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Ozone
molecules that protect the Earth from harsh UV rays. They are mainly found in the strartosphere
Ozone thickness
Thicker in the spring / thinner in the summer
Thinner in the equator / thicker near the poles
Ozone's dynamic equilibrium
The UV rays from the sun causes the ozone molecules to break apart in order to absorb the UV rays. However, they later reform under normal conditions.
Halogen atoms
cause chemical depletion of stratospheric ozone over the globe by slowing down the rate of ozone production
CFCs
Destroys the straspheric ozone layer
Ex: 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
Carbon tetrachloride - cleaning substance
Effects of UV rays
Increase in mutation rates in DNA causing cancer
Can cause eye cataracts
Can damage the ability to carry out photosynthesis in plants and phytoplankton
Reduces primary production and therefore total productivity
Damage to immune system
Solutions to helping ozone
recycling refrigerants
developing alternatives to gas-blown plastics, halogenated pesticides, propellants and aerosols
developing non-propellant alternatives.