Temporal trends of perfluoroalkyl compounds with isomer analysis in lake trout from Lake Ontario (1979-2004)

被引:69
作者
Furdui, Vasile I. [1 ,2 ,4 ]
Helm, Paul A. [2 ]
Crozier, Patrick W. [2 ]
Lucaciu, Corina [2 ]
Reiner, Eric J. [2 ]
Marvin, Chris H. [3 ]
Whittle, D. Michael [1 ,4 ]
Mabury, Scott A. [1 ,4 ]
Tomy, Gregg T. [5 ]
机构
[1] Univ Toronto, Dept Chem, Toronto, ON M5S 3H6, Canada
[2] Ontario Minist Environm, Toronto, ON M9P 3V6, Canada
[3] Environm Canada, Burlington, ON L7R 4A6, Canada
[4] Fisheries & Oceans Canada, Burlington, ON L7R 4A6, Canada
[5] Fisheries & Oceans Canada, Winnipeg, MB R3T 2N6, Canada
关键词
D O I
10.1021/es7032372
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The temporal trends of perfluoroalkyl compounds (PFCs), including C7-C15 perfluorocarboxylates (PFCAs), perfluorosulfonates (PFSAs) and heptadecafluorooctane sulfonamide (PFOSA), were determined in lake trout collected between 1979 and 2004 from Lake Ontario. The average concentrations of total PFSAs (+/- standard error of the mean; range) increased from 20 ng g(-1) wet weight (+/- 4; 8-26) in 1979, peaked at 70 ng g(-1) (+/- 7; 58-91) in 1993, and were 46 ng g(-1) (+/- 10; 30-83) in 2004,with perfluorooctane sulfonate (PFOS) as the most abundant PFC. The PFCAs exhibited similar temporal variation, with concentrations increasing from 1.4 ng g(-1) (+/- 0.1; 0.9-1.9) in 1979 to 9.4 ng g(1) (+/- 3.1; 3-17) in 1988, and were 6.8 ng g(-1) (+/- 1.0; 4.5-9.8) in 2004. Individual mean PFCA concentrations varied between 0.2 and 2 ng g(-1) (wet weight). Perfluorodecane sulfonate (PFDS) and PFOSA were the only compounds showing a declining trend in the past decade, after reaching a peak value in 1993. Branched C11 and C13 PFCA isomers were detected in the lake trout and confirmed in Niagara River suspended sediments, with trends in both matrices suggesting that declining emissions or use of products containing these isomers in part account for the observed PFCA trends in the mid-1990s. However, the most recent samples, comprised almost exclusively of linear isomers, indicate that current PFCA sources to Lake Ontario result from the telomerization process of linear telogens.
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页码:4739 / 4744
页数:6
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