Abstract

Dissolved organic matter (DOM) controls the degradation and sequestration of aquatic pollutants and, in turn, water quality. In particular, pollutant degradation is performed by oxidant species that are generated by exposure of DOM to solar light, yet, since DOM is a very complex mixture of poorly known substances, the relationships between potential oxidant precursors in DOM and their oxydative capacity is poorly known. Here, we hypothesized that production of oxidant species could be predicted using fluorescence analysis. We analysed water samples from an alluvial plain by fluorescence spectroscopy; the three-dimensional spectra were then decomposed into seven individual components using a multi-way algorithm. Components include a protein-like fluorophore, e.g. tryptophan-like and tyrosine-like, three humic fluorophores, 2-naphthoxyacetic acid, and a by-product. We compared component levels with the ability of water samples to generate reactive species under solar light. The results show a strong correlation between reactive species production and the intensity of two humic-like fluorophores assigned to reduced quinones. Monitoring these fluorophores should thus allow to predict the ability of DOM degradation of pollutants in surface waters.

Highlights

  • Dissolved organic matter (DOM) encompasses ubiquitous natural components able to generate oxidant species under solar light exposure and to degrade aquatic pollutants in surface waters

  • Our goal was to investigate the fluorophores linked to the photochemical generation of oxidant species such as DOM triplet excited states (3DOM*) and singlet oxygen (SO) on waters sampled in an experimental site

  • Component C4 is a widespread component that has been described as high molecular weight fluorophores (Kowalczuk et al 2013; Murphy et al 2006; Stedmon et al 2007)

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Summary

Introduction

Dissolved organic matter (DOM) encompasses ubiquitous natural components able to generate oxidant species under solar light exposure and to degrade aquatic pollutants in surface waters. Previous works have shown that the capacity of DOM to generate reactive species under solar irradiation. Our goal was to investigate the fluorophores linked to the photochemical generation of oxidant species such as DOM triplet excited states (3DOM*) and singlet oxygen (SO) on waters sampled in an experimental site. This site was chosen because it offers a variety of water types: riverine, underground and stagnant. The exploration of correlations between component intensities and rates of oxidant species formation allowed to connect reactive species formation to

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