Abstract

The photochemical reactivity of humic substances plays a critical role in the global carbon cycle, and influences the toxicity, mobility, and bioavailability of contaminants by altering their molecular structure and the mineralization of organic carbon to CO2. Here, we examined the simulated irradiation process of Chinese standard fulvic acid (FA) and humic acid (HA) by using excitation-emission matrix fluorescence combined with fluorescence regional integration (FRI), parallel factor (PARAFAC) analysis, and kinetic models. Humic-like and fulvic-like materials were the main materials (constituting more than 90%) of both FA and HA, according to the FRI analysis. Four components were identified by the PARAFAC analysis: fulvic-like components composed of both carboxylic-like and phenolic-like chromophores (C1), terrestrial humic-like components primarily composed of carboxylic-like chromophores (C2), microbial humic-like overwhelming composed of phenolic-like fluorophores (C3), and protein-like components (C4). After irradiation for 72 h, the maximum fluorescence intensity (F max) of C1 and C2 of FA was reduced to 36.01–58.34%, while the F max of C3 of both FA and HA also decreased to 0–9.63%. By contrast, for HA, the F max of its C1 and C2 increased to 236.18–294.77% when irradiated for 72 h due to greater aromaticity and photorefractive tendencies. The first-order kinetic model (R 2 = 0.908–0.990) fitted better than zero-order kinetic model (R 2 = 0–0.754) for the C1, C2, and C3, of both FA and HA, during their photochemical reactivity. The photodegradation rate constant (k 1) of C1 had values (0.105 for FA; 0.154 for HA) that surpassed those of C2 (0.059 for FA, 0.079 for HA) and C3 (0.079 for both FA and HA) based on the first-order kinetic model. The half-life times of C1, C2, and C3 ranged from 6.61–11.77 h to 4.50–8.81 h for FA and HA, respectively. Combining an excitation-emission matrix with FRI and PARAFAC analyses is a powerful approach for elucidating changes to humic substances during their irradiation, which is helpful for predicting the environmental toxicity of contaminants in natural ecosystems.

Highlights

  • Humic substances (HSs) are mixture of heterogeneous organic molecules that are ubiquitous in terrestrial and aquatic ecosystems, playing an essential role in biogeochemical and ecological processes (Du et al, 2016)

  • The photochemical reactivity of HSs was investigated by excitation-emission matrix (EEM) combined with FRI and PARAFAC and kinetic models

  • 424–444 nm) for fulvic acid (FA), and another one, Peak D (Ex/Em: 272/ 484 nm) for humic acid (HA), were observed in the EEMs before apply the irradiation treatment. The positioning of those peaks underwent a differential red shift during the irradiation process, this related to the changed structural composition of the FA and HA components

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Summary

Introduction

Humic substances (HSs) are mixture of heterogeneous organic molecules that are ubiquitous in terrestrial and aquatic ecosystems, playing an essential role in biogeochemical and ecological processes (Du et al, 2016). HSs are significant portion of aquatic dissolved organic matter (DOM), which are isolated and purified by ruling out hydrophilic acid, lipids, proteins etc. The photochemical reactivity of DOM produces dissolved inorganic carbon (Gao, 1998), in addition to organic molecules of low molecular weight (Kulovaara, 1996; Gonsior et al, 2014) and complex aromatic structures (Timko et al, 2015), all of which could influence the toxicity, mobility, and transformation of aquatic contaminants (Kida et al, 2019). Many previous studies have focused on the photodegradation of non-purified DOM in natural water (Zhu et al, 2017; Kida et al, 2019). How photochemical reactivity variously acts upon the structures and functions of HSs is still not well understood; the proper isolation and purification of HSs is critical to elucidate photochemical reactivity mechanisms

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