Deposition History of Polychlorinated Biphenyls to the Lomonosovfonna Glacier, Svalbard: A 209 Congener Analysis
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文摘
A 37 m deep ice core representing 1957鈥?009 and snow from 2009 to 2010 were collected on the Lomonosovfonna glacier, Svalbard (78.82掳 N; 17.43掳 E) and analyzed for 209 polychlorinated biphenyl (PCB) congeners using high-resolution mass spectrometry. Congener profiles in all samples showed the prevalence of tetra- and pentachlorobiphenyls, dominated in all samples by PCB-44, PCB-52, PCB-70 + PCB-74, PCB-87 + PCB-97, PCB-95, PCB-99, PCB-101, and PCB-110. The 鈭慞CB flux varied over time, but the peak flux, 19 pg cm鈥? year鈥? from 1957 to 1966, recurred in 1974鈥?983, 1998鈥?009, and 2009鈥?010. The minimum was 5.75 pg cm鈥? year鈥? in 1989鈥?998, following a 15 year decline. Peak 鈭慞CB fluxes here are lower than measured in the Canadian Arctic. The analysis of all 209 congeners revealed that PCB-11 (3,3鈥?dichlorobiphenyl) was present in all samples, representing 0.9鈥?.5% of 鈭慞CB. PCB-11 was not produced in a commercial PCB product, and its source to the Arctic has not been well-characterized; however, our results confirm that the sources to Lomonosovfonna have been active since 1957. The higher fluxes of 鈭慞CB correspond to periods when average 5 day air mass back trajectories have a frequency of 8鈥?0% and reach 60掳 N or beyond over northern Europe and western Russia or the North Sea into the U.K.

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