
Journal of the American Chemical Society p. 3636 - 3642 (1993)
Update date:2022-08-11
Topics:
Awad
Stanbury
The reaction of chlorine dioxide with excess azide in aqueous media proceeds with complex kinetics and produces N2, N2O, NO3-, Cl-, and ClO2-. In the presence of the spin trap PBN, the reaction is much simpler, and the rate law is -d [ClO2]/dt = k1 [ClO2] [N3-] [PBN]/([PBN] + [ClO2-]k-1/k2), with k1 = 809 M-1 s-1 and k-1/k2 = 19.0 at 25 °C. The inferred mechanism implies that k1 is the rate constant of electron transfer between ClO2 and N3-, k-1 is the reverse rate constant (N3 with ClO2-), and k2 is the rate constant for reaction of N3 with PBN. A dramatically lower value for k1 of 0.62 M-1 s-1 is calculated from the Marcus cross relationship and literature values for the self-exchange rates. The discrepancy is attributed to systematic errors in the literature self-exchange rates that were derived by applying the Marcus cross relationship to reactions of coordination complexes with N3- and ClO2. Such errors develop whenever this method is applied to reactions between species of widely differing size. Correcting for this effect leads to a calculated value of 56 M-1 s-1 for k1, which is in much improved agreement with the observed value. Similar corrections lead to greatly improved correlations for the self-exchange reaction of NO2 with NO2- and the electrontransfer reaction of ClO2 with NO2-.
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