6.2 Stratospheric Ozone Flashcards
how are ozone molecules formed?
solar ultraviolet radiation breaks apart one oxygen molecule (O2) to produce two oxygen atoms (2 O)
each of these highly reactive atoms combines with an oxygen molecule to produce an ozone molecule (O3).
these reactions occur continually whenever solar ultraviolet radiation is present in the stratosphere. As a result, the largest ozone production occurs in the tropical stratosphere
why is stratospheric ozone a dynamic equilibrium?
ozone is constantly being created and destroyed
seasonal changes in stratospheric ozone in polar regions
- cold temps in winter allow formation of clouds of ice particles : polar stratospheric clouds
- ice particles offers surfaces on which chemical reactions can take place, involving chlorine compounds present in the stratosphere as a result of human activities
- Reactions release chlorine atoms
- in the presence of sunlight (UV atoms) in spring -> chlorine atoms destroy ozone in a series of chemical reactions
→ hole in ozone increases in spring - in summer, the ice clouds evaporate, chlorine converted into other compounds (i.e. chlorine nitrate), ozone hole diminishes
Ozone-depleting substances (ODS) examples
- Chlorofluorocarbons (CFCs or freons) - propellants in spray cans, foam, refrigerants
- Hydrochlorofluorocarbons (HCFCs) - replacements for CFCs
- Halon - fire extinguishers
- Methyl bromide - pesticides
- Nitrogen oxides - bacterial breakdown of nitrites and nitrates in the soil, supersonic aircraft
how is ozone depleted by CFCs?
1) UV radiation breaks off a chlorine atom from a CFC molecule.
2) The chlorine atom attacks an ozone molecule (O3), breaking it apart and destroying the ozone.
3) The result is an ordinary oxygen molecule (O2) and a chlorine monoxide molecule (ClO).
4) The chlorine monoxide molecule (ClO) is attacked by a free oxygen atom releasing the chlorine atom and forming an ordinary oxygen molecule (O2).
effects of ultraviolet radiation on human health
exposure to UV-B=
- eye damage (catarcas)
- mutations during cell division, sunburn and in the long term, skin cancers
- immune system can be damaged
effects of ultraviolet radiation on biological productivity
- damage to photosynthetic organisms
- ! phytoplankton (form the basis of aquatic food webs)
- decreases rate of photosynthesis
- mutations
Altering Human Activity to reduce ozone depletion
- Replace gas-blown plastics
- Replace the old fridge with the existing “greenfreeze” technology which does not deplete the ozone
- Non-propellant alternatives
Regulating and reducing pollutants to reduce ozone depletion
- Recover and recycle CFCs from refrigerators and AC units
- legislate to return fridges to manufacturer and coolants
- capture CFCs from scrap products to prevent harm from entering atmosphere
Cleanup and Restoration to reduce ozone depletion
- Add ozone to or remove chlorine from stratosphere
UNEP
- United Nations Environmental Programme
- provide information to countries and public on disadvantages of pollution
Identify issues that still persist with ozone-depleting substances
- illegal market for ODSs continues and requires consistent monitoring
- in many low income countries, there is still a significant demand for CFCs as reliance on equipment using these chemicals remains high
what are reasons for the illegal trade of ODSs?
- ODS substitutes are often costlier than CFCs
- updating equipment to enable use of alternative chemicals is generally expensive
- the lifetime of CFC-containing equipment is often long
- penalties in many countries for ODS smuggling is small
magnitude of illegal ODS trade is between 7000-14000 tonnes of CFCs annually
montreal procotol successes
- by end of 2002: industrialised coutnries reduced ODS consumption by 99%
- raised awareness of effect of ODS on environment
- provided an incentive for countries to find alternatives
Vienna Convention
- 1985
- protection of Ozone Layer
- aimed to protect human health and the environment against adverse effects resulting from human activities which modified or were likely to modify the ozone layer