A molecular probe, 3-amino-2,2,5,5,-tetramethy-1-pyrrolydinyloxy (3ap), was employed to determine the formation rates of one-electron reducing intermediates generated photochemically from both untreated and borohydride-reduced Suwanee River fulvic and humic acids (SRFA and SRHA, respectively). This stable nitroxyl radical reacts rapidly with reducing radicals and other one-electron reductants to produce a relatively stable product, the hydroxylamine, which can be derivatized with fluorescamine, separated by HPLC and quantified fluorimetrically. We provide evidence that O and 3ap compete for the same pool(s) of photoproduced reducing intermediates, and that under appropriate experimental conditions, the initial rate of hydroxylamine formation (R) can provide an estimate of the initial rate of superoxide (O) formation. However, comparison of the initial rates of HO formation (R) to that of R show far larger ratios of R/R (∼6-13) than be accounted for by simple O dismutation (R/R = 2), implying a significant oxidative sink of O (∼67-85%). Because of their high reactivity with O and their likely importance in the photochemistry of CDOM, we suggest that coproduced phenoxy radicals could represent a viable oxidative sink. Because O/phenoxy radical reactions can lead to more highly oxidized products, O could be playing a far more significant role in the photooxidation of CDOM than has been previously recognized.
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http://dx.doi.org/10.1021/acs.est.6b02919 | DOI Listing |
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