The breakdown of ozone in the stratosphere involves a catalytic cycle where chlorine atoms and chlorine monoxide are continuously regenerated to destroy ozone. Reactions outside this cycle are not part of the process.
The breakdown of ozone in the stratosphere is primarily due to catalytic cycles involving certain free radicals such as chlorine (\(Cl\)), bromine (\(Br\)), and others. These cycles involve a series of reactions that result in the conversion of ozone (\(O_3\)) into oxygen gas (\(O_2\)), while regenerating the free radical involved, thus continuing the cycle.
Let's analyze each given reaction to determine which one does not belong to the atmospheric breakdown of ozone:
Therefore, the reaction \(2Cl\dot{O}\rightarrow ClO_2(g)+C\dot{l}(g)\) is not a part of the breakdown of ozone in the stratosphere.