Abstract

Two aquatic fulvic acids and one soil humic acid were irradiated to examine the resulting changes in the redox and photochemical properties of the humic substances (HS), the relationship between these changes, and their relationship to changes in the optical properties. For all HS, irradiation caused photooxidation, as shown by decreasing electron donating capacities. Photooxidation was accompanied by decreases in specific UV absorbance and increases in the E2/E3 ratio (254 nm absorbance divided by that at 365 nm). In contrast, photooxidation had little effect on the samples' electron accepting capacities. The coupled changes in optical and redox properties for the different HS suggest that phenols are an important determinant of aquatic HS optical properties and that quinones may play a more important role in soil HS. Apparent quantum yields of H2O2, ·OH, and triplet HS decreased with photooxidation, thus demonstrating selective destruction of HS photosensitizing chromophores. In contrast, singlet oxygen ((1)O2) quantum yields increased, which is ascribed to either decreased (1)O2 quenching within the HS microenvironment or the presence of a pool of photostable sensitizers. The photochemical properties show clear trends with SUVA and E2/E3, but the trends differ substantially between aquatic and soil HS. Importantly, photooxidation produces a relationship between the (1)O2 quantum yield and E2/E3 that differs distinctly from that observed with untreated HS. This finding suggests that there may be watershed-specific correlations between HS chemical and optical properties that reflect the dominant processes controlling the HS character.

Highlights

  • Dissolved organic matter (DOM) is a ubiquitous component of natural surface waters produced by transformation of plant and plankton-derived precursor molecules

  • Nordic Aquatic Fulvic Acid (NAFA), Suwannee River Fulvic Acid (SRFA), and Elliot Soil Humic Acid (ESHA) standards were obtained from the International Humic

  • These changes were accompanied by decreases in specific UV absorbance at 280 nm (SUVA280) and increases in E2/E3 (Fig. 2) [29,34,35,63]

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Summary

Introduction

Dissolved organic matter (DOM) is a ubiquitous component of natural surface waters produced by transformation of plant and plankton-derived precursor molecules It comprises moderately hydrophobic aromatic polyelectrolytes of variable molecular weight (100’s to 1000’s of g/mol) [1,2] and plays an important role in the biogeochemistry of aquatic environments. DOM triplet states (3DOM*) are both important precursor species for many of these ROS and strong oxidants in DOM-sensitized photoreactions [7,8,9] Together, these photooxidants play a critical role in the redox speciation of trace metals [10,11,12], transformation rates of organic contaminants [9,13,14,15], and solar inactivation of pathogens [16]

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