attack of the toxic mist – ian d. longley school of earth, atmospheric & environmental...
TRANSCRIPT
Attack of the Toxic Mist –
Ian D. Longley
School of Earth, Atmospheric & Environmental Sciences,University of Manchester
Why we study Urban Aerosol Dispersion
Urban air is cleaner than it was – isn’t it?
Urban smogs in the UK:December 1991
March 1996December 2001February 2003
Aftermath of the Clean Air Acts
0
100
200
300
400
500
600
1940 1950 1960 1970 1980 1990 2000 2010
traf
fic
(b
illio
n v
kt)
PM10
Mass concentration of particulate matter with an aerodynamic diameter < 10 m
>50% probability of penetrating into thorax
UK-wide Automated Urban and Rural Networks
Bury (M60) Piccadilly Gardens North-West
What PM10 levels do we experience?
weekly means 1999-2005 incl.
0
5
10
15
20
25
30
35
40
45
50
PM
10 /
g m
-3
EcclesPiccadillyShaw Heath
December 2001
0
50
100
150
200
01-Dec 06-Dec 11-Dec 16-Dec 21-Dec 26-Dec 31-Dec
PM
10 /
g
m-3
EcclesStockport
wind speed
0
2
4
6
8
10
12
14
16
01-Dec 06-Dec 11-Dec 16-Dec 21-Dec 26-Dec 31-Dec
U /
m s
-1
1999-2005 Means:
Piccadilly 27
Eccles 23
Stockport 22
PM10 episodes and health risk
• Rise of 10 gm-3 PM10 linked to ~0.5% rise in mortality
• Translates as ~8 000 deaths brought forward per year in UK urban population (COMEAP, 1998) – compared to 3 700 total deaths due to RTAs.
• PM10 also linked to increased morbidity
• No lower threshold!• Deaths from respiratory causes• Also cardiovascular causes• Deaths mostly of the ‘vulnerable’• Episode promotes an
exacerbation of pre-existing condition
• What is the cause?
Urban particle sources and sizes
Dp / m
0.001 0.01 0.1 1 10 100
dV/d
log(
Dp)
/ m
3 m
-3
0.01
0.1
1
10
100Vehicle emissions,
combustion
Long-range transport, secondary particles
Dust, wear products,
biological particles, minerals
Measured in Princess Street, Manchester
PM10
Urban Particle Size Distributions
Particle number concentrations dominated by ultrafines
Dp / m
0.001 0.01 0.1 1 10 100
dV/d
log(
Dp)
/ m
3 m
-3
0.01
0.1
1
10
100
Dp / m
0.001 0.01 0.1 1 10 100
dN/d
log(
Dp)
/ cm
-3
1e-1
1e+0
1e+1
1e+2
1e+3
1e+4
1e+5
1e+6
Above: mass size distribution from Manchester street canyon
Above: number size distribution from Manchester street canyon
Data: Longley et al., Atmos. Environ., 2003.
dM
/dlo
gD
a /
g m
-3
Aerodynamic Diameter (nm)
1.0
0.8
0.6
0.4
0.2
0.0
dM
/dlo
gD a
(µg
m-3
)
2 3 4 5 6 7 8 9100
2 3 4 5 6 7 8 91000
2 3
Aerodynamic Diameter (nm)
OrganicsSulphateNitrateAmmonium
Manchester winter
4
3
2
1
0
dM
/dlo
gD
a (µ
g m
-3)
2 3 4 5 6 7 8 9100
2 3 4 5 6 7 8 91000
2 3
Aerodynamic Diameter (nm)
SulphateNitrateOrganicsAmmonium
Manchester_Summer
3.0
2.5
2.0
1.5
1.0
0.5
0.0<20
0nm
Par
ticul
ate
Org
anic
s (µ
gm-3
)
14012010080604020NOx (ppb)
Urban particle speciated mass size distributions
UFP mostly organic compounds
Also:
•Black carbon
•Sulphuric acid
i.e. Traffic is the major source
Data: Allan et al., JGR 2002, Alfarra et al., Atmos. Environ., 2004
Ultrafine Particles in the body
•Ultrafines (UFP) efficiently deposit to alveolar walls
•Overload can cause chronic inflammation and irreversible damage to tissues and defences
•Inflammatory response triggers systemic reaction in cardiovascular system – increases in blood viscosity, formation and disruption of plaques, heart rate variability.
•Can lead to arrythmia, ischaemia and heart attack (immediately or in future)
Effects seen in ‘non-toxic’ particles –
is toxicity in size, surface area or composition???
UFP dispersion in urban areas
coagulation
condensation
Recirculation/sheltering
dilution
65000
70000
75000
80000
85000
90000
95000
100000
105000
110000
Ventilation of the urban canopy
0
10000
20000
30000
40000
50000
60000
00:00 06:00 12:00 18:00 00:00local time
FN /
cm
-2s-1
0
40
80
120
160
200
240
H /
W m
-2
particles
sensible heat
Regular emission cycles
Sheltering, recirculation, deposition, inversions
0
10000
20000
30000
40000
50000
60000
70000
00:00 06:00 12:00 18:00 00:00
N2
5 /
cm
-3
0
2000
4000
6000
8000
10000
12000
14000
N2 /
cm
-3
25 m
2 m
Mean diurnal fluxes at 90 m above Manchester
Diurnal mean concentrations at 2 and 25 m
NOTE: ventilation is suppressed during morning emission peak
Data: NERC CityFlux project, Longley et al., 2006
Long-term PM10 exposure and health risk
• For long-term exposure relative risk is doubled to ~1.0% (Dockery et al., 1993, Pope et al., 1995, Kunzli et al., 2001)
• Suggests long-term exposure (to mean or repeated episodes?) causes or increases vulnerability
• Episodes NOT followed by ‘harvesting’ for cardiovascular deaths – episodes create a newly vulnerable cohort
Consequences:
Need to consider complete history of personal exposure, especially UFP
Fixed PM10 monitors versus personal UFP exposure
PM10 monitors are supposed to be ‘representative’
UFP has high spatial gradients, fixed monitors expensive and unrepresentative(?)
Daily/Hourly PM10 data biases concept of episode to day/hour durations
Personal UFP exposure dominated by short (< 1 hour) very high ‘excursions’
Need to consider residential and workplace, but especially commuting exposures
commuting exposure, 23 Nov 05
0
50000
100000
150000
200000
250000
300000
350000
400000
8:38 8:45 8:52 9:00 9:07
N /
cm-3
Walk to stop At bus stop On bus
Street canyon UFP number size distribution in channelled flow
Dp / nm
1 10 100 1000dN
/dlo
g(D
p) /
cm-3
103
104
105
106
channelled
Street canyon UFP number size distribution in recirculating flow
Dp / nm
1 10 100 1000dN
/dlo
g(D
p) /
cm-3
103
104
105
106
channelledrecirculation
Recirculation caused by perpendicular approach flow (>40 deg from canyon axis)
Extra particles in ‘fresh exhaust’ size range
Data: Longley et al., Atmos. Environ., 2003, CityFlux: Longley et al., 20060
10000
20000
30000
40000
50000
60000
70000
00:00 06:00 12:00 18:00 00:00
N25
/ c
m-3
0
2000
4000
6000
8000
10000
12000
14000
N2
/ cm
-3
25 m
2 m
Parameterising street canyon turbulencei
2 = (AiU)2 + 22
Where i = u, v, w
Ai, 2 = f(z)
U / m s-1
0 1 2 3 4
w/U
0.0
0.5
1.0
1.5
2.0
3.5 m3.5 m
3.5m: w2 = (0.17 U)2 + ((0.62 T / 3600) + 0.01)
Longley et al. 2004, Atmos. Env. 38, 69-79
Longley et al. 2004, Atmos. Env. 38, 4589-4592
Au, v, w
0.0 0.1 0.2 0.3 0.4 0.5 0.6
z / m
0
2
4
6
8
10
12
14
16
18
20
Au
Av
Aw
Au, v, w
0.0 0.1 0.2 0.3 0.4 0.5
z / m
1
2
3
4
5
6
7
8
9
Au
Av
Aw
Explicit numerical modelling of dispersion hampered by sub-grid
scale processes
Thus, empirical modelling presents practical
alternative
Outstanding problems
• Rate of dispersal from street canyons – advection - turbulent diffusion – deposition
• Generalising dispersion into the neighbourhood
• Coagulation/condensation/nucleation/reactions – require timescales
• How indoor exposure is related to outdoor concentrations
• Rapid growth of megcities – a challenge for the 21st century
Thanks for your attention
Statistical variation in ultra-fine concentrations
N0.1/cm-3
1x103 10x103 100x103 1x106
n i/n
tota
l
0.00
0.05
0.10
0.15
0.20
channelledrecirculated
N0.1 / cm-3
1000 10000 100000
Cum
f
0.0
0.2
0.4
0.6
0.8
1.0channelledrecirculatedbackground
Spatial variation in urban PM10
PM10 heavily influenced by
•Resuspended dusts
•Long-range transport of secondary PM
… but does this represent the variation in exposure potential?
Emission/dispersion modelling leads to…
Edinburgh measurements (SASUA, 1999-2001)
SASUA diurnal particle number flux (May)
Below: sensible surface heat flux
0
5000
10000
15000
20000
25000
0:00 6:00 12:00 18:00 0:00Time
N (
cm-3
)
0
10000
20000
30000
40000
50000
60000
70000
80000
90000
100000
FN (
cm-2
s-1
)
ConcentrationFlux
-50
0
50
100
150
200
0:00 6:00 12:00 18:00 0:00
Time
H (
W m
-2)
Oct/NovMay
`
Dorsey et al., 2002, Atmos. Environ. 36, 791-800.
•Diurnal cycle in urban ventilation related to heat flux cycle
UFP dispersion in road corridors
Factors affecting dispersion
Ptrak data
Visualisation of road corridor concept