Articles | Volume 13, issue 6
Biogeosciences, 13, 1877–1900, 2016
Biogeosciences, 13, 1877–1900, 2016

Research article 30 Mar 2016

Research article | 30 Mar 2016

Trace element transport in western Siberian rivers across a permafrost gradient

Oleg S. Pokrovsky et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (25 Feb 2016) by Manmohan Sarin
AR by O.S. Pokrovsky on behalf of the Authors (11 Mar 2016)  Author's response    Manuscript
ED: Publish as is (16 Mar 2016) by Manmohan Sarin
Short summary
Climate change in western Siberia and permafrost boundary migration will essentially affect the elements controlled by underground water feeding (DIC, alkaline earth elements (Ca, Sr), oxyanions (Mo, Sb, As) and U). The thickening of the active layer may increase the export of trivalent and tetravalent hydrolysates in the form of organo-ferric colloids.
Final-revised paper