Mechanism of Fenton Oxidation of Levoglucosan in Water
Shinichi Enami, Yu Morino, Kei Sato
Abstract
Levoglucosan (Levo) is a major saccharide formed by the combustion of cellulosic materials. Levo was once considered an inert tracer of biomass-burning aerosols; however, recent studies have indicated that Levo in atmospheric condensed phases does indeed react with atmospheric reactants. Here, we report the results of a time-resolved mass spectrometric study of the oxidation of Levo in aqueous solutions with ferrous ion (Fe 2+ )/hydrogen peroxide (H 2 O 2 ) (i.e., Fenton’s reagent). The major products of the Fenton oxidation of Levo were oxygen-atom-incorporated species (Levo+ n O, n = 1–3). Experiments using Levo-d7 (all C–H bonds replaced by C–D) and D 2 O or H 2 18 O as the solvent revealed that OH predominantly (∼85% of all C–H bonds) abstracts H atoms attached to the carbon atoms possessing a hydroxyl moiety (−OH), which is followed by the formation of a carbonyl moiety (−C═O). Subsequent hydration of these products results in the formation of geminal diols (detected as Levo+1O species). Our results also suggest the formation of α-hydroxy-hydroperoxides (detected as Levo+2O species) that exist in equilibrium, with the compounds possessing a −C═O moiety and with H 2 O 2 . H-abstractions from −O-H were found to be a minor reaction pathway (≤5% of all H-abstractions). The present proposed oxidation mechanisms improve our understanding of how the chemical components of atmospheric condensed phases change by metal-catalyzed aging processes without sunlight.