Final answer:
The rate law for the decomposition of ozone in terms of the constants k1, k2, and k−1 is rate = k1k2[O3]^2 / (k−1 + k2[O3]). This is derived using the proposed two-step mechanism and making an assumption that the backward reaction is much slower than the forward reaction.
Step-by-step explanation:
The proposed mechanism for the decomposition of ozone to molecular oxygen involves two elementary steps:
O3 O + O2 (rate constant k1)
O + O3 2O2 (rate constant k2)
There is also a reverse reaction to step 1 that should be considered, where O and O2 combine to reform O3 (rate constant k⁻1). According to the steady-state approximation, the concentration of intermediate species O remains constant because it is produced and consumed at the same rate. Therefore, the rate of its formation in step 1 is equal to its rate of consumption in step 2 and any reverse reaction.
The rate law for the given mechanism can be expressed as:
rate = k2[O][O3]
However, [O] is not directly measurable, so we need to link it to other reactants. We can express [O] from the equilibrium of step 1, assuming that the backward reaction is much slower than the forward reaction:
[O] = k1[O3] / (k⁻1 + k2[O3])
Then by substituting [O] back into the rate law:
rate = k2(k1[O3] / (k⁻1 + k2[O3]))[O3]
This simplifies to:
rate = k1k2[O3]^2 / (k⁻1 + k2[O3])
This rate law now relates the overall rate to the experimental rate constants k1, k2, and k⁻1.