Let brackets denote number densities and impose a local photochemical steady state. The atomic-oxygen and ozone balances are
Subtracting gives . If photodissociation is the dominant direct ozone loss, , the second balance becomes . Eliminating atomic oxygen yields the Chapman ozone equilibrium
High in the atmosphere ultraviolet photons make large but the third-body density is small; low down, is large but O2-dissociating ultraviolet radiation has been absorbed. Their product peaks at intermediate altitude, producing an ozone layer.

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