The Tale of Two Smogs
When we talk about severe air pollution in urban environments, the word smog immediately comes to mind. Coined as a portmanteau of 'smoke' and 'fog', smog is a visible manifestation of toxic air. However, not all smog is created equal. In environmental chemistry, we broadly classify smog into two distinct categories based on their chemical nature and the conditions required for their formation: Classical Smog and Photochemical Smog.
Classical smog, often associated with the infamous Great Smog of London, occurs in cool, humid climates. It is primarily a mixture of smoke, fog, and sulfur dioxide (SO2). Because SO2 is a reducing agent, classical smog is chemically referred to as reducing smog.
The Role of Sunlight
Photochemical Smog
The question specifically asks about the air pollution that occurs in sunlight. This is the ultimate giveaway. Photochemical smog, as the prefix 'photo' implies, is driven by the energy from sunlight ($h
u$).
Unlike its classical counterpart, photochemical smog thrives in warm, dry, and sunny climates—think of cities like Los Angeles or heavily congested metropolitan areas during the summer. The intense solar radiation acts as a catalyst, initiating a cascade of complex chemical reactions in the atmosphere.
The Chemical Recipe
From Exhaust to Oxidants
So, what are the ingredients for this toxic soup? The primary culprits are nitrogen oxides (NOx) and unburnt hydrocarbons. These primary pollutants are continuously pumped into the atmosphere by automobile exhausts and industrial emissions.
When sunlight strikes these primary pollutants, it triggers a photochemical chain reaction. The nitrogen dioxide (NO2) absorbs sunlight and breaks down, eventually leading to the formation of highly reactive secondary pollutants. The most prominent among these are ozone (O3) and peroxyacetyl nitrate (PAN), which has the chemical formula CH3−C(=O)−O−O−NO2.
Conclusion
Oxidising vs Reducing
Because ozone and PAN are exceptionally strong oxidising agents, the resulting photochemical smog is highly oxidising in nature. It often appears as a brownish haze due to the presence of NO2 gas.
Therefore, the air pollution that occurs in sunlight is unequivocally oxidising smog. Understanding this fundamental difference not only helps in solving such direct questions but also builds a strong foundation for tackling complex assertion-reasoning problems in environmental chemistry.