論文

査読有り
2014年8月

Levels and distribution of hexabromocyclododecane and its lower brominated derivative in Japanese riverine environment

CHEMOSPHERE
  • Jung Keun Oh
  • ,
  • Kensuke Kotani
  • ,
  • Satoshi Managaki
  • ,
  • Shigeki Masunaga

109
開始ページ
157
終了ページ
163
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1016/j.chemosphere.2014.01.074
出版者・発行元
PERGAMON-ELSEVIER SCIENCE LTD

Hexabromocyclododecane (HBCD) and its lower brominated derivatives were measured in both surface water and sediment samples from three Japanese rivers; Tsurumi River, Yodo River, and Kuzuryu River. The concentration level of Sigma HBCD (sum of alpha-, beta-, and gamma-HBCD) was in the order of Kuzuryu > Yodo > Tsurumi Rivers, reflective of the different emission sources for each basin. The highest Sigma HBCD concentration (7800 ng g(-1)) was detected in the sediment sample from the Kuzuryu River that receives effluents from textile industries, which use HBCD in flame retardant finishes. A different diastereomeric pattern of alpha-, beta-, and gamma-HBCD of each river was investigated, indicating the level of HBCD in these rivers is directly influenced by emission source. Enantiomer fractions of HBCDs in water and sediment samples were also determined. Racemic mixtures were observed in the water samples, whereas enantiomeric enrichment of (-) gamma-HBCD and (+) alpha-HBCD was observed in the sediment samples. Some lower brominated HBCD derivatives such as pentabromocyclododecenes were detected in both the water and sediment samples, and their concentration ranged from below the detection limit to 15 ng L-1 and 20 ng g(-1) dw, respectively. (C) 2014 Elsevier Ltd. All rights reserved.

リンク情報
DOI
https://doi.org/10.1016/j.chemosphere.2014.01.074
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000337881100023&DestApp=WOS_CPL
ID情報
  • DOI : 10.1016/j.chemosphere.2014.01.074
  • ISSN : 0045-6535
  • eISSN : 1879-1298
  • Web of Science ID : WOS:000337881100023

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