Topics of investigatory project in biology for 2 on ozone depletion
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Increment in chlorofluorocarbon dioxide in ozone layer.
At the point when CFCs achieve the stratosphere, the bright radiation from the sun makes them break separated and discharge chlorine particles which respond with ozone, beginning compound cycles of ozone devastation that drain the ozone layer.
One chlorine iota can break separated in excess of 100,000 ozone particles.
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