Articles | Volume 17, issue 12
Biogeosciences, 17, 3083–3097, 2020
https://doi.org/10.5194/bg-17-3083-2020
Biogeosciences, 17, 3083–3097, 2020
https://doi.org/10.5194/bg-17-3083-2020

Research article 18 Jun 2020

Research article | 18 Jun 2020

A revised pan-Arctic permafrost soil Hg pool based on Western Siberian peat Hg and carbon observations

Artem G. Lim et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (17 Apr 2020) by Andreas Richter
AR by O.S. Pokrovsky on behalf of the Authors (29 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (11 May 2020) by Andreas Richter
RR by Anonymous Referee #2 (15 May 2020)
ED: Publish as is (19 May 2020) by Andreas Richter
Download
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.
Altmetrics
Final-revised paper
Preprint