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Royal Society of Chemistry, Environmental Science: Processes & Impacts, 9(24), p. 1443-1459, 2022

DOI: 10.1039/d1em00547b

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Organic carbon, and major and trace elements reside in labile low-molecular form in the ground ice of permafrost peatlands: a case study of colloids in peat ice of Western Siberia

Journal article published in 2022 by Artem G. Lim, Sergey V. Loiko ORCID, Daria M. Kuzmina, Ivan V. Krickov, Liudmila S. Shirokova, Sergey P. Kulizhsky, Oleg S. Pokrovsky ORCID
This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

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Abstract

The low molecular weight fraction of peat porewater is enriched in DOC, anions, oxyanions, alkalis and some trace metals. An increase in the active layer depth can liberate a large amount of labile metals and nutrients from the peat.