globalchange  > 气候变化事实与影响
DOI: 10.1002/2016GB005411
Scopus记录号: 2-s2.0-84988448917
论文题名:
Historical variations of mercury stable isotope ratios in Arctic glacier firn and ice cores
作者: Zdanowicz C; M; , Kr�mmel E; M; , Poulain A; J; , Yumvihoze E; , Chen J; , Štrok M; , Scheer M; , Hintelmann H
刊名: Global Biogeochemical Cycles
ISSN: 8866236
出版年: 2016
卷: 30, 期:9
起始页码: 1324
结束页码: 1347
语种: 英语
英文关键词: air pollution ; Arctic ; ice cores ; isotopes ; mercury ; snow
Scopus关键词: arctic environment ; atmospheric pollution ; concentration (composition) ; glacier dynamics ; historical perspective ; ice core ; isotopic ratio ; mercury (element) ; nineteenth century ; precipitation (climatology) ; snow ; snow accumulation ; stable isotope ; twentieth century ; Arctic Ocean ; Baffin Bay [Arctic Ocean] ; Canada ; Canadian Arctic
英文摘要: The concentration and isotopic composition of mercury (Hg) were determined in glacier core samples from Canadian Arctic ice caps dating from preindustrial to recent time (early 21st century). Mean Hg levels increased from ≤ 0.2 ng L−1 in preindustrial time to ~0.8–1.2 ng L−1 in the modern industrial era (last ~200 years). Hg accumulated on Arctic ice caps has Δ199Hg and Δ201Hg that are higher (~ −1 to 2.9‰) than previously reported for Arctic snow impacted by atmospheric Hg depletion events (mostly < −1‰), suggesting that these events contribute little to Hg accumulation on ice caps. The range of δ202Hg, Δ199Hg, and Δ201Hg in glacier cores overlaps with that of Arctic Hg0 (g) and of seawater in Baffin Bay and also with that of midlatitude precipitation and industrial Hg sources, including coal and Hg ores. A core from Agassiz ice cap (80.7�N) shows a ~ +1‰ shift in δ202Hg over the nineteenth to twentieth centuries that could reflect changes in the isotopic composition of the atmospheric Hg pool in the High Arctic in response to growing industrial emissions at lower latitudes. This study is the first ever to report on historical variations of Hg stable isotope ratios in Arctic ice cores. Results could help constrain future modeling efforts of the global Hg biogeochemical cycle and the atmosphere's response to changing Hg emissions, past and future. �2016. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/77822
Appears in Collections:气候变化事实与影响

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作者单位: Department of Earth Sciences, Uppsala University, Uppsala, Sweden; Inuit Circumpolar Council of Canada, Ottawa, ON, Canada; Department of Biology, University of Ottawa, Ottawa, ON, Canada; State Key Laboratory of Environmental Geochemistry, Chinese Academy of Sciences, Guyiang, China; Jožef Stefan Institute, Ljubljana, Slovenia; Department of Chemistry, Trent University, Peterborough, ON, Canada; Scheer Software Solutions, Barry's Bay, ON, Canada

Recommended Citation:
Zdanowicz C,M,, Kr�mmel E,et al. Historical variations of mercury stable isotope ratios in Arctic glacier firn and ice cores[J]. Global Biogeochemical Cycles,2016-01-01,30(9)
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