Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation - PowerPoint PPT Presentation

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Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation

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Arizona's Valley of the Sun 'Brown Cloud' ... Phoenix photo from http://phoenix.about.com/library/weekly/uc051601a.htm, accessed Mar 2004 ... – PowerPoint PPT presentation

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Title: Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation


1
Charlotte-Rock Hill-Gastonia MSA Summertime
Ozone Formation
Photos from 2001 Mecklenburg Country State of the
Environment Report
2
Arizonas Valley of the Sun Brown Cloud
Phoenix photo from http//phoenix.about.com/librar
y/weekly/uc051601a.htm, accessed Mar 2004
  • Observed since early 1990s contains C
    Particles and NO2 (brown) gas
  • From burning fossil fuels cars, construction
    equipment, power plants, lawn mowers, leaf
    blowers contribute to this brown cloud
  • Weather also a key factor

3
Image take from http//www.al.noaa.gov/WWWHD/Pubdo
cs/TropoRural.html, accessed Mar 2004
4
Presence of NO2 (brown gas) results in inevitable
formation of ozone
NO2 (brown) sunlite ? NO O
O O2 ? O3
(Ozone)
  • Control measures to effectively address
    ground-level ozone must focus on minimizing NO2
    formation

5
Ozone precursors
  • Nitrogen Oxides
  • Dry Air is 78 Nitrogen (N2), 21 Oxygen (O2)
  • Heating air to high temperatures forms NO (motor
    vehicles, fossil-fuel power plants, lightning)
  • NO is an ozone precursor and also reacts
    directly with ozone to destroy it
  • Volatile Organic Compounds (VOCs)
  • VOCs continuously emitted by fuel spills, motor
    vehicles, trees, air fresheners, paints, and
    countless other sources
  • OH hydroxyl radical is the atmospheres natural
    detergent that cleans VOCs from the air by
    initiating the process that converts them into
    carbon dioxide and water

6
Volatile Organic Compound (VOC) Removal
  • Airs natural VOC cleanser produced from ozone
    and water
  • Ozone (O3) UV-B -gt O2 O
  • O H2O ? 2OH
  • OH works by transforming stable VOC molecules
    (R-H) into reactive radicals (R)
  • OH R-H ? R H2O
  • Reactive organic radicals immediately combine
    with oxygen to form peroxide radicals
  • R O2 ? (R-O-O)

7
Formation of Nitrogen Dioxide
  • NO R-O-O ? NO2 RO
  • Formation of NO2 (and O3) driven primarily by
  • Concentration of VOCs (near emission sources)
  • Concentration of NO (rural downwind areas)
  • Concentrations of both NO and VOCs
  • Summertime ozone pollution results from an
    overload in our air of NO, VOCs, or both

8
NO and VOC Effects on Ozone Production
Both NO VOC Sensitive
VOC Sensitive Region
NO Sensitive Region
Both NO VOC Sensitive
Figure from http//www-personal.engin.umich.edu/
sillman/ozone.htm, accessed Mar 2004
9
95-99 AM NMOC/NOy Ratios for the Plaza
Monitoring Site
20
NO
Limited
x
15
y
10
NMOC/NO
VOC Limited
5
0
1994
1995
1996
1997
1998
1999
2000
From Perry, JL and Owens, PM, Weekday/Weekend
Variability and Long-Term Trends in Traffic, CO,
NOy, and Ozone for the Charlotte Metropolitan
Area during the 1990's, AWMA, June 2001
10
I-77 Traffic Volume vs. Time of Day
5000
4000
3000
Hourly Volume
2000
1000
0
Time of Day (Hour)
Sun
Mon
Tues
Wed
Thu
Fri
Sat
From Perry and Owens, AWMA, 2001
11
May-Sep 95-98 Plaza Average Hourly NOy
40
35
y
30
25
Avg Hourly NO
Concentration (ppb)
20
15
10
5
1
3
5
7
9
11
13
15
17
19
21
23
Time of Day
Sunday
Monday
Tuesday
Wednesday
Thursday
Friday
Saturday
From Perry and Owens, AWMA, 2001
12
1990-1998 May-Sep Diurnal Charlotte Ozone
Averages By Day of Week (weekend days-lines,
weekdays-markers
From Perry and Owens, AWMA, 2001
13
Obtained from John White, NC DAQ
14
From http//www.epa.gov/airnow/showmaps.html?/air
now/2000/20000601/8p-ncsc.gif, accessed Mar 2004
15
From http//www.epa.gov/airnow/showmaps.html?/air
now/2000/20000601/8p-ncsc.gif, accessed Mar 2004
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