Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation Photos from 2001 Mecklenburg Country State of the Environment Report.

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Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation
Presentation transcript:

Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation Photos from 2001 Mecklenburg Country State of the Environment Report

2 Arizona’s Valley of the Sun “Brown Cloud” Observed since early 1990’s; contains C Particles and NO 2 (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 Phoenix photo from accessed Mar 2004http://phoenix.about.com/library/weekly/uc051601a.htm

3 Image take from accessed Mar 2004http://

4 Presence of NO 2 (brown gas) results in inevitable formation of ozone NO 2 (brown) + sunlite  NO + O O + O 2  O 3 (Ozone) Control measures to effectively address ground-level ozone must focus on minimizing NO 2 formation

5 Ozone precursors Nitrogen Oxides Dry Air is 78% Nitrogen (N 2 ), 21% Oxygen (O 2 ) 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 (VOC’s) VOC’s continuously emitted by fuel spills, motor vehicles, trees, air fresheners, paints, and countless other sources OH hydroxyl radical is the atmosphere’s “natural detergent” that cleans VOC’s from the air by initiating the process that converts them into carbon dioxide and water

6 Volatile Organic Compound (VOC) Removal Air’s natural VOC cleanser produced from ozone and water Ozone (O 3 ) + UV-B -> O 2 + *O *O + H 2 O  2OH OH works by transforming stable VOC molecules (R-H) into reactive radicals (R) OH + R-H  R + H 2 O Reactive organic radicals immediately combine with oxygen to form peroxide radicals R + O 2  (R-O-O)

7 Formation of Nitrogen Dioxide NO + R-O-O  NO 2 + RO Formation of NO 2 (and O 3 ) driven primarily by: Concentration of VOC’s (near emission sources) Concentration of NO (rural & downwind areas) Concentrations of both NO and VOC’s ***Summertime ozone pollution results from an overload in our air of NO, VOC’s, or both

8 NO and VOC Effects on Ozone Production NO Sensitive Region VOC Sensitive Region Both NO + VOC Sensitive Figure from : accessed Mar 2004http://www-personal.engin.umich.edu/~sillman/ozone.htm

9 ’95-’99 AM NMOC/NO y Ratios for the Plaza Monitoring Site NMOC/NO y NO x Limited VOC Limited From Perry, JL and Owens, PM, “Weekday/Weekend Variability and Long-Term Trends in Traffic, CO, NO y, and Ozone for the Charlotte Metropolitan Area during the 1990's, AWMA, June 2001

10 I-77 Traffic Volume vs. Time of Day Time of Day (Hour) Hourly Volume SunMonTuesWed ThuFriSat From Perry and Owens, AWMA, 2001

Time of Day Avg Hourly NO y Concentration (ppb) SundayMondayTuesdayWednesday ThursdayFridaySaturday May-Sep ‘95-‘98 Plaza Average Hourly NO y From Perry and Owens, AWMA, 2001

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: accessed Mar 2004http://

15 From: accessed Mar 2004http://