globalchange  > 气候变化事实与影响
DOI: 10.1002/2015GB005323
Scopus记录号: 2-s2.0-84991396226
论文题名:
Mercury isotope compositions across North American forests
作者: Zheng W; , Obrist D; , Weis D; , Bergquist B; A
刊名: Global Biogeochemical Cycles
ISSN: 8866236
出版年: 2016
卷: 30, 期:10
起始页码: 1475
结束页码: 1492
语种: 英语
英文关键词: atmosphere ; biogeochemical cycle ; forest ecosystems ; mercury ; soils ; stable isotopes
Scopus关键词: atmospheric deposition ; biogeochemical cycle ; biomass ; enrichment ; forest ecosystem ; forest soil ; isotopic composition ; litterfall ; mercury (element) ; spatial distribution ; stable isotope ; United States
英文摘要: Forest biomass and soils represent some of the largest reservoirs of actively cycling mercury (Hg) on Earth, but many uncertainties exist regarding the source and fate of Hg in forest ecosystems. We systematically characterized stable isotope compositions of Hg in foliage, litter, and mineral soil horizons across 10 forest sites in the contiguous United States. The mass-independent isotope signatures in all forest depth profiles are more consistent with those of atmospheric Hg(0) than those of atmospheric Hg(II), indicating that atmospheric Hg(0) is the larger source of Hg to forest ecosystems. Within litter horizons, we observed significant enrichment in Hg concentration and heavier isotopes along the depth, which we hypothesize to result from additional deposition of atmospheric Hg(0) during litter decomposition. Furthermore, Hg isotope signatures in mineral soils closely resemble those of the overlying litter horizons suggesting incorporation of Hg from litter as a key source of soil Hg. The spatial distribution of Hg isotope compositions in mineral soils across all sites is modeled by isotopic mixing assuming atmospheric Hg(II), atmospheric Hg(0), and geogenic Hg as major sources. This model shows that northern sites with higher precipitation tend to have higher atmospheric Hg(0) deposition than other sites, whereas drier sites in the western U.S. tend to have higher atmospheric Hg(II) deposition than the rest. We attribute these differences primarily to the higher litterfall Hg input at northern wetter sites due to increased plant productivity by precipitation. These results allow for a better understanding of Hg cycling across the atmosphere-forest-soil interface. �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/77812
Appears in Collections:气候变化事实与影响

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作者单位: Department of Earth Sciences, University of Toronto, Toronto, ON, Canada; School of Earth and Space Exploration, Arizona State University, Tempe, AZ, United States; Divison of Atmospheric Sciences, Desert Research Institute, Reno, NV, United States; Pacific Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC, Canada

Recommended Citation:
Zheng W,, Obrist D,, Weis D,et al. Mercury isotope compositions across North American forests[J]. Global Biogeochemical Cycles,2016-01-01,30(10)
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