Articles | Volume 13, issue 6
https://doi.org/10.5194/bg-13-1877-2016
https://doi.org/10.5194/bg-13-1877-2016
Research article
 | 
30 Mar 2016
Research article |  | 30 Mar 2016

Trace element transport in western Siberian rivers across a permafrost gradient

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

Viewed

Total article views: 3,140 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,534 1,518 88 3,140 479 89 115
  • HTML: 1,534
  • PDF: 1,518
  • XML: 88
  • Total: 3,140
  • Supplement: 479
  • BibTeX: 89
  • EndNote: 115
Views and downloads (calculated since 10 Nov 2015)
Cumulative views and downloads (calculated since 10 Nov 2015)

Cited

Saved (preprint)

Latest update: 18 Apr 2024
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.
Altmetrics
Final-revised paper
Preprint