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DOI | 10.1029/2017GB005840 |
Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution | |
Olson C.; Jiskra M.; Biester H.; Chow J.; Obrist D. | |
发表日期 | 2018 |
ISSN | 0886-6236 |
EISSN | 1944-9224 |
起始页码 | 1058 |
结束页码 | 1073 |
卷号 | 32期号:7 |
英文摘要 | Tundra soils serve as major sources of mercury (Hg) input to the Arctic Ocean via river runoff and coastal erosion; yet little information is available on tundra soil Hg concentrations, pool sizes, origins, and dynamics. We present a detailed investigation of Hg in the active layer (upper ~100 cm subject to seasonal thaw) of tundra soils across 11 sites in Alaska. Soil Hg concentrations in organic horizons (151 ± 7 μg/kg) were in the upper range of temperate soil organic horizons, and concentrations in mineral horizons (98 ± 6 μg/kg) were much higher than in temperate soils. Soil Hg concentrations declined from inland to coastal sites, in contrast to a hypothesized northward increase expected because of proximity to coastal atmospheric mercury depletion events. Principle component analyses and elemental ratios results show that exogenic sources dominated over geogenic sources—in A-horizons (66 ± 4%) and mineral B-horizons (51 ± 1%). 14C age-dating suggested recent origins of Hg in surface soils but showed that mineral soils (more than 7,300 years old) must have accumulated atmospheric inputs across millennia leading to high soil concentrations and pools. We estimated a total Northern Hemisphere active-layer tundra soil Hg pool of 184 Gg (range of 136 to 274 Gg), suggesting a globally important Hg storage pool. Tundra soils are subject to seasonal thaw and freeze dynamics, thereby providing large inputs to rivers, lakes, and the Arctic Ocean. Understanding processes that mobilize Hg from tundra soils will be critical to understanding future Arctic wildlife and human Hg exposures. ©2018. American Geophysical Union. All Rights Reserved. |
英文关键词 | Alaska; Arctic; mercury; pollution; soils; tundra |
语种 | 英语 |
scopus关键词 | active layer; concentration (composition); mercury (element); Northern Hemisphere; pollutant source; soil horizon; soil pollution; spatial distribution; temperate environment; tundra soil; Alaska; Arctic; Arctic Ocean; United States |
来源期刊 | Global Biogeochemical Cycles |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129810 |
作者单位 | Desert Research Institute, Reno, NV, United States; Geosciences Environment Toulouse, CNRS, Toulouse, France; Environmental Geochemistry, Technische Universität Braunschweig, Braunschweig, Germany; Department of Environmental, Earth and Atmospheric Sciences, University of Massachusetts, Lowell, MA, United States |
推荐引用方式 GB/T 7714 | Olson C.,Jiskra M.,Biester H.,et al. Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution[J],2018,32(7). |
APA | Olson C.,Jiskra M.,Biester H.,Chow J.,&Obrist D..(2018).Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution.Global Biogeochemical Cycles,32(7). |
MLA | Olson C.,et al."Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution".Global Biogeochemical Cycles 32.7(2018). |
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