Journal
ENVIRONMENTAL POLLUTION
Volume 229, Issue -, Pages 627-638Publisher
ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2017.06.090
Keywords
Sediment resuspension; Remobilization; Polycyclic aromatic hydrocarbons; Fluorescent dissolved organic matter; Sediment-water partition
Categories
Funding
- CNRS MISTRALS MERMEX-WP3-C3A research program
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Polycyclic aromatic hydrocarbons (PAHs) and organic matter contents were measured in seawater during resuspension experiments using sediments collected from Toulon Bay (Northwestern Mediterranean Sea, France). The studied sediments were very highly contaminated in PAHs, especially in 4-ring compounds emitted from combustion processes. The sediments used for resuspension experiments were collected at 0-2 cm (diagenetically new organic matter, OM) and 30-32 cm depths (diagenetically transformed OM). They were both mostly composed of fine particles (<63 mu m), enriched in organic carbon (8.2 and 6.3%, respectively) and in PAHs (concentration of Sigma 34 PAHs: 38.2 and 35.7 x 10(3) ng g(-1), respectively). The resuspension of these sediments led to an increase in concentrations of dissolved 234 PAHs, dissolved organic carbon (DOC) and dissolved humic- and tryptophan-like fluorophores in seawater up to 10-, 1.3-, 4.4- and 5.7-fold, respectively. The remobilization in seawater was higher for 4-6 ring PAHs, especially benzo(g,h,i)perylene, whose concentration exceeded the threshold values of the European Water Framework Directive. This noted the potential harmful effects of sediment resuspension on marine biota. From these sediment resuspension experiments, we determined OC-normalized partition coefficients of PAHs between sediment and water (K-oc) and found that during such events, the transfer of PAHs from sediment particles to seawater was lower than that predicted from octanol-water partition coefficients (K-ow) (i.e., measured K-oc > K-oc predicted from K-ow). The results confirmed the sequestration role of sedimentary OC quality and grain size on PAHs; the OM diagenetic state seemed to impact the partition process but in a relatively minor way. Furthermore, differences were observed between 2-4 ring and 5-6 ring PAHs, with the latter displaying a relatively higher mobility towards seawater. These differences may be explained by the distribution of these two PAH pools within different OM moieties, such as humic substances and black carbon. (C) 2017 Elsevier Ltd. All rights reserved.
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