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Unit 7 · Topic 7.2

7.2 Photochemical Smog

Photochemical smog is the brownish haze over sunny, traffic-heavy cities. It forms when nitrogen oxides and volatile organic compounds react in sunlight to make ground-level ozone and other irritants, and it harms both lungs and plants.

Key terms

  • photochemical smog
  • ground-level (tropospheric) ozone
  • volatile organic compounds (VOCs)
  • nitrogen oxides
  • sunlight

The ingredients

  • Nitrogen oxides (NOₓ), mostly from vehicle engines and power plants.
  • Volatile organic compounds (VOCs), carbon-based chemicals that evaporate easily, from gasoline vapor, paints, solvents and some industries. Trees also give off natural VOCs.
  • Sunlight, which supplies the energy for the reactions. That is why it's called photochemical: 'photo' means light.
  • Warm temperatures, which speed up the reactions.

How ozone builds up

Sunlight splits nitrogen dioxide: NO₂ + sunlight → NO + O. The single oxygen atom (O) is very reactive and joins an oxygen molecule to form ozone: O + O₂ → O₃.

Without VOCs, the cycle mostly balances out, because NO reacts with ozone and turns it back into NO₂ and O₂. VOCs break that balance. Sunlight breaks VOCs into reactive fragments that turn NO back into NO₂ without using up ozone, so less NO is left to destroy ozone, and ozone accumulates. VOCs and NOₓ also combine into other smog chemicals such as peroxyacyl nitrates (PANs), which irritate eyes and harm plants.

So smog needs both NOₓ and VOCs plus sunlight. Cutting either NOₓ or VOCs reduces ozone.

A day of smog

If you graph pollutant levels over a sunny weekday in a big city, you'll see a clear sequence. NO rises first, peaking during the morning rush hour as cars start up. NO₂ peaks a little later in the morning as NO reacts in the air. Ozone climbs through the late morning and peaks in the early to mid afternoon, when sunlight is strongest, then falls in the evening as sunlight fades.

Smog is worst in summer, in cities with heavy traffic, lots of sunshine and surrounding mountains that trap air, such as Los Angeles and Mexico City. Thermal inversions (topic 7.3) make it worse.

Effects and solutions

Ground-level ozone irritates the airways, causes coughing and chest pain, reduces lung function and triggers asthma attacks. It also damages plant leaves, reducing photosynthesis and crop yields. Smog reduces visibility too.

Ways to reduce it include driving less and using public transit, catalytic converters that cut NOₓ and unburned hydrocarbons, vapor recovery nozzles at gas pumps that capture VOCs, lower-VOC paints and solvents, and cleaner power plants.

Don't confuse this ground-level ozone with the stratospheric ozone layer high above, which protects you from UV radiation (topic 9.1). Same molecule, different place: harmful near the ground, helpful high up.

Worked examples

Try each one yourself first, then open the solution.

  1. Example 1

    Reading the daily smog pattern

    A graph shows NO, NO₂ and O₃ concentrations over a sunny day in a city. One curve peaks at 7–8 a.m., one at about 10 a.m., and one at about 2 p.m. Identify each curve and explain the order.

    Show the solution
    1. Step 1: The 7–8 a.m. peak is NO, emitted directly by cars during the morning commute.
    2. Step 2: The 10 a.m. peak is NO₂, which forms as NO reacts with oxygen and VOC-derived chemicals in the air, so it lags behind NO.
    3. Step 3: The 2 p.m. peak is ozone. It needs NO₂ to be split by sunlight, and sunlight is most intense around midday to early afternoon, so ozone builds latest.
    4. Step 4: Ozone falls by evening because sunlight weakens and the reactions that make it slow down.

    Answer: 7–8 a.m. = NO; about 10 a.m. = NO₂; about 2 p.m. = O₃. Each forms from the one before, and ozone also needs strong sunlight.

  2. Example 2

    Trap: why smog is worse on sunny days, not just busy ones

    Two cities have the same traffic. City X is cloudy and cool; City Y is hot and sunny. Which has more photochemical smog, and why?

    Show the solution
    1. Step 1: Both cities have similar NOₓ and VOC emissions from traffic.
    2. Step 2: Smog formation is driven by sunlight splitting NO₂, and warmth speeds the reactions.
    3. Step 3: City Y has more sunlight and heat, so more ozone forms from the same emissions.

    Answer: City Y. Same emissions, but more sunlight and heat drive more ozone formation.

Common mistakes

  • Calling ozone a primary pollutant from cars. Cars emit NOₓ and VOCs; ozone forms afterward in sunlight.
  • Mixing up ground-level ozone (harmful smog) with the stratospheric ozone layer (protective).
  • Putting the ozone peak at rush hour. It peaks in the early to mid afternoon, when sunlight is strongest.

On the exam

  • Expect a described graph of NO, NO₂ and O₃ over a day. Explain the order of peaks using emissions plus sunlight.
  • If asked how to reduce smog, name a way to cut NOₓ or VOCs (catalytic converters, vapor recovery nozzles, public transit) and say which precursor it reduces.

Connected topics

Videos

Check yourself

4 questions on 7.2 Photochemical Smog. Pick an answer to see if you got it, and why.

TimeNitrogen monoxide, NO (ppb)Nitrogen dioxide, NO₂ (ppb)Ozone, O₃ (ppb)
6:00 a.m.201510
8:00 a.m.903515
10:00 a.m.407040
2:00 p.m.1530110
8:00 p.m.252535

Hypothetical data from a city on a hot, sunny summer day

Question 1 of 4

Which statement best explains why ozone peaks in the afternoon?

Question 2 of 4

On which kind of day would this city most likely have its worst photochemical smog?

Question 3 of 4

Which policy would most directly reduce the ozone levels shown in the data?

Question 4 of 4

In the formation of photochemical smog, what is the main role of sunlight?

0 of 4 answered