Organic matter structure and composition of permafrost peatlands in the European North-East

The paper deals with structure of permafrost peatlands from the southern part of the Bolshezemelskaya Tundra region. The soil-geocryological complex of peatlands was found for three constituents in its structure as ’active layer – upper permafrost – lower permafrost’. Profile distribution and compos...

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Bibliographic Details
Main Authors: D. A. Kaverin, E. M. Lapteva, A. V. Pastukhov
Format: Dataset
Language:Russian
Published: Theoretical and Applied Ecology 2015
Subjects:
Online Access:https://dx.doi.org/10.25750/1995-4301-2015-1-013-020
http://envjournal.ru/ari/v2015/v1/files/15103.pdf
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Summary:The paper deals with structure of permafrost peatlands from the southern part of the Bolshezemelskaya Tundra region. The soil-geocryological complex of peatlands was found for three constituents in its structure as ’active layer – upper permafrost – lower permafrost’. Profile distribution and composition of some soil organic matter components at peatlands was studied. The humus state parameters which are accessed on base of fraction-group humus composition data are good markers of formation conditions of active layers and permafrost rocks in soils of peatlands from the south- eastern part of the Bolshezemelskaya Tundra region. The most indicative among them are: carbon content of water-soluble organic compounds, humic to fulvic acids ratio,ratio of fractions in composition of humic acids. Zero vegetation cover on peat circles corresponds with low content of easy-mineralizable organic compounds in soil which provide plants with nitrogen and nutrients.