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In the stratosphere, ultraviolet (UV) radiation breaks down chlorofluorocarbons (like Freons, e.g., CF2Cl2, releasing highly reactive chlorine free radicals (Cl•). These radicals act as catalysts that continuously break down ozone molecules O3 into oxygen O2.
This step correctly shows UV light cleaving a C-Cl bond to generate the initial reactive chlorine free radical.
The chlorine radical attacks an ozone molecule, destroying it and producing a chlorine monoxide radical ($$Cl^•$$O).
The chlorine monoxide radical reacts with a free oxygen atom, regenerating the catalytic chlorine radical to continue the cycle.
This hypothetical step does not occur in any atmosphere layer because it is energetically unfavorable and unstable.
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