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Lower Atmosphere
basics
1. Extension and composition
2. Greenhouse, light & biosphere
3. Ozone and nitrogen oxides
- ozone
- nitrogen oxides
- ozone smog
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Lower Atmosphere

Basics

Ozone smog

Ozone smog is a significant problem in big cities. Ozone is formed as part of a complicated process involving nitrogen oxides, ozone formation and ozone loss.  Ozone smog formation shows just how interconnected processes in the atmosphere really are.
 

 

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NOx emissions in town

1. NOx emissions in the city.  Image: Anja Kaiser.  Please click to enlarge (80 K).

 

What happens in the city?

Lets make the example simple and assume almost all nitrogen oxides come from combustion processes happening in car engines.  Nitrogen monoxide (NO) rich air rises from the roads. This NO reacts with ozone (O3) already in the air to form nitrogen dioxide (NO2).  So the first part of the reaction cycle actually causes a loss of ozone from the atmosphere.  Indeed, directly over roads, ozone concentrations are often very low.  During ozone smog periods, ozone concentrations in cities can be lower than in the rural areas around.  The plumes of NOx rich air are then transported by the wind to the countryside.

 

An additional problem can arise from diesel cars equipped with particles filters. Although such filters prevent harmful particles in the exhaust gas, the cars often emit more nitrogen dioxide (NO2). At the moment (2008) there was not yet a common technology on the market preventing the emission of particles and NO2 in diesel cars in parallel.
 

organic emissions

2. Organic emissions from forests and industry.  Image: Anja Kaiser.  Please click to enlarge (120 K).

 

Where do organic compounds come from?
 
The second partner needed in the reaction cycle are organic peroxides. What are these and where do they come from? Organic molecules are emitted from forests and other plants but also from human sources (e.g. solvents or fuel at filling stations).  The structure of a few organic compounds, which are abbreviated as RH, are shown here. These compounds are chemically attacked in the air. The typical reaction favoured during the day is the reaction with the hydroxyl radical (OH) followed by addition of an oxygen molecule (O2). The result is a peroxy-radical (RO2), with R representing the unreactive organic part of the molecule.  Radical species have a spare electron which makes them very reactive.

 

formation of ozone smog

3. Formation of ozone smog.  Image: Anja Kaiser.  Please click to enlarge (115 K).

 

When are the best conditions for ozone smog?

Over rural areas, downwind of cities, the ozone formation cycle starts:

1) Nitrogen dioxide (NO2) is broken down by the Sun to form oxygen atoms (O) and nitrogen monoxide (NO).
2) The O atoms react with oxygen gas (O2) to form ozone (O3).
3) The NO reacts with peroxy radicals RO2 forming NO2 again.
4) Some O3 is removed by reaction with NO.  The amount lost depends on the concentration of the competing RO2 radicals.

 

In the end the peroxy radicals are lost and ozone is formed while the nitrogen oxides are always recycled. This cycle only happens if:

a) There is enough sunlight to breakdown NO2 into NO and O (the reaction happens on hot sunny days).
b) If the mixture of peroxy-radicals and nitrogen oxides favours the reaction.

 

the complete ozone oxidation cycle

4. The complete ozone oxidation cycle.  Image: Anja Kaiser. ESPERE

If no nitrogen oxides are available, the reaction cycle can't take place.
If nitrogen oxide concentrations are very high, NO reacts not only with peroxy radicals but also with ozone and this removes ozone from the system.
If sunlight is not available, NO can't be recycled again and not enough peroxy radicals are formed to keep the cycle going.

Nitrogen oxide concentrations are usually low enough to prevent severe ozone smog events occurring but if we continue to emit them during combustion processes, ozone smog events are likely to increase.  A comparable situation is seen in the smoke plume of a vegetation fire as the temperatures generated in these fires are hot enough to allow nitrogen oxide to form.

 

Related pages

Find out more about how tropospheric ozone levels are controlled at:
Lower Atmosphere - More - Unit 3 - Ozone abundance

 

About this page:
author: Dr. Elmar Uherek - Max Planck Institute for Chemistry, Mainz, Germany
scientific reviewing: Dr. Rolf von Kuhlmann - Max Planck Institute for Chemistry, Mainz, Germany
educational proofreading: Michael Seesing - Uni Duisburg , Germany- 2003-07-02
last published: 2008-10-09

 

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last updated 10.10.2008 15:11:21 | © ESPERE-ENC 2003 - 2013