METO 637 LESSON 18. Schematic of ozone production from VOC.
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Transcript of METO 637 LESSON 18. Schematic of ozone production from VOC.
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METO 637
LESSON 18
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Schematic of ozone production from VOC
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SMOG
• NEEDS• Hydrocarbons and nitrogen oxides• Strong sunlight to start reactions• Warm temperatures to maintain reactions – the higher
the temperature the faster the rate.• Peak ozone will be close to peak temperature –
afternoon
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Standards
• Ozone: 1-hour 125 ppbv*, 8-hour 85 ppbv– The 8-hour standard is much more stringent, and
encompasses many areas where transport is the only issue (e.g Shenandoah National Park)
• PM2.5: daily 65 g/m3, yearly 15 g/m3
– Most areas will have trouble only with the annual standard
• Visibility: a 60+ year glide path back to “natural conditions”
*parts per billion by volume
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Ozone isopleths (NMHC vs NOx)
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Ozone vs NOx for NHMC=0.6 ppmc
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Daily Ozone Cycle
Sunrise Sunset
Time of day
Ozone Concentration
Ozone productionfollows a dailycycle with maximumconcentrations typically observedin the late afternoon.
This cycle is a signature of the dynamic processes of atmospheric air pollution
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Comparison of ozone data at Fort Meade for August 2 and 8 2002
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Overplot of 2 and 8 Aug 2002 and the difference between the two days
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Difference 2 Aug minus 8 Aug*1.2
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Back Trajectories, Hysplit
AUG 2, 2002 AUG 8, 2002
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Comparison of Aug 2 and 8, 2002
• Ozone data for August 8 is typical for local pollution on a clear warm day.
• The NOx and VOC are emitted early in the morning and the ozone amount slowly increases as the temperature increases. The peak production is at about 3-4 in the afternoon when the temperature at the ground is a maximum.
• The back trajectory shows fast upper level winds, which start at a high altitude and then subside to boundary levels at Baltimore.
• Small probability of upper air being polluted.
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Comparison of Aug 2 and 8, 2002• On the 2nd of August the back trajectories show that the
air is moving slowly at the boundary layer, and the probability of this air being polluted is high.
• The nocturnal inversion typically breaks down at about 10-11 in the morning.
• Hence the peak in ozone at this time must come from downward transport.
• The overall shape of the ozone data on Aug 2 is a combination of locally produced ozone peaking at about 3 pm and a downward movement of ozone from above at about 10.00 am.
• This ozone above the boundary layer is yesterday’s ozone
• The winds above the boundary layer are usually high. Hence the ozone has been transported some distance
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Natural levels of Acidity in Rain• Carbon dioxide dissolves in the rain drop
CO2(g) + H2O(aq) ↔ H2CO3(aq)
• Henry’s Law states that
[H2CO3] = KHP(CO2)
• KH = 3.4E-2 M ATM-1
• In the liquid some of the H2CO3 ionizes
H2CO3(aq) ↔ H+(aq) + HCO3-(aq)
• This reaction has an equilibrium constant of 4.2E-7 M-3
• For the overall reaction
CO2(g) + H2O(aq) ↔ H+(aq) + HCO3(aq)
The equilibrium constant Kc is 1.43E-8 M2.ATM-1
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Natural levels of Acidity in Rain
)(
]][[ where
2
3
COP
HCOHKc
• in a liquid [H+] = [HCO3-] hence
[H+]2 = KcP[CO2]
given that CO2 has a mixing ratio of 320 ppm we get
[H+] = 2.14E-6 and a pH of 5.67
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Dispersion of acid rain
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pH of precipitation over the US
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Acid rain
• Acid rain over the Eastern States is the highest – most of the sulfur containing coal occurs in this region
• Shaded areas in the figure show where granite is found.
• If the soil/rocks are carbonates (chalk, limestone) then the acid rain can be neutralized, and does not change the pH of the streams and lakes
• If the soil/rocks are granite then acid rain is not neutralized, and can also leach out the heavy metals. Thus the pH of the lakes and streams can be lowered, and the heavy metal concentration raised.
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Sources of pollutants in the USA
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Sulfur Dioxide emissions
67%
17%
4%
3%2%
7%
Fuel Combustion- Electric Utility
Fuel Combustion- Industrial
Fuel Combustion- Other
MetalsProcessing
Non-RoadVehicles
All Other
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Annual mean haze, United States
IMPROVE network
Flight area
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Detection Techniques
• In situ via UV pulsed fluorescence.– Modified commercial instrument– Detection limit ~70 ppt ()– Response time ~3 min
• Satellite via UV (315 to 327 nm ) spectroscopy
(modified DOAS)
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Median (25% 75%) Mixing Ratio (ppb)
650
700
750
800
850
900
950
1000
1050
0 1 2 3 4 5 6
SO2 over the Eastern USSummer, 2002 (over 100 profiles)
Pre
ssu
re (
hP
a) Scale height ~1.1 km
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