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Air Pollution

Secondary Pollutants

Why in the News?

A recent analysis by the Centre for Research on Energy and Clean Air has revealed that secondary pollutants now contribute nearly one third of Delhi’s annual PM2.5 load, highlighting a major shift in the nature of urban air pollution.

What are Secondary Pollutants?

  • Secondary pollutants are not emitted directly from pollution sources.
  • They are formed in the atmosphere when primary pollutants such as SO₂, NOx and VOCs undergo chemical reactions.
  • These reactions are influenced by sunlight, temperature, humidity and stagnant air conditions.
  • They often accumulate downwind and over time, making monitoring and control more complex than primary pollutants.

Major Secondary Pollutants

  • Secondary PM2.5: Ammonium sulfate and Ammonium nitrate
  • Ozone (O₃): Formed from nitrogen oxides (NOx) and volatile organic compounds (VOCs) in the presence of sunlight
  • Acids: Sulfuric acid and Nitric acid (contributors to acid rain)
  • Photochemical smog components: Peroxyacetyl nitrates (PANs) and Nitrogen dioxide (NO₂)

Implications

Regional and transboundary impact

  • Secondary aerosols can travel hundreds of kilometres
  • Delhi’s air quality is influenced by emissions from coal intensive states beyond the NCR

Winter smog intensification

  • Moist and stagnant winter air sharply increases secondary PM2.5

Health risks

  • Fine secondary particles penetrate deep into the lungs
  • Increase risks of respiratory and cardiovascular diseases

Prelims Pointers

  • Secondary pollutants are formed in the atmosphere, not emitted directly
  • Ammonia plays a key role in secondary PM2.5 formation
  • Winter meteorology is crucial for secondary aerosol build up
  • Air pollution control requires regional coordination, not only city level measures
[2013] Photochemical smog is a resultant of the reaction among 

(a) NO₂, O₃ and peroxyacetyl nitrate in the presence of sunlight

(b) CO₂, O₂, and peroxyacetyl nitrate in the presence of sunlight

(c) CO, CO₂, and NO₂ at low temperature

(d) high concentration of NO₂, O₃ and CO in the evening

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