the interaction of continuous plumes released from point sources with buildings– short-range dispersion of atmospheric pollutants in built-up
areas– Simple, isolated structures: main characteristics of flow and
dispersion• Present case: Cylindrical obstacle (“building”)
– Previously studied case: “Atmospheric dispersion in the presence of a three-dimensional cubical obstacle: Modelling of mean concentration and concentration fluctuations”, by Mavroidis, Andronopoulos, Bartzis, Griffiths, Atmospheric Environment 41 (2007), 2740-2756
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
3
Tools, data, methods
• CFD code ADREA-HF– Mean concentrations, concentration fluctuations
• Data from field experiments– “Field and wind tunnel investigations of plume dispersion
around single surface obstacles”, by Mavroidis, Griffiths, Hall, Atmospheric Environment 37 (2003) 2903-2918
• Comparisons of calculated with experimental results / model performance
• Study of computed dispersion patterns• Comparisons between cylindrical and cubical obstacles
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
4
Experimental set up: cylinder
• Dual source:- Ammonia- Propane
• Ammonia source displaced laterally
• Height and diameter of cylinder H=1.15m
• Source and detector height: H/2
• Atmospheric stability: D (neutral)
• Wind speed: 2.6 – 4.5 m/s
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
5
Experimental set up: cube
• Dual source:- Ammonia- Propane
• Ammonia source displaced laterally
• Height and diameter of cylinder H=1.15m
• Source and detector height: H/2
• Atmospheric stability: D (neutral)
• Wind speed: 4.7 – 6.3 m/s
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
6
Experimental results: ammonia concentrations
Sensor at ٠.٥H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
(non
-dim
.)
CubeCylinder
Sensor at ٢H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
(non
-dim
.)
CubeCylinder
Sensor at ٣H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
(non
-dim
.)
CubeCylinder
Sensor at ٥H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
(non
-dim
.)
CubeCylinder
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
7
Experimental results: ammonia concentration fluctuations
Sensor at ٠.٥H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
fluct
uatio
n (c
'/C)
CubeCylinder
Sensor at ٢H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
fluct
uatio
n (c
'/C)
CubeCylinder
Sesnor at ٣H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
fluct
uatio
n (c
'/C)
CubeCylinder
Sensor at ٥H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
fluct
uatio
n (c
'/C)
CubeCylinder
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
8
Experimental results: ammonia concentration intermittency
Sensor at ٠.٥H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
inte
rmitt
ency
CubeCylinder
Sensor at ٢H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
inte
rmitt
ency
CubeCylinder
Sesnor at ٣H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
inte
rmitt
ency
CubeCylinder
Sensor at ٥H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xH
Source displacement
Am
mon
ia c
once
ntra
tion
inte
rmitt
ency
CubeCylinder
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
9
Computational results: non-dimensional mean concentration
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
C non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠١
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
C non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٢
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
C non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٥
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
C non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N١١
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
C non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٧
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
10
Computational results: non-dimensional concentration StD
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
StD non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠١
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
StD non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٢
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
StD non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٥
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
StD non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N١١
X (H)
Y(H
)
-٥ ٠ ٥ ١٠
-٦
-٤
-٢
٠
٢
٤
٦
StD non-dim١٠١٠.٧٠.٥٠.٣٠.١٠.٠١
N٠٧
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
11
Model evaluation: turbulence closure schemes – k-l (1), k-ε, k-l (2)
Non-dimensional ammonia concentration
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
٠ ٠.١ ٠.٢ ٠.٣ ٠.٤ ٠.٥ ٠.٦ ٠.٧ ٠.٨ ٠.٩
Experimental
Cal
cula
ted N٠١
N٠٢N٠٥N١١N٠٧
Non-dimensional ammonia concentration
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠ ٠.١ ٠.٢ ٠.٣ ٠.٤ ٠.٥ ٠.٦ ٠.٧
Experimental
Cal
cula
ted N٠١
N٠٢N٠٥N١١N٠٧
Non-dimensional ammonia concentration
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠.٣٠
٠.٣٥
٠.٤٠
٠.٠٠ ٠.٠٥ ٠.١٠ ٠.١٥ ٠.٢٠ ٠.٢٥ ٠.٣٠ ٠.٣٥ ٠.٤٠
Experimental
Cal
cula
ted
N٠١N٠٢N٠٥N١١N٠٧
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
12
Model evaluation : turbulence closure schemes – k-l (1), k-ε, k-l (2)
Non-dimensional ammonia concentration StD
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
٠ ٠.١ ٠.٢ ٠.٣ ٠.٤ ٠.٥ ٠.٦ ٠.٧ ٠.٨ ٠.٩
Experimental
Cal
cula
ted N٠١
N٠٢N٠٥N١١N٠٧
Non-dimensional ammonia concentration StD
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠ ٠.١ ٠.٢ ٠.٣ ٠.٤ ٠.٥ ٠.٦ ٠.٧
Experimental
Cal
cula
ted N٠١
N٠٢N٠٥N١١N٠٧
Non-dimensional ammonia concentration StD
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٠ ٠.١ ٠.٢ ٠.٣ ٠.٤ ٠.٥ ٠.٦ ٠.٧
Experimental
Cal
cula
ted
N٠١N٠٢N٠٥N١١N٠٧
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
13
Model evaluation : turbulence closure schemes – k-l (1), k-l (2), k-ε
Ammonia concentration fluctuation
٠
١
٢
٣
٤
٥
٦
٧
٨
٩
٠ ١ ٢ ٣ ٤ ٥ ٦ ٧ ٨ ٩
Experimental
Cal
cula
ted
N٠١N٠٢N٠٥N١١N٠٧
Ammonia concentration fluctuation
٠
١
٢
٣
٤
٥
٦
٧
٨
٩
٠ ١ ٢ ٣ ٤ ٥ ٦ ٧ ٨ ٩
Experimental
Cal
cula
ted
N٠١N٠٢N٠٥N١١N٠٧
Ammonia concentration fluctuations
٠
١
٢
٣
٤
٥
٦
٠ ١ ٢ ٣ ٤ ٥ ٦
Experimental
Cal
cula
ted
N٠١N٠٢N٠٥N١١N٠٧
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
14
Model evaluation : turbulence closure schemes – k-l (1), k-l (2), k-ε
٠.٥H ٣.٠H ٠.٥H ٣.٠H ٠.٥H ٣.٠H ٠.٥H ٣.٠HN٠١ ٠.٤٢٣ ٠.٢٣٨ ٠.٧٨٨ ٠.٤٤٥ ٠.٦٢٩ ٠.٤٤٢ ٠.٢٦٢ ٠.١٤٧N٠٢ ٠.٣١٩ ٠.١٧١ ٠.٨٠٦ ٠.٤٦٣ ٠.٦٦٤ ٠.٤٨١ ٠.٢٩٥ ٠.١٦٨N٠٥ ٠.٢٨٨ ٠.١٧٥ ٠.٧٩٠ ٠.٤٥١ ٠.٦٤٢ ٠.٤٥٩ ٠.٢٨٠ ٠.١٥٨N١١ ٠.٣٣٨ ٠.٢٣٨ ٠.٨٠٥ ٠.٤٦١ ٠.٦٦١ ٠.٤٧٨ ٠.٢٨٨ ٠.١٦٤N٠٧ ٠.٢٠٤ ٠.١٢٢ ٠.٧٨٧ ٠.٤٤٩ ٠.٦٣٦ ٠.٤٥٣ ٠.٢٧٦ ٠.١٥٦
Average ٠.٣١٤ ٠.١٨٩ ٠.٧٩٥ ٠.٤٥٤ ٠.٦٤٦ ٠.٤٦٢ ٠.٢٨٠ ٠.١٥٨Calc/Exper ٢.٥٣ ٢.٤٠ ٢.٠٦ ٢.٤٥ ٠.٨٩ ٠.٨٤
Experimental Calculated k-εCalculated k-l (١) Calculated k-l (٢)
٠.٥H ٣.٠H ٠.٥H ٣.٠H ٠.٥H ٣.٠H ٠.٥H ٣.٠HN٠١ ٠.٥٣٧ ٠.٢٧٨ ١.٠٤٤ ٠.٨٢٠ ١.٠١٧ ٠.٩٣٥ ٠.٧٦٥ ٠.٤٢٥N٠٢ ٠.٤٧٨ ٠.٢٣٥ ١.٢١٥ ٠.٩٥٩ ٠.٩٧٢ ٠.٩٧٧ ٠.٩٠٨ ٠.٥١٢N٠٥ ٠.٤١٦ ٠.٢٣٦ ١.١٤١ ٠.٨٩٧ ٠.٩٨٧ ٠.٩٦٦ ٠.٨٤٥ ٠.٤٧٥N١١ ٠.٣٧٢ ٠.٢٧١ ١.٢١٠ ٠.٩٥٥ ٠.٩٧٩ ٠.٩٨٣ ٠.٨٩٩ ٠.٥١٠N٠٧ ٠.٣٣٩ ٠.١٩٩ ١.١٢٢ ٠.٨٨١ ٠.٩٩٣ ٠.٩٦١ ٠.٨٢٩ ٠.٤٦٥
Average ٠.٤٢٩ ٠.٢٤٤ ١.١٤٦ ٠.٩٠٢ ٠.٩٨٩ ٠.٩٦٤ ٠.٨٤٩ ٠.٤٧٨Calc/Exper ٢.٦٧ ٣.٧٠ ٢.٣١ ٣.٩٦ ١.٩٨ ١.٩٦
Experimental Calculated k-l (١) Calculated k-ε Calculated k-l (٢)
Propane Concentration
Propane Concentration
StD
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
15
Model evaluation: comparison between cube and cylinder cases
Experimental Calculated, k-l ( )١ Ratio Calculated, k-ε Ratio٠.٥H ٠.٧٣٩ ٠.٨١٦ ١.١٠٣ ٠.٨٠٩ ١.٠٩٤٣.٠H ٠.٢٤٦ ٠.٤٣٨ ١.٧٧٧ ٠.٤٩١ ١.٩٩٣
Experimental Calculated, k-l ( )١ Ratio Calculated, k-ε Ratio٠.٥H ٠.٣١٤ ٠.٧٩٥ ٢.٥٢٩ ٠.٦٤٦ ٢.٠٥٦٣.٠H ٠.١٨٩ ٠.٤٥٤ ٢.٤٠٢ ٠.٤٦٢ ٢.٤٤٨
Experimental Calculated, k-l ( )١ Ratio Calculated, k-ε Ratio٠.٥H ٠.٥٠٩ ٠.٤٨٩ ٠.٩٦٠ ٠.٣٦٧ ٠.٧٢١٣.٠H ٠.٣٢٢ ٠.٤٠٥ ١.٢٥٦ ٠.٣٥٠ ١.٠٨٥
Experimental Calculated, k-l ( )١ Ratio Calculated, k-ε Ratio٠.٥H ٠.٤٢٩ ١.١٤٦ ٢.٦٧٥ ٠.٩٨٩ ٢.٣٠٨٣.٠H ٠.٢٤٤ ٠.٩٠٢ ٣.٧٠٣ ٠.٩٦٤ ٣.٩٥٧
Average propane concentrations for CUBE
Average propane concentrations for CYLINDER
Average propane concentration StD for CUBE
Average propane concentration StD for CYLINDER
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
16
Model evaluation: comparison between cube and cylinder cases
Cube, sensor at ٠.٥ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.)
MeasuredCalc., k-lCalc., k-ε
Cube, sensor at ٢ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.)
MeasuredCalc., k-lCalc., k-ε
Cylinder, sensor at ٠.٥ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.) Measured
Calc., k-l(١)Calc., k-εCalc., k-l(٢)
Cylinder, sensor at ٢ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.) Measured
Calc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
17
Model evaluation: comparison between cube and cylinder cases
Cube, sensor at ٣ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.)
MeasuredCalc., k-lCalc., k-ε
Cylinder, sensor at ٣ H downwind
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.) Measured
Calc., k-l(١)Calc., k-εCalc., k-l(٢)
Cube, sensor at ٥ H downwind
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠.٣٠
٠.٣٥
٠.٤٠
٠.٤٥
٠.٥٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.)
MeasuredCalc., k-lCalc., k-ε
Cylinder, sensor at ٥ H downwind
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠.٣٠
٠.٣٥
٠.٤٠
٠.٤٥
٠.٥٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n (n
on-d
im.) Measured
Calc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
18
Model evaluation: comparison between cube and cylinder cases
Cube, sensor at ٠.٥ H downwind
٠.٠
٢.٠
٤.٠
٦.٠
٨.٠
١٠.٠
١٢.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-ε
Cylinder, sensor at ٠.٥ H downwind
٠.٠
٢.٠
٤.٠
٦.٠
٨.٠
١٠.٠
١٢.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-εCalc., k-l(٢)
Cube, sensor at ٢ H downwind
٠.٠
٢.٠
٤.٠
٦.٠
٨.٠
١٠.٠
١٢.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-ε
Cylinder, sensor at ٢ H downwind
٠.٠
٢.٠
٤.٠
٦.٠
٨.٠
١٠.٠
١٢.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
19
Model evaluation: comparison between cube and cylinder cases
Cube, sensor at ٣ H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٨.٠
٩.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-ε
Cylinder, sensor at ٣ H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٧.٠
٨.٠
٩.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-εCalc., k-l(٢)
Cube, sensor at ٥ H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-ε
Cylinder, sensor at ٥ H downwind
٠.٠
١.٠
٢.٠
٣.٠
٤.٠
٥.٠
٦.٠
٠xH ٠.٥xH ٠.٧٥xH ١.٠xH ١.٢٥xH ١.٥xH ١.٧٥xH ٢.٠xHLateral Source displacement
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
MeasuredCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
20
Model evaluation: comparison between cube and cylinder cases
E٠٣, YS = ٠ H
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-lCalc., k-ε
N٠١, YS = ٠ H
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
E٠٤, YS = ٠.٥ H
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind dstance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-lCalc., k-ε
N٠٢, Ys=٠.٥ H
٠.٠
٠.١
٠.٢
٠.٣
٠.٤
٠.٥
٠.٦
٠.٧
٠.٨
٠.٩
١.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
21
Model evaluation: comparison between cube and cylinder cases
E١٠, YS = ١ H
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠.٣٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (Η)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-lCalc., k-ε
N٠٥, Ys = ١ H
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠.٣٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im) Experimental
Calc., k-l(١)Calc., k-εCalc., k-l(٢)
E٠٦, YS = ١.٥ H
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-lCalc., k-ε
N١١, Ys = ١.٥ H
٠.٠٠
٠.٠٥
٠.١٠
٠.١٥
٠.٢٠
٠.٢٥
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
22
Model evaluation: comparison between cube and cylinder cases
E٠٧, YS = ٢ H
٠.٠٠
٠.٠٢
٠.٠٤
٠.٠٦
٠.٠٨
٠.١٠
٠.١٢
٠.١٤
٠.١٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-lCalc., k-ε
N٠٧, YS = ٢ H
٠.٠٠
٠.٠٢
٠.٠٤
٠.٠٦
٠.٠٨
٠.١٠
٠.١٢
٠.١٤
٠.١٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n (n
on-d
im)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
23
Model evaluation: comparison between cube and cylinder cases
E٠٣, YS = ٠ H
٠
٠.٢
٠.٤
٠.٦
٠.٨
١
١.٢
١.٤
١.٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
ExperimentalCalc., k-lCalc., k-ε
N٠١, YS = ٠ H
٠.٠
٠.٢
٠.٤
٠.٦
٠.٨
١.٠
١.٢
١.٤
١.٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
E٠٤, YS = ٠.٥ H
٠.٠
٠.٢
٠.٤
٠.٦
٠.٨
١.٠
١.٢
١.٤
١.٦
١.٨
٢.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n Fl
uctu
atio
ns (c
'/C)
ExperimentalCalc., k-lCalc., k-ε
N٠٢, Ys = ٠.٥ H
٠.٠
٠.٢
٠.٤
٠.٦
٠.٨
١.٠
١.٢
١.٤
١.٦
١.٨
٢.٠
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
) ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
24
Model evaluation: comparison between cube and cylinder cases
E١٠, YS = ١ H
٠
١
٢
٣
٤
٥
٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n Fl
uctu
atio
n (c
'/C)
ExperimentalCalc., k-lCalc., k-ε
N٠٥, Ys = ١ H
٠
١
٢
٣
٤
٥
٦
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
E٠٦, YS = ١.٥ H
٠
١
٢
٣
٤
٥
٦
٧
٨
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n Fl
uctu
atio
n (c
'/C)
ExperimentalCalc., k-lCalc., k-ε
N١١, Ys = ١.٥ H
٠
١
٢
٣
٤
٥
٦
٧
٨
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
)ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
25
Model evaluation: comparison between cube and cylinder cases
E٠٧, YS = ٢ H
٠
٢
٤
٦
٨
١٠
١٢
١٤
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n Fl
uctu
atio
n (c
'/C)
ExperimentalCalc., k-lCalc., k-ε
N٠٧, YS = ٢ H
٠
٢
٤
٦
٨
١٠
١٢
١٤
٠ ٢ ٤ ٦ ٨ ١٠ ١٢Downwind distance from obstacle (H)
Con
cent
ratio
n flu
ctua
tion
(c'/C
)
ExperimentalCalc., k-l(١)Calc., k-εCalc., k-l(٢)
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
26
Summary and conclusions (1)
• Computational simulations of atmospheric dispersion experiments around isolated obstacles in the field
• CFD code ADREA-HF: dispersion of positively or negatively buoyant gases in complicated geometries
• Single cylindrical obstacle normal to the mean wind direction and two upwind sources of ammonia and propane, with the ammonia source located at different lateral positions
• Concentrations and concentration fluctuations for both gases were calculated by the model and compared with the experimental results
• Comparisons of experimental and model results with the case of dispersion around an isolated cubical obstacle are also presented and discussed
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
27
Summary and conclusions (2)
• Analysis of experimental results:– Variation of ammonia concentrations, concentration
fluctuations and intermittency as the source is displaced laterally
• Source at 0. H and 0.5 H: higher concentrations for cube• Sharper decrease of concentration with source displacement• Concentration peaks for source at 0.5 H (2, 3 and 5 H downwind)• Cylinder: fluctuations increase, cube: fluctuations peak for
source at 1.5 H off• Intermittency increases with source displacement, more sharply
for cube• Computational results: k-l (2 versions for cylinder)
and k-ε turbulence closure schemes tested
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
28
Summary and conclusions (3)
• Model performance evaluation:– “Scatter” plots for cylinder case
• Ammonia concentrations– k-l(1) and k-ε similar performance, around factor-of-2– k-l(1) more points inside the factor-of-2 range, large
overestimation for cases with large source displacement• Ammonia concentration StD
– Most points inside the factor-of-2 range for all models• Ammonia concentration fluctuations
– Most points inside the factor-of-2 range for all models– k-l(2) model results show little variation
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
29
Summary and conclusions (4)
• Model performance evaluation:– Propane results statistics:
• “Ensemble” averages (same source position, stability conditions, similar wind)
• The model performance for the cube case was better than for the cylinder case
• The ratio Calc. / Exper. for concentrations is 2 times higher and for concentration StD is 3 times higher in the cylinder case
– Ammonia concentration variation as the source is displaced laterally
• k-l(1) and k-ε model results are similar and in general overestimate. Some peaks are predicted, only for the cube
• k-l(2) model results are better for small source displacements but show little variation
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
30
Summary and conclusions (5)
• Model performance evaluation:– Ammonia concentration fluctuation variation as the source is
displaced laterally• Models do not predict the experimental peak for the cube for
source displaced 1.5 H off the centreline• k-l(2) model results show very little variation
– Ammonia concentration profiles downwind• Experimental values are higher for the cube than for the
cylinder close to the obstacle and decrease more sharply• k-l(1) and k-ε results are similar and overestimate the
experimental values for source placed at 0, 0.5, 1 and 1.5 H off the centreline
• k-l(2) agree better for source placed at 0, 0.5, 1 H but are worse for source placed at 1.5 and 2 H off the centreline
ERELEREL 12th Int. Conf. on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes, 6 – 9/10/2008, Cavtat, Croatia
31
Summary and conclusions (6)
• Model performance evaluation:– Ammonia concentration fluctuations profiles downwind
• Model results peaks are “weaker” than the experimental and occur closer to the obstacle
• For the cylinder case no peak is observed in the experimental data for source displacement above 1 H off centreline
• k-l(2) model results are better for smaller source displacements, k-l(1) and k-ε are better for larger source displacements.
• Future work:– More detailed analysis of the differences in results and
model performance between cubical and cylindrical obstacle cases