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

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

Mobilization of dissolved organic carbon (DOC) and related trace elements (TEs) from the frozen peat to surface waters in the permafrost zone is expected to enhance under ongoing permafrost thaw and active layer thickness (ALT) deepening in high-latitude regions. The interstitial soil solutions a...

Full description

Bibliographic Details
Main Authors: T. V. Raudina, S. V. Loiko, A. G. Lim, I. V. Krickov, L. S. Shirokova, G. I. Istigechev, D. M. Kuzmina, S. P. Kulizhsky, S. N. Vorobyev, O. S. Pokrovsky
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/14/3561/2017/bg-14-3561-2017.pdf

Internet

https://www.biogeosciences.net/14/3561/2017/bg-14-3561-2017.pdf

Similar Items