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.

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Cited articles

Abgottspon, F.: Bigalke, M., and Wilcke, W.: Mobilization of trace elements in a carbonatic soil after experimental flooding, Geoderma, 259–260, 156–163, 2015.
Alexeeva, L. B., Strachan, W. M. J., Shluchkova, V. V., Nazarova, A. A., Nikanorov, A. M., Korotova, L. G., and Koreneva, V. I.: Organochlorine pesticide and trace metal monitoring of Russian rivers flowing to the Arctic Ocean: 1990–1996, Mar. Pollut. Bull., 43, 71–85, 2001.
Andersson, P. S., Dahlqvist, R., Ingri, J., and Gustafsson, Ö.: The isotopic composition of Nd in a boreal river: A reflection of selective weathering and colloidal transport, Geochim. Cosmochim. Ac., 65, 521–527, 2001.
Anisimova, N. P.: Cryohydrochemical Features of Permafrost Zone. (Kriogidrokhimicheskie osobennosti merzloi zony), Nauka, 1981 (in Russian).
Antcibor, I., Eschenbach, A., Zubrzycki, S., Kutzbach, L., Bolshiyanov, D., and Pfeiffer, E.-M.: Trace metal distribution in pristine permafrost-affected soils of the Lena River delta and its hinterland, northern Siberia, Russia, Biogeosciences, 11, 1–15,, 2014.
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