Ozone reacts with nitric oxide in the stratosphere according to the overall reaction
O3(g)+NO(g)→O2(g)+NO2(g).
Experimental studies at 250K and 1.0×10−6atm total pressure give the rate law
rate=k[O3][NO].
Two alternative mechanisms have been proposed.
Mechanism A (two-step):
Step 1: O3(g)⇌O2(g)+O(g) (fast equilibrium)
Step 2: O(g)+NO(g)→NO2(g) (slow, rate-determining)
Mechanism B (single-step):
O3(g)+NO(g)+NO(g)→O2(g)+NO2(g)+NO(g) (termolecular elementary step)
Complete the tasks below.
(1) Part 1: a) Derive the rate law predicted by Mechanism A, expressing the rate solely in terms of the measurable concentrations [O3] and [NO].
(2) Part 2: b) Write the rate law that would result if Mechanism B were the correct single elementary step.
(3) Part 3: c) Using your results from parts (a) and (b), identify which mechanism is consistent with the experimentally observed rate law and justify your choice.
(4) Part 4: d) Beyond the rate-law comparison, evaluate the intrinsic likelihood of the elementary step in Mechanism B at 250K and 1.0×10−6atm. Your answer should refer explicitly to the statistical probability of simultaneous three-particle collisions under the given conditions.