Spring Melt and the Redistribution of Organochlorine Pesticides in the Sea-Ice Environment: A Comparative Study between Arctic and Antarctic Regions

被引:49
作者
Bigot, Marie [1 ]
Hawker, Darryl W. [2 ]
Cropp, Roger [2 ]
Muir, Derek C. G. [3 ]
Jensen, Bjarne [4 ]
Bossi, Rossana [4 ]
Nash, Susan M. Bengtson [1 ]
机构
[1] Griffith Univ, Environm Futures Res Inst, 170 Kessels Rd, Nathan, Qld 4111, Australia
[2] Griffith Univ, Griffith Sch Environm, 170 Kessels Rd, Nathan, Qld 4111, Australia
[3] Environm & Climate Change Canada, Aquat Contaminants Res Div, 867 Lakeshore Rd, Burlington, ON L7S 1A1, Canada
[4] Aarhus Univ, Arctic Res Ctr, Dept Environm Sci, Frederiksborgvej 399, DK-4000 Roskilde, Denmark
基金
澳大利亚研究理事会;
关键词
PERSISTENT ORGANIC POLLUTANTS; HEMISPHERE HUMPBACK WHALES; LONG-RANGE TRANSPORT; SOUTHERN-OCEAN; TEMPORAL TRENDS; ALPHA-HCH; WATER; HEXACHLOROCYCLOHEXANES; ATMOSPHERE; POPS;
D O I
10.1021/acs.est.7b02481
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Complementary sampling of air, snow, sea-ice, and seawater for a range of organochlorine pesticides (OCPs) was undertaken through the early stages of respective spring sea-ice melting at coastal sites in northeast Greenland and eastern Antarctica to investigate OCP concentrations and redistribution during this time. Mean concentrations in seawater, sea-ice and snow were generally greater at the Arctic site. For example, alpha-HCH was found to have the largest concentrations of all analytes in Arctic seawater and sea-ice meltwater samples (224-253 and 34.7-48.2 pg center dot L-1 respectively compared to 1.0-1.3 and <0.63 pg center dot L-1 respectively for Antarctic samples). Differences in atmospheric samples were generally not as pronounced however. Findings suggest that sea-ice OCP burdens originate from both snow and seawater. The distribution profile between seawater and sea-ice showed a compound-dependency for Arctic samples not evident with those from the Antarctic, possibly due to full submersion of sea-ice at the former. Seasonal sea-ice melt processes may alter the exchange rates of selected OCPs between air and seawater, but are not expected to reverse their direction, which fugacity modeling indicates is volatilisation in the Arctic and net deposition in the Antarctic. These predictions are consistent with the limited current observations.
引用
收藏
页码:8944 / 8952
页数:9
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