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Course: LLB
Subject : Environment Laws
Unit: 3
Course: LLB
Subject : Environment Laws
Unit: 3
Ozone Depletion
Importance of the ozone layer
• Near ground level (trochosphere) -
pollution
• Form photochemical smog and acid rain
• In the stratosphere (15 - 50 km) - ozone
layer screen out harmful Ultra-violet
radiation from the sun.
Our atmosphere [1]
 Troposphere:
- The lowest layer (about 15 km from the ground)
- Contains normal air composed of N2, O2, water vapour, CO2, etc.
- Temperature decreases with altitude
 Stratosphere:
- Above the troposphere
- Temperature increases with altitude
- Contains a lot of ozone (ozone layer):
• Found in the stratosphere between 10 - 50km above the ground
• Protects us from the harmful effects of UV of certain wavelengths
• Decrease in ozone concentration  Increase in UV-B radiation
reaching the earth surface
Formation of ozone layer
O2 + sunlight  O + O
O + O2  O3
Ozone formation [2]
Ozone (O3)
 Chemically forms when UV hits on stratosphere
 Oxygen molecules dissociate into atomic oxygen
 Atomic oxygen quickly combines with other oxygen molecules
to form ozone
O2 O + O
O + O2 O3
Ozone formation [3]
Ozone (O3)
 A pollutant on ground level
– A component of photochemical smog
 Important for our survival
– Absorbs some of the potentially harmful UV radiation
which can cause skin cancer and damage to vegetation
 Split and regenerate repeatedly
 Highest concentration in the upper atmosphere
 Concentration decreases at lower altitudes
Ozone formation [1]
Ozone (O3)
 Made up of three oxygen atoms
 Occurs naturally as a layer in the stratosphere
 The layer is thinnest around the equator and the concentration
increases towards the poles
 The amount of ozone above a point on the earth’s surface is
measured in Dobson units (DU)
– ~ 260 DU near the Tropics
– higher elsewhere
What is CFCs? [1]
 Chlorofluorocarbons (CFCs)
 Composed of elements chlorine, fluorine, and carbon
 Developed in 1930 by DuPont
 CFCs were welcomed by industries:
– Low toxicity
– Chemical stability
– Cheap
 Usage:
– As refrigerants
– As blowing agents
– For making flexible foam
– As cleaning agents
– As propellants
What is CFCs? [2]
CFCs are used in aerosol sprays
(Sources: http://www.yahoo.com) CFCs were used as refrigerants in the
past (Sources: http://www.yahoo.com )
Present situation
 Stratospheric ozone over Antarctica:
– Has been depleted over the last 15 years
– The ozone hole:
 enlarging
 large enough to cover most of the North America
 would take at least 50 years to restore
Destruction of ozone layer
Chlorine atoms from CFCs attack the
ozone, taking away ozone and forming
chlorine monoxide (ClO).
O3 + Cl  O2 + ClO
Chlorine monoxide then combines with
another oxygen atom to form a new
oxygen molecule and a chlorine atom.
ClO + O  Cl + O2
The chlorine atom is free to destroy up to 100,000 ozone
molecules
Causes of ozone depletion
 Details are not fully understood
 Catalyzed by halocarbons (carbon compounds containing fluorine,
chlorine, bromine and iodine)
– Examples: CFCs and ClONO2
 Halogen atoms catalyze ozone layer depletion by destroying ozone
molecules and forming oxygen molecules.
 Much more serious in Antarctica than other regions on the planet
Consequences of less ozone
• Because CFCs has long life span and
very stable, it continuous to attack
the ozone layer and more UV-B
reach our earth.
Health
• Sunburn, eye diseases (cataract),
skin cancer.
• Reduce our immune system 
other diseases
Impacts on human health
 Skin Cancer
 Cataracts and Other Eye Damages
 Suppression of Immunity
Food supply
• Reduce photosynthesis - crops
affected.
• Kills plankton  fish 
Impacts on other animals
 Reduces plankton population
 Reduces penguin population
 Reduces the percentage of hatching of
frog eggs
What has been done? [1]
 Ban the use of CFCs as aerosol propellants
 The Vienna Convention on the Protection of the Ozone Layer in 1985
– Governments committed themselves to protect the ozone
layer and to co-operate with each other to improve
understanding of ozone crisis.
 The Montreal Protocol on Substances that deplete the Ozone Layer
– Adopted by Governments in 1987
– Aims to reduce and eventually eliminate the emissions of
man-made ozone-depleting substances.
International cooperation:
What has been done? [2]
 SunWise School Program by EPA of the
US
 Phaseout of production of CFCs
 Substitutes for CFCs
Relevant websites [1]
 US Environmental Protection Agency (http://www.epa.gov)
– The Science of Ozone Depletion
(http://www.epa.gov/students/ozone_depletion.htm)
– United States Environmental Protection Agency: Ozone
Depletion Home Page (http://www.epa.gov/docs/ozone/)
 USA NASA (http://www.nasa.gov)
– NASA-Stratospheric Ozone Depletion Tutorial
(http://www.nas.nasa.gov/About/Education/Ozone)
 Union of Concerned Scientists (http://www.ucsusa.org)
– Ozone Depletion
(http://www.ucsusa.org/ozonedepletion/ozone.sciupdate.html
Relevant websites [2]
 The National Oceanic and Atmospheric Administration (NOAA)
(http://www.al.noaa.gov)
– WMO/UNEP Scientific Assessment of Ozone Depletion
1994
(http://www.al.noaa.gov/WWWHD/pubdocs/Assessment94
.html)
 Hong Kong Cyber Campus (http:/www.hkcampus.net/main.phtml)
– Ozone depletion (http://cwc.hkcampus.net/~cwc-
fkc/Ozone%20Depletion.files/frame.htm)
– Chemistry Summer Project Work
(http://ucc.hkcampus.net/~ucc-ckt/ozone/first.htm)
http://archive.greenpeace.org/~ozone/gallery/sshow/sshow.html
Thank You

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Llb el u 3.1 ozone.delpetion

  • 1. Course: LLB Subject : Environment Laws Unit: 3 Course: LLB Subject : Environment Laws Unit: 3
  • 3. Importance of the ozone layer • Near ground level (trochosphere) - pollution • Form photochemical smog and acid rain • In the stratosphere (15 - 50 km) - ozone layer screen out harmful Ultra-violet radiation from the sun.
  • 4.
  • 5. Our atmosphere [1]  Troposphere: - The lowest layer (about 15 km from the ground) - Contains normal air composed of N2, O2, water vapour, CO2, etc. - Temperature decreases with altitude  Stratosphere: - Above the troposphere - Temperature increases with altitude - Contains a lot of ozone (ozone layer): • Found in the stratosphere between 10 - 50km above the ground • Protects us from the harmful effects of UV of certain wavelengths • Decrease in ozone concentration  Increase in UV-B radiation reaching the earth surface
  • 6. Formation of ozone layer O2 + sunlight  O + O O + O2  O3
  • 7. Ozone formation [2] Ozone (O3)  Chemically forms when UV hits on stratosphere  Oxygen molecules dissociate into atomic oxygen  Atomic oxygen quickly combines with other oxygen molecules to form ozone O2 O + O O + O2 O3
  • 8. Ozone formation [3] Ozone (O3)  A pollutant on ground level – A component of photochemical smog  Important for our survival – Absorbs some of the potentially harmful UV radiation which can cause skin cancer and damage to vegetation  Split and regenerate repeatedly  Highest concentration in the upper atmosphere  Concentration decreases at lower altitudes
  • 9. Ozone formation [1] Ozone (O3)  Made up of three oxygen atoms  Occurs naturally as a layer in the stratosphere  The layer is thinnest around the equator and the concentration increases towards the poles  The amount of ozone above a point on the earth’s surface is measured in Dobson units (DU) – ~ 260 DU near the Tropics – higher elsewhere
  • 10. What is CFCs? [1]  Chlorofluorocarbons (CFCs)  Composed of elements chlorine, fluorine, and carbon  Developed in 1930 by DuPont  CFCs were welcomed by industries: – Low toxicity – Chemical stability – Cheap  Usage: – As refrigerants – As blowing agents – For making flexible foam – As cleaning agents – As propellants
  • 11. What is CFCs? [2] CFCs are used in aerosol sprays (Sources: http://www.yahoo.com) CFCs were used as refrigerants in the past (Sources: http://www.yahoo.com )
  • 12. Present situation  Stratospheric ozone over Antarctica: – Has been depleted over the last 15 years – The ozone hole:  enlarging  large enough to cover most of the North America  would take at least 50 years to restore
  • 13.
  • 14. Destruction of ozone layer Chlorine atoms from CFCs attack the ozone, taking away ozone and forming chlorine monoxide (ClO). O3 + Cl  O2 + ClO Chlorine monoxide then combines with another oxygen atom to form a new oxygen molecule and a chlorine atom. ClO + O  Cl + O2 The chlorine atom is free to destroy up to 100,000 ozone molecules
  • 15. Causes of ozone depletion  Details are not fully understood  Catalyzed by halocarbons (carbon compounds containing fluorine, chlorine, bromine and iodine) – Examples: CFCs and ClONO2  Halogen atoms catalyze ozone layer depletion by destroying ozone molecules and forming oxygen molecules.  Much more serious in Antarctica than other regions on the planet
  • 16. Consequences of less ozone • Because CFCs has long life span and very stable, it continuous to attack the ozone layer and more UV-B reach our earth.
  • 17. Health • Sunburn, eye diseases (cataract), skin cancer. • Reduce our immune system  other diseases
  • 18. Impacts on human health  Skin Cancer  Cataracts and Other Eye Damages  Suppression of Immunity
  • 19. Food supply • Reduce photosynthesis - crops affected. • Kills plankton  fish 
  • 20. Impacts on other animals  Reduces plankton population  Reduces penguin population  Reduces the percentage of hatching of frog eggs
  • 21. What has been done? [1]  Ban the use of CFCs as aerosol propellants  The Vienna Convention on the Protection of the Ozone Layer in 1985 – Governments committed themselves to protect the ozone layer and to co-operate with each other to improve understanding of ozone crisis.  The Montreal Protocol on Substances that deplete the Ozone Layer – Adopted by Governments in 1987 – Aims to reduce and eventually eliminate the emissions of man-made ozone-depleting substances. International cooperation:
  • 22. What has been done? [2]  SunWise School Program by EPA of the US  Phaseout of production of CFCs  Substitutes for CFCs
  • 23. Relevant websites [1]  US Environmental Protection Agency (http://www.epa.gov) – The Science of Ozone Depletion (http://www.epa.gov/students/ozone_depletion.htm) – United States Environmental Protection Agency: Ozone Depletion Home Page (http://www.epa.gov/docs/ozone/)  USA NASA (http://www.nasa.gov) – NASA-Stratospheric Ozone Depletion Tutorial (http://www.nas.nasa.gov/About/Education/Ozone)  Union of Concerned Scientists (http://www.ucsusa.org) – Ozone Depletion (http://www.ucsusa.org/ozonedepletion/ozone.sciupdate.html
  • 24. Relevant websites [2]  The National Oceanic and Atmospheric Administration (NOAA) (http://www.al.noaa.gov) – WMO/UNEP Scientific Assessment of Ozone Depletion 1994 (http://www.al.noaa.gov/WWWHD/pubdocs/Assessment94 .html)  Hong Kong Cyber Campus (http:/www.hkcampus.net/main.phtml) – Ozone depletion (http://cwc.hkcampus.net/~cwc- fkc/Ozone%20Depletion.files/frame.htm) – Chemistry Summer Project Work (http://ucc.hkcampus.net/~ucc-ckt/ozone/first.htm) http://archive.greenpeace.org/~ozone/gallery/sshow/sshow.html