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#ozone–oxygen_cycle

Ozone–oxygen cycle

Biogeochemical cycle

The ozone–oxygen cycle is the process by which ozone is continually regenerated in Earth's stratosphere, converting ultraviolet radiation (UV) into heat. In 1930 Sydney Chapman resolved the chemistry involved. The process is commonly called the Chapman cycle by atmospheric scientists.

Mon 1st

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Ozone–oxygen cycle Oxygen cycle Ozone layer Ozone Ozone depletion Stratosphere Chemical cycling Geochemical cycle List of cycles Null cycle
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