Elsevier

Chemosphere

Volume 64, Issue 7, August 2006, Pages 1204-1211
Chemosphere

Effects of photodegradation of dissolved organic matter on the binding of benzo(a)pyrene

https://doi.org/10.1016/j.chemosphere.2005.11.043Get rights and content

Abstract

Dissolved organic matter (DOM) in natural waters can bind various organic pollutants, and the affinity of this binding is strongly influenced by the chemical characteristics of the DOM and water pH. This study examined the effects of photochemically induced alteration of the DOM’s chemical properties and water pH on the binding of benzo(a)pyrene (BaP). Time- and pH-series of solar-simulated irradiations were performed on a natural water sample and aqueous DOM solutions prepared from aquatic and soil humic substances. The binding affinity of BaP, expressed as a partition coefficient of a compound to DOM, decreased substantially after the DOM samples were irradiated over environmentally relevant radiation doses and pH ranges. The lowering of the pH due to the photoproduction of acidic products often partly offsets the reduction of the binding affinity caused by direct photoalteration of the DOM’s chemical structure. The decrease of the binding affinity, after correction for the photoinduced pH change, was positively correlated with the decrease in the molecular weight and the aromaticity of the DOM in the course of irradiation. Increasing O2 abundance accelerated the decrease of the binding affinity as a result of enhanced DOM photodegradation. Visible light played a more important role in reducing the molecular weight and aromaticity of the DOM than in reducing the content of dissolved organic carbon (DOC) via photoremineralization while the reverse was true for UV radiation, indicating that photochemical reduction of the binding affinity may occur in natural waters at depths greater than UV radiation can reach. A decrease of the affinity of DOM for binding BaP will increase the free dissolved fraction of BaP and thus its availability and toxicity to aquatic organisms. The results from this study may have similar implications for organic pollutants other than BaP.

Introduction

Dissolved organic matter (DOM) in natural waters can bind various organic pollutants delivered into aquatic environments (e.g., McCarthy and Jimenez, 1985, Chiou et al., 1986, Kulovaara et al., 1992, Vinken et al., 2005, Tremblay et al., 2005). This binding affects the transport and fate of the pollutants, and hence their bioavailability and toxicity (Kukkonen et al., 1990, Kukkonen and Oikari, 1991). The binding affinity, usually expressed as a partition or binding coefficient, Koc, is controlled by the physicochemical properties of the DOM (e.g., molecular size, aromaticity, polarity, alkyl moieties) (Chin et al., 1997, Gunasekara and Xing, 2003, Tanaka et al., 2005), the chemical characteristics of the pollutant of interest (e.g., hydrophobicity), and some water chemistry variables (e.g., pH, ionic strength, water hardness) (Schlautman and Morgan, 1993, Penttinen et al., 1998). Therefore, naturally occurring processes that significantly modify the properties of DOM and water chemistry can have a profound impact on the affinity of DOM for binding organic pollutants and thereby on their environmental and ecological ramifications.

Photodegradation is one of the most important processes occurring in natural waters that chemically modify DOM. For example, photodegradation reduces DOM’s average molecular size (Fukushima et al., 2001) and aromaticity (Vähätalo et al., 1999), alters its hydrophobicity (Kulovaara et al., 1996), and lowers pH (Gao and Zepp, 1998, Xie et al., 2004). A reduction in molecular size and aromaticity usually decreases Koc while changes in pH or hydrophobicity either increase or decrease Koc, depending on the chemical characteristics of the pollutants (Kukkonen, 1995).

The nature and extent of DOM photoprocessing are affected by various environmental factors, such as O2 levels, the concentration and speciation of some metal ions (e.g., Fe and Cu) (Gao and Zepp, 1998, Voelker et al., 2000), and the intensity and wavelength of incident light. Raising O2 levels accelerates the rate of photodegradation and increases the O/C atomic ratio of photoprocessed DOM (Schmitt-Kopplin et al., 1998). DOM photodegradation is also strongly wavelength dependent, with ultraviolet (UV) radiation usually being more efficient than visible light (Gao and Zepp, 1998, Vähätalo et al., 2000). Therefore, these environmental factors can exert significant influences on DOM’s organic binding properties.

To the best of our knowledge, this is the first study to investigate the impact of the photodegradation of DOM on its affinity for binding organic pollutants. We tested one model compound, benzo(a)pyrene (BaP), using a natural DOM sample and aquatic and soil humic substances obtained from different geographic regions. BaP represents an environmentally important class of pollutants, i.e., polycyclic aromatic hydrocarbons. We also examined the effects of O2 abundance and the wavelength of incident light on the photoalteration of Koc. The environmental and ecological implications of the photochemically induced changes of Koc are discussed.

Section snippets

DOM samples

Suwannee River humic acid (SRHA, Cat. No. 2S101H) and fulvic acid (SRFA, Cat. No. 1R101F) were purchased from the International Humic Substances Society (IHSS). Isolation procedures and characterization of these materials are reported at the IHSS website (www.ihss.gatec.edu). The C:H:O:N atomic ratios reported by IHSS are 1:0.98:0.60:0.019 for SRHA and 1:0.99:0.62:0.012 for SRFA. Humic acid extracted from a forest soil (Ah, Dystric Cambisol, pH 4.5) in Steigerwald, Germany, was provided by Dr.

pH-series irradiation

The pH-dependence of Koc for unirradiated samples is shown in Table 1. The Koc for SRFA and SFW decreased monotonically with increasing pH, with the value at pH 8.0 being ca. half of that at pH 4.1. The Koc for SRHA and FSHA also decreased with rising pH, but showed a noticeable peak at pH 6.0, which was similar to the findings by De Paolis and Kukkonen (1997). The occurrence of these peaks might be due to a dramatic change in the surfactant properties of the humic acids around pH 6, as

Conclusion

A reduction in the BaP binding affinity due to photodegradation of DOM would increase the free dissolved fraction of this compound in aquatic environments. As free dissolved organic pollutants are usually more bioavailable than their counterparts bound to DOM (Kukkonen, 1995), photodegradation of DOM is expected to increase the bioaccumulation of BaP and hence its toxicity to aquatic organisms. The overall effect might be that biota may be exposed to a higher level of the free dissolved form of

Acknowledgements

We thank R. Ji for providing the soil humic acid, M. Gosselin and S. Demers for the use of the liquid scintillation counter, and M. Simard for assistance in the analysis of DOC samples. This work was supported by grants awarded to H.X. by the Natural Sciences and Engineering Research Council of Canada (NSERC) and the Canada Foundation of Innovation. This is a contribution to the research programs of Institut des sciences de la mer de Rimouski, Université du Québec à Rimouski.

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