INVESTIGATION OF THE PRODUCTION AND DECAY PATHWAYS OF SUPEROXIDE BY CHROMOPHORIC DISSOLVED ORGANIC MATTER

Abstract

Chromophoric dissolved organic matter (CDOM) in natural waters absorbs sunlight which leads to the production of a suite of reactive intermediates and reactive oxygen species (ROS) such as superoxide (O2⦁-) and hydrogen peroxide (H2O2). A significant amount of research over the years has investigated the sources and sinks of these two ROS. The currently accepted sequence of reactions for their production involves photochemically produced one-electron reductants (OER) within CDOM reacting with dissolved oxygen to form O2⦁-, which undergoes self-dismutation to produce H2O2. A previously used method to detect radical species with CDOM has been modified herein to be conducted simply using a fluorometer. Production rates of OER and H2O2 were measured for a variety of samples and correlations between the rates and optical/structural properties of the samples indicate that lower molecular weight species produce more OER and H2O2. Based on the stoichiometry of the mechanism above, the ratio of the production rate of OER to that of H2O2 should be two. However, ratios from five to sixteen were obtained, which suggests that O2⦁- undergoes oxidative reactions that compete with dismutation. The possibility of a light-dependent pathway for O2⦁- decay has been proposed but had yet to be explicitly demonstrated. Herein this sink is directly shown through O2⦁- spiking experiments. Rapid consumption of the O2⦁- spike occurs if injected into a sample during irradiation, as compared to a spike introduced into the sample in the dark, suggesting the presence of a light-dependent sink. Extensive data analysis and kinetic modeling of the O2⦁- decay data has allowed for approximations as to the extent of the sink and its decay rate constant. O2⦁- and H2O2 are environmentally important species, and a significant amount of work has been done on modeling their concentrations in natural waters. Based on the work here, O2⦁- is produced at higher concentrations than previously believed, which has implications on the modeling of O2⦁- and H2O2 in natural waters. Additionally, the light-dependent oxidative sink of O2⦁- could be with moieties within CDOM, providing further insight to the photochemical transformation of DOM during transit from terrestrial sources to marine waters.