12.12: Reaction Intermediate
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Ozone (O3) depletion in the atmosphere is of significant concern. This gas serves as a protection against the ultraviolet rays of the sun. Ozone is naturally depleted in addition to the depletion caused by human-made chemicals. The depletion reaction is a two-step process:
O3+ultraviolet light→O2+O⋅(free radical) slow reaction
O⋅+O3→2O2fast reaction
The free radical is not a part of the overall equation, but can be detected in the lab.
Reaction mechanisms describe how the material in a chemical reaction gets from the initial reactants to the final products. One reaction that illustrates a reaction mechanism is the reaction between nitrogen monoxide and oxygen to form nitrogen dioxide:
2NO(g)+O2(g)→2NO2(g)
It may seem as though this reaction would occur as the result of a collision between two NO molecules with one O2 molecule. However, careful analysis of the reaction has detected the presence of N2O2 during the reaction. A proposed mechanism for the reaction consists of two elementary steps:
Step 1: 2NO(g)→N2O2(g)
Step 2: N2O2(g)+O2(g)→2NO2(g)
In the first step, two molecules of NO collide to form a molecule of N2O2. In the second step, that molecule of N2O2 collides with a molecule of O2 to produce two molecules of NO2. The overall chemical reaction is the sum of the two elementary steps:
2NO(g)→N2O2(g)N2O2(g)+O2(g)→2NO2(g)2NO(g)+O2(g)→2NO2(g)
The N2O2 molecule is not part of the overall reaction. It was produced in the first elementary step, then reacts in the second elementary step. An intermediate is a species which appears in the mechanism of a reaction, but not in the overall balanced equation. An intermediate is always formed in an early step in the mechanism and consumed in a later step.