4.7 Article

Colloidal organic carbon and trace elements in peat porewaters across a permafrost gradient in Western Siberia

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Summary: The study found that dissolved organic carbon (DOC), alkali and alkaline-earth metals, sulfate, phosphorus, and other substances were significantly more concentrated in peat ice compared to peat porewaters from the active layer. During full freezing of the soil column in winter, there was a local maximum of enrichment in certain substances located 30-50 cm below the active layer. This research highlights the importance of assessing the consequences of permafrost thaw on surface aquatic systems.

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