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WHAT IS OZONE?
1. O3
2. A gas composed of three atoms of oxygen
3. Bluish gas that is harmful to breathe
4. Nearly 90% of earth’s ozone is in the stratosphere and
referred to as the ozone layer.
5. Ozone absorbs a band of ultraviolet radiation called UVB.
OZONE LAYERS
FORMATION OF OZONE
LAYER
O2 + sunlight  O + O
O + O2  O3
Ozone (O3)
Chemically forms when UV hits on stratosphere
Oxygen molecules dissociate into atomic oxygen
O2 O + O
Atomic oxygen quickly combines with other oxygen
molecules to form ozone
O + O2 O3
OZONE DEPLETION
Ozone layer depletion, is simply the wearing out (reduction) of
the amount of ozone in the stratosphere. Unlike pollution,
which has many types and causes, Ozone depletion has been
pinned down to one major human activity.
Industries that manufacture things like insulating foams,
solvents, soaps, cooling things like Air Conditioners,
Refrigerators and ‘Take-Away’ containers use something called
chlorofluorocarbons (CFCs).
Depletion begins when CFC’s get into the stratosphere. Ultra
violet radiation from the sun breaks up these CFCs.
The breaking up action releases Chlorine atoms. Chlorine
atoms react with Ozone, starting a chemical cycle that
destroys the good ozone in that area.
One chlorine atom can break apart more than 100,000
ozone molecules.
CAUSES OF OZONE
DEPLETION
IMPACTS OF OZONE
DEPLETION
1) HARM TO HUMAN HEALTH:
(a) More skin cancers, sunburns and premature aging of
the skin.
(b) More cataracts, blindness and other eye diseases.
2) ADVERSE IMPACTS ON AGRICULTURE:
(a) Plant growth, especially in seedlings, is harmed by
more intense UV radiation.
(b) Major crop species are particularly vulnerable to
increased UV, resulting in reduced growth,
photosynthesis and flowering.
3) EFFECTS ON PLANTS:
Physiological and developmental processes of plants are
affected by UVB radiation, even by the amount of UVB in
present-day sunlight.

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O.4.pptxdoes u iti opinion Rio Rio Rio Rio k

  • 1. WHAT IS OZONE? 1. O3 2. A gas composed of three atoms of oxygen 3. Bluish gas that is harmful to breathe 4. Nearly 90% of earth’s ozone is in the stratosphere and referred to as the ozone layer. 5. Ozone absorbs a band of ultraviolet radiation called UVB.
  • 3. FORMATION OF OZONE LAYER O2 + sunlight  O + O O + O2  O3
  • 4. Ozone (O3) Chemically forms when UV hits on stratosphere Oxygen molecules dissociate into atomic oxygen O2 O + O Atomic oxygen quickly combines with other oxygen molecules to form ozone O + O2 O3
  • 5. OZONE DEPLETION Ozone layer depletion, is simply the wearing out (reduction) of the amount of ozone in the stratosphere. Unlike pollution, which has many types and causes, Ozone depletion has been pinned down to one major human activity. Industries that manufacture things like insulating foams, solvents, soaps, cooling things like Air Conditioners, Refrigerators and ‘Take-Away’ containers use something called chlorofluorocarbons (CFCs).
  • 6. Depletion begins when CFC’s get into the stratosphere. Ultra violet radiation from the sun breaks up these CFCs.
  • 7. The breaking up action releases Chlorine atoms. Chlorine atoms react with Ozone, starting a chemical cycle that destroys the good ozone in that area. One chlorine atom can break apart more than 100,000 ozone molecules.
  • 9. IMPACTS OF OZONE DEPLETION 1) HARM TO HUMAN HEALTH: (a) More skin cancers, sunburns and premature aging of the skin. (b) More cataracts, blindness and other eye diseases. 2) ADVERSE IMPACTS ON AGRICULTURE: (a) Plant growth, especially in seedlings, is harmed by more intense UV radiation. (b) Major crop species are particularly vulnerable to increased UV, resulting in reduced growth, photosynthesis and flowering.
  • 10. 3) EFFECTS ON PLANTS: Physiological and developmental processes of plants are affected by UVB radiation, even by the amount of UVB in present-day sunlight.