Chemistry · Ch 13 — Environmental Chemistry
Photochemical Smog
Photochemical Smog
Photochemical smog is a brownish, oxidising haze that forms over sunny cities with heavy
vehicular traffic -- Los Angeles and, more relevantly for us, many large Indian cities on a clear,
bright day are classic settings for it. Unlike classical smog, it needs no fog and no coal-burning:
its two essential raw ingredients are oxides of nitrogen () and unburnt hydrocarbons,
both supplied in abundance by vehicle exhaust, and its essential extra ingredient is strong sunlight, which drives the whole sequence of reactions.
The formation sequence, in outline (see the accompanying figure for the full cycle), runs as
follows:
- Vehicle exhaust releases , which is oxidised in air to .
- Sunlight splits back into and a free oxygen atom: .
- That free oxygen atom reacts immediately with in air to form ozone: .
- Meanwhile, unburnt hydrocarbons react with oxygen and with through a chain of free-radical steps to produce peroxyacetyl nitrate (PAN).
- Ozone and PAN accumulate through the day as sunlight keeps driving the cycle, both being strong oxidising agents and irritants -- which is why photochemical smog, chemically, is described as oxidising, the opposite character to classical smog.
The nitrogen dioxide in this cycle plays what is often called a catalytic role: it is consumed
in step 2 but regenerated as is re-oxidised back to in step 1, so the
- pair keeps cycling through the reaction rather than being used up,
sustaining ozone production for as long as sunlight and hydrocarbons are available.
Effects. On humans, ozone and PAN irritate the eyes (a stinging, watering sensation) and the
respiratory tract, and can aggravate asthma and other lung conditions; prolonged exposure is linked
to reduced lung function. On plants, ozone damages leaf tissue, causing visible bronzing or …
What this figure shows. A reaction-cycle diagram of photochemical smog formation: vehicle exhaust arrows feed and unburnt hydrocarbons into a central sunlight ("") box; is oxidised to by atmospheric oxidants; sunlight then splits into and a free oxygen atom (); the free oxygen atom combines with to give ozone (), shown looping back to react with more hydrocarbons; a parallel branch shows hydrocarbon free radicals reacting with and to yield peroxyacetyl nitrate (PAN); the cycle's two end products, ozone and PAN, are shown exiting the diagram as the haze's harmful oxidants, with the regenerated $\ …