In ozone reactions, singlet dioxygen [O 2 ( 1 ∆ g )] is formed when ozone reacts by O-atom transfer. O 2 ( 1 ∆ g ) yields were determined for more than 50 compounds using as reference the reaction of hydrogen peroxide with hypochlorite. Close to 100% yields were found in the reaction of O 3 with sulfides, disulfides, methanesulfinic acid, and nitrite. In accordance with this, the only products are: methionine sulfoxide, methanesulfonic acid, and nitrate for the reaction of O 3 with methionine, methanesulfinic acid, and nitrite, respectively. In the case of aliphatic tertiary amines (trimethylamine, triethylamine, and DABCO), the O 2 ( 1 ∆ g ) yields range between 70 and 90%, the aminoxide being the other major product. With EDTA and nitrilotriacetic acid (NTA), the O 2 ( 1 ∆ g ) yield is around 20%. The interpretation of the data with DABCO required the determination of the quenching constant of O 2 ( 1 ∆ g ) by this amine, k q = 1.8 × 10 9 dm 3 mol Ϫ1 s Ϫ1 in H 2 O and D 2 O, two orders of magnitude lower than previously reported. Aromatic tertiary amines give even lower O 2 ( 1 ∆ g ) yields [N,N-dimethylaniline (7%), N,N,N Ј,N Ј-tetramethylphenylenediamine (9%)]. Substantial amounts of O 2 ( 1 ∆ g ) are also formed with the DNA model compounds, 2Ј-deoxyguanosine (40%) and 2Ј-deoxyadenosine (15%, in the presence of tert-butyl alcohol as ؒ OH scavenger). The pyrimidine nucleobases only yield O 2 ( 1 ∆ g ) when deprotonated at N(1). O 2 ( 1 ∆ g ) formation is also observed with hydrogen sulfide (15%), azide (17%), bromide (56%), iodide (12%), and cyanide ions (20%). The O 2 ( 1 ∆ g ) yield from the reaction of O 3 with phenols and phenolates is typically around 20%, but may rise closer to 50% in the case of pentachloro-and pentabromophenolate. Low O 2 ( 1 ∆ g ) yields are found with unsaturated acids such as dihydroxyfumarate (6%), muconate (2%), and acetylenedicarboxylate (15%). With saturated compounds, also, no O 2 ( 1 ∆ g ) (e.g. with propan-2-ol, acetaldehyde, acetaldehyde dimethylacetal and glyoxal) or very little O 2 ( 1 ∆ g ) (formic acid; 6%, at high formate concentrations) was detected. As shown with some examples, knowledge of the O 2 ( 1 ∆ g ) yield (in combination with that of other products) is a prerequisite for the elucidation of the mechanisms of O 3 reactions in aqueous solutions.