Articles | Volume 14, issue 14
https://doi.org/10.5194/bg-14-3561-2017
https://doi.org/10.5194/bg-14-3561-2017
Research article
 | 
27 Jul 2017
Research article |  | 27 Jul 2017

Dissolved organic carbon and major and trace elements in peat porewater of sporadic, discontinuous, and continuous permafrost zones of western Siberia

Tatiana V. Raudina, Sergey V. Loiko, Artyom G. Lim, Ivan V. Krickov, Liudmila S. Shirokova, Georgy I. Istigechev, Daria M. Kuzmina, Sergey P. Kulizhsky, Sergey N. Vorobyev, and Oleg S. Pokrovsky

Viewed

Total article views: 3,548 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,902 1,502 144 3,548 479 88 130
  • HTML: 1,902
  • PDF: 1,502
  • XML: 144
  • Total: 3,548
  • Supplement: 479
  • BibTeX: 88
  • EndNote: 130
Views and downloads (calculated since 02 Feb 2017)
Cumulative views and downloads (calculated since 02 Feb 2017)

Viewed (geographical distribution)

Total article views: 3,548 (including HTML, PDF, and XML) Thereof 3,403 with geography defined and 145 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Short summary
We collected peat porewaters across a 640 km latitudinal transect of sporadic to continuous permafrost zone and analyzed organic carbon and trace metals. There was no distinct decrease in concentration along the latitudinal transect from 62.2° N to 67.4° N. The northward migration of the permafrost boundary or the change of hydrological regime is unlikely to modify chemical composition of peat porewater fluids larger than their natural variation within different micro-landscapes.
Altmetrics
Final-revised paper
Preprint