Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution

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 su...

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Published in:Global Biogeochemical Cycles
Main Authors: Olson, C., Jiskra, M., Biester, H., Chow, J., Obrist, D.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1539722
https://www.osti.gov/biblio/1539722
https://doi.org/10.1029/2017gb005840
id ftosti:oai:osti.gov:1539722
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spelling ftosti:oai:osti.gov:1539722 2023-07-30T04:01:18+02:00 Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution Olson, C. Jiskra, M. Biester, H. Chow, J. Obrist, D. 2023-06-29 application/pdf http://www.osti.gov/servlets/purl/1539722 https://www.osti.gov/biblio/1539722 https://doi.org/10.1029/2017gb005840 unknown http://www.osti.gov/servlets/purl/1539722 https://www.osti.gov/biblio/1539722 https://doi.org/10.1029/2017gb005840 doi:10.1029/2017gb005840 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1029/2017gb005840 2023-07-11T09:34:54Z 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%). 14 C 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. Other/Unknown Material Arctic Arctic Ocean Tundra Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Arctic Ocean Global Biogeochemical Cycles 32 7 1058 1073
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Olson, C.
Jiskra, M.
Biester, H.
Chow, J.
Obrist, D.
Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
topic_facet 54 ENVIRONMENTAL SCIENCES
description 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%). 14 C 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.
author Olson, C.
Jiskra, M.
Biester, H.
Chow, J.
Obrist, D.
author_facet Olson, C.
Jiskra, M.
Biester, H.
Chow, J.
Obrist, D.
author_sort Olson, C.
title Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
title_short Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
title_full Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
title_fullStr Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
title_full_unstemmed Mercury in Active-Layer Tundra Soils of Alaska: Concentrations, Pools, Origins, and Spatial Distribution
title_sort mercury in active-layer tundra soils of alaska: concentrations, pools, origins, and spatial distribution
publishDate 2023
url http://www.osti.gov/servlets/purl/1539722
https://www.osti.gov/biblio/1539722
https://doi.org/10.1029/2017gb005840
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Tundra
Alaska
genre_facet Arctic
Arctic Ocean
Tundra
Alaska
op_relation http://www.osti.gov/servlets/purl/1539722
https://www.osti.gov/biblio/1539722
https://doi.org/10.1029/2017gb005840
doi:10.1029/2017gb005840
op_doi https://doi.org/10.1029/2017gb005840
container_title Global Biogeochemical Cycles
container_volume 32
container_issue 7
container_start_page 1058
op_container_end_page 1073
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