One of the steps involved in the depletion of ozone in the stratosphere by nitric acid (NO) may be represented as: NO(g)+O3(g)⟶NO2(g)+O2(g) The oxidation number of N changes from +2 to +4.
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Solution
NO(g)+O3(g)⟶NO2(g)+O2(g)
Hence, the oxidation state of N changes from +2 to +4.