The rate constants of the reaction of ozone with DNA, its constituents and related compounds have been determined as a function of pH by competition with nitrite and/or buten-3-ol and, when the rate constant was ≤103 dm3 mol−1 s−1, by the indigo method. Depending on the degree of protonation, the rate constant (in units of dm3 mol−1 s−1) varies substantially, e.g. in the case of cytosine, k = 18 (protonated), k = 1.4 × 103 (neutral) and k = 1.5 × 106 (deprotonated). A similar variation has been found with the other nucleobases. Upon deprotonation the mechanism of the ozone reaction may also change; e.g. no singlet dioxygen (O21Δg) is formed in its reaction with 5-chlorouracil, but when the 5-chlorouracilate ion predominates it becomes a major product (∼42%). Rate constants for the neutral compounds are: thymine (4.2 × 104), thymidine (3.0 × 104), 1,3-dimethyluracil (2.8 × 103), uracil (650), 6-methyluracil (140), 5-chlorouracil (4.3 × 103), orotic acid (5.9 × 103), isoorotic acid (3.7 × 103), 2′-deoxycytidine (3.5 × 103), cytidine (3.5 × 103), adenine (12), 2′-deoxyadenosine (14), adenosine (16), guanosine (1.6 × 104), 2′-deoxyguanosine (1.9 × 104) and DNA (410). In the case of adenine and its derivatives, and thus also in the case of DNA, ˙OH is produced (via O2˙− as an intermediate). For the determination of their intrinsic ozone rate constants, tert-butyl alcohol was added as the ˙OH scavenger.