Articles | Volume 17, issue 12
https://doi.org/10.5194/bg-17-3083-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3083-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A revised pan-Arctic permafrost soil Hg pool based on Western Siberian peat Hg and carbon observations
Artem G. Lim
BIO-GEO-CLIM Laboratory, Tomsk State University, Tomsk, Russia
Martin Jiskra
University of Basel, Environmental Geosciences, Bernoullistrasse 30, 4056 Basel, Switzerland
Jeroen E. Sonke
Geosciences and Environment Toulouse, UMR 5563 CNRS, 14 Avenue Edouard Belin, 31400 Toulouse, France
Sergey V. Loiko
BIO-GEO-CLIM Laboratory, Tomsk State University, Tomsk, Russia
Natalia Kosykh
Lab Biogeocenol, Institute of Soil Science and Agrochemistry, Russian Academy of Sciences, Siberian Branch, Novosibirsk, Russia
Oleg S. Pokrovsky
CORRESPONDING AUTHOR
Geosciences and Environment Toulouse, UMR 5563 CNRS, 14 Avenue Edouard Belin, 31400 Toulouse, France
N. Laverov Federal Center for Integrated Arctic Research, Russian Academy of Sciences, Arkhangelsk, Russia
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Latest update: 01 Nov 2024
Short summary
To better understand the mercury (Hg) content in northern soils, we measured Hg concentration in peat cores across a 1700 km permafrost gradient in Siberia. We demonstrated a northward increase in Hg concentration in peat and Hg pools in frozen peatlands. We revised the 0–30 cm northern soil Hg pool to be 72 Gg, which is 7 % of the global soil Hg pool of 1086 Gg. The results are important for understanding Hg exchange between soil, water, and the atmosphere under climate change in the Arctic.
To better understand the mercury (Hg) content in northern soils, we measured Hg concentration in...
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