■ Nitrite (NO 2 – ) is further reduced to nitric oxide (NO), molecular nitrogen
(N 2 ), and nitrous oxide (N 2 O).
Nitrous oxide also causes ozone depletion whereby nitrous oxide (N 2 O)
gives rise to nitric oxide (NO) on reaction with oxygen atoms: N 2 O + O → 2NO
and NO in turn reacts with ozone: NO + O 3 → NO 2 + O 2 . Nitrous oxide is one
of the most significant ozone-depleting substances and is expected to remain so
throughout the 21st century.
OZONE (O 3 )
Ozone is an inorganic molecule with the chemical formula O 3 . Tropospheric
ozone is a secondary air pollutant. Examples include: (1) UV reacting with the
NOx released by vehicles, which causes oxygen atoms to react with O 2 gas,
resulting in ozone O 3 :
NO 2 + uv → NO + O
O + O 2 → O 3
or (2) when volatile organic compounds (VOCs) react with NOx, producing
peroxyacyl nitrates (PANs), which are powerful respiratory and eye irritants that
are present in photochemical smog:
NOx + VOCs → PANs + O 3
Human activities that can lead to the formation of tropospheric ozone include
burning fossil fuels (e.g., power plants, motor vehicles, etc.) and releasing
VOCs. Ozone is a short-lived greenhouse gas that decays in the atmosphere
much more quickly than carbon dioxide does. Because of its short-lived nature,
tropospheric ozone does not have strong global effects, but instead is more
influential in its effects on smaller, more localized areas.
Tropospheric ozone can:
■ Harm lung function and irritate the respiratory system
■ Cause asthma and bronchitis
■ Suppress the immune system
■ Result in heart attacks and other cardiopulmonary problems