4.8 Article

Occurrence and partitioning of polyhalogenated carbazoles in seawater and sediment from East China Sea

Journal

WATER RESEARCH
Volume 190, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.watres.2020.116717

Keywords

Carbazole; PHCZs; Seawater; Sediment; Partitioning

Funding

  1. National Natural Science Foundation of China [21806139, U20A20134]
  2. Natural Science Foundation of Zhejiang Province [YQ 202043985]

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This study investigated the occurrence and spatial distribution of carbazole and polyhalogenated carbazoles in seawater and sediment samples from the East China Sea. The results showed that carbazole and various polyhalogenated carbazoles were detected in both seawater and sediment samples, with different concentrations and detection frequencies. These findings provide insights into the environmental behaviors of these compounds in marine environments.
Polyhalogenated carbazoles (PHCZs) have received great concern due to their environmental persistence and potential dioxin-like toxicities. Their presence in the marine sediment had been well characterized, but limited studies had investigated their environmental behaviors in the marine environment. In this study, we collected paired seawater (n = 48) and surface sediment samples (n = 48) from East China Sea and analyzed for carbazole (CZ) and 11 PHCZs to investigate the occurrence and spatial distribution of CZ and PHCZs in seawater and sediment, as well as to explore the partitioning behaviors of CZ and PHCZs between seawater and sediment. In seawater samples, CZ and nine PHCZs were detected, with the concentrations of Sigma PHCZs ranging from 0.21 to 11 ng/L (mean 2.7 ng/L). CZ (94%), 3-CCZ (89%), 1368-CCZ (65%), and 36-CCZ (57%) had relatively higher detection frequencies. Among PHCZs, 36-CCZ (mean 1.1 ng/L) had the highest mean seawater concentration, followed by 3-CCZ (0.51 ng/L) and 1368-CCZ (0.19 ng/L). In sediment, CZ and 11 PHCZs were detected, with the concentrations of Sigma PHCZs ranged from 0.34 to 2.0 ng/g (mean 1.0 ng/g). CZ, 3-CCZ, 3-BCZ, 36-CCZ, 27-BCZ, and 36-BCZ were measurable in all sediment samples, and 36-CCZ was the predominant PHCZ (0.47 ng/g, 0.025-1.1 ng/g), followed by 1368-BCZ (0.16 ng/g,

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