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PHOTOCHEMICAL FORMATION OF SMOG
SUBMITTED BY:
Keshav Kumar
Singh
Y19266023
Department of Chemistry
Dr. Harisingh Gaur Vishwavidyalaya (A Central University)
Sagar, M.P.
Natural photochemical phenomena have contributed to the
evolution of life and have allowed its continued existence on
the Earth. let us discuss atmospheric structure because
photochemical reactions depend on atmospheric structure.
Region Altitude range
(Km)
Temperature
Range (° C)
Important
Chemical
Species
1) Troposphere 0-11 15 to -56 N2 , O2 , CO2 , H2O
2) Stratosphere 11-50 -56 to -2 O3
3) Mesosphere 50-85 -2 to -92 O2
+ , NO+
4) Thermosphere 85-500 -92 to 1200 O2
+ , NO+ , O+
Photochemical Reactions in Atmosphere
What is Smog ?
 Hydrocarbons and other organic compounds in the
atmosphere are susceptible to oxidation through a series of
steps of chemical and photochemical reactions. As a result
many noxious secondary pollutant products and
intermediates are produced, which belong to the category of
photochemical smog.
 Smog is often seen as brown haze above large cities.
 Frequency and severity depends on local topography,
climate, population density, fossil fuel use.
 Deforestation and burning may also contribute to smog
Two types of pollutants which produce
photochemical smog are primary pollutants and
secondary pollutants.
 Primary Pollutant :
Harmful substances
put directly into air by
human activities.
These include oxides
of nitrogen, volatile
organic compounds
and carbon
monoxide.
 Secondary
Pollutant : These
include ozone,
Nitrogen Dioxide,
hydrogen
peroxide,
peroxyacetyl
nitrate(PAN)
Formation of Photochemical smog
• Hydrocarbons do not react readily with sunlight,
but they are reactive towards other substances
produced photochemically.
• An important characteristic of atmosphere which
are loaded with large quantities of automobile
exhausts, trapped by an inversion layer and at
the same time exposed to intense sunlight, is the
formation of photochemical oxidant in the
atmosphere. This gives rise to the phenomenon
of Photochemical smog.
• Photochemical smog is an oxidizing smog having
high concentration of oxidant (i.e., O3 and NO2 )
Probable Mechanism for Smog
formation
REACTIONS
INVOLVED
REFERENCES:
1) Photochemistry and pericyclic reactions by Jagdamba Singh and Jaya
Singh.
2) https://www.google.com/search?q=health+effects+due+to+photochemi
cal+smog&rlz=1C1RXQR_enIN928IN928&sxsrf=ALeKk017ePkVhLaQ
C3A0ns_hHTbHW8mxAA:1621597588089&source=lnms&tbm=isch&s
a=X&ved=2ahUKEwjviNPh2drwAhWIxzgGHYV7CDYQ_AUoAXoECA
EQAw&biw=1536&bih=666#imgrc=VhzeDj37C1W_vM
3) https://www.epa.sa.gov.au/files/8238_info_photosmog.pdf
4) https://chem.libretexts.org/Ancillary_Materials/Exemplars_and_Case_
Studies/Exemplars/Environmental_and_Green_chemistry/Photochemi
cal_Smog
5) https://www.sciencedirect.com/science/article/pii/S0166111608717928
6) https://www.sciencedirect.com/science/article/abs/pii/S1389556703000
066
Photochemical formation of smog

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Photochemical formation of smog

  • 1. PHOTOCHEMICAL FORMATION OF SMOG SUBMITTED BY: Keshav Kumar Singh Y19266023 Department of Chemistry Dr. Harisingh Gaur Vishwavidyalaya (A Central University) Sagar, M.P.
  • 2. Natural photochemical phenomena have contributed to the evolution of life and have allowed its continued existence on the Earth. let us discuss atmospheric structure because photochemical reactions depend on atmospheric structure. Region Altitude range (Km) Temperature Range (° C) Important Chemical Species 1) Troposphere 0-11 15 to -56 N2 , O2 , CO2 , H2O 2) Stratosphere 11-50 -56 to -2 O3 3) Mesosphere 50-85 -2 to -92 O2 + , NO+ 4) Thermosphere 85-500 -92 to 1200 O2 + , NO+ , O+ Photochemical Reactions in Atmosphere
  • 3. What is Smog ?  Hydrocarbons and other organic compounds in the atmosphere are susceptible to oxidation through a series of steps of chemical and photochemical reactions. As a result many noxious secondary pollutant products and intermediates are produced, which belong to the category of photochemical smog.  Smog is often seen as brown haze above large cities.  Frequency and severity depends on local topography, climate, population density, fossil fuel use.  Deforestation and burning may also contribute to smog
  • 4. Two types of pollutants which produce photochemical smog are primary pollutants and secondary pollutants.  Primary Pollutant : Harmful substances put directly into air by human activities. These include oxides of nitrogen, volatile organic compounds and carbon monoxide.  Secondary Pollutant : These include ozone, Nitrogen Dioxide, hydrogen peroxide, peroxyacetyl nitrate(PAN)
  • 6. • Hydrocarbons do not react readily with sunlight, but they are reactive towards other substances produced photochemically. • An important characteristic of atmosphere which are loaded with large quantities of automobile exhausts, trapped by an inversion layer and at the same time exposed to intense sunlight, is the formation of photochemical oxidant in the atmosphere. This gives rise to the phenomenon of Photochemical smog. • Photochemical smog is an oxidizing smog having high concentration of oxidant (i.e., O3 and NO2 )
  • 7. Probable Mechanism for Smog formation
  • 9.
  • 10. REFERENCES: 1) Photochemistry and pericyclic reactions by Jagdamba Singh and Jaya Singh. 2) https://www.google.com/search?q=health+effects+due+to+photochemi cal+smog&rlz=1C1RXQR_enIN928IN928&sxsrf=ALeKk017ePkVhLaQ C3A0ns_hHTbHW8mxAA:1621597588089&source=lnms&tbm=isch&s a=X&ved=2ahUKEwjviNPh2drwAhWIxzgGHYV7CDYQ_AUoAXoECA EQAw&biw=1536&bih=666#imgrc=VhzeDj37C1W_vM 3) https://www.epa.sa.gov.au/files/8238_info_photosmog.pdf 4) https://chem.libretexts.org/Ancillary_Materials/Exemplars_and_Case_ Studies/Exemplars/Environmental_and_Green_chemistry/Photochemi cal_Smog 5) https://www.sciencedirect.com/science/article/pii/S0166111608717928 6) https://www.sciencedirect.com/science/article/abs/pii/S1389556703000 066