Trace element transport in western Siberian rivers across a permafrost gradient

Pokrovsky, Oleg S.; Manasypov, Rinat M.; Loiko, Sergey V.; Krickov, Ivan A.; Kopysov, Sergey G.; Kolesnichenko, Larisa G.; Vorobyev, Sergey N.; Kirpotin, Sergey N.

doi:https://doi.org/10.5194/bg-13-1877-2016

Articles | Volume 13, issue 6

https://doi.org/10.5194/bg-13-1877-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/bg-13-1877-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 13, issue 6

Research article

|

30 Mar 2016

Research article |

| 30 Mar 2016

Trace element transport in western Siberian rivers across a permafrost gradient

Oleg S. Pokrovsky, Rinat M. Manasypov, Sergey V. Loiko, Ivan A. Krickov, Sergey G. Kopysov, Larisa G. Kolesnichenko, Sergey N. Vorobyev, and Sergey N. Kirpotin

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Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC C8372: 'Comment to ms', Anonymous Referee #3, 09 Dec 2015
- AC C9704: 'Response to Reviewer No 3', O.S. Pokrovsky, 12 Feb 2016
RC C9945: 'Detailed evaluation report on « Trace elements transport in western Siberia rivers across a permafrost gradient. » by O.S. Pokrovsky et al.', Anonymous Referee #2, 23 Feb 2016
- AC C9958: 'Reply to Reviewer No 2', O.S. Pokrovsky, 25 Feb 2016

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

AR by O.S. Pokrovsky on behalf of the Authors (16 Mar 2016)

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.