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way of forming nitric oxide. Ozone photodissociation also occurs mainly in the stratosphere, where most of the ozone is. Many of the free oxygen atoms resulting from the photodissociation reaction combine quickly with ordinary oxygen to form new ozone. In other words, this reaction is reversible. The rates at which these reactions occur depend on the availability of the molecules, the availability of sunlight, and the availability, in this case, of the mediator molecule, whose only function is to carry away energy. the stratosphere and in the region above it called the mesosphere. Why? Because that’s where the sunlight first contacts the Popular the skull and rose all over printed shirtatmosphere, and because the reaction absorbs sunlight at just the wavelengths needed to break up the oxygen molecules, so that down in the lower atmosphere not much sunlight in those particular wavelengths remains. What about the other 78% or so of the atmosphere that consists of nitrogen? Is there a reaction that breaks ordinary nitrogen into N + N? No, there isn’t. The chemical bond between the two atoms of nitrogen in the N2 molecule is so

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