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19 Cards in this Set

  • Front
  • Back
Structure of ozone
2 pi bonds
Breaking down of ozone vs. breaking down of oxygen gas (in terms of wavelengths)
Ozone can be broken down by longer wavelengths than oxygen gas.
Example of a hydroclorofluorocarbon
Chlorodifluoromethane (CHF2Cl)
Why are HClFCs only a temporary solution?
They reduce the ozone layer due to the C - Cl bond in the molecule.
Ozone properties
Pale-bluish gas with a pungent odour, very reactive
Formation of O3
O2 + UV light ->2.O / O2 + .O -> O3
Where is O3 located?
In the stratosphere (15-45 km above earth's surface)
Ozone layer is constantly:
Formed and broken down.
Formation of O3
Photo-dissociation of molecular O2
CFCs
Found in sprays - chemically inert and contain Cl
Ozone bonding
O = O - O
Nitric oxide
(Increased temperature) NO + O3 = NO2 +O2
How does ozone act as a shield?
Absorbs 99% of the sun's harmful UV light.
Ozone formula and place in atmosphere
O3, stratosphere
Properties of ozone (3)
Pale bluish gas, acrid odor, very reactive (powerful oxidizing agent).
Formation of ozone
Photodissociation of molecular oxygen by UV light :
O2 + UV -> 2 .O / O2 + .O -> O3
Ozone is being depleted by
CFCs, nitric oxides etc.
Alternatives for CFCs
Hydrocarbons, hydrochlorofluocarbons, fluorocarbons, hydrofluorocarbons.
Oxygen radicals forming O2 gas (equation)
O3(g) + O(g) -> 2O2 (g)