Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...

The formation of significant amounts of low molecular weight (LMW) water-soluble organic compounds, which are highly reactive compounds of a non-specific nature, is a feature of the biogeocenoses of the North. Soil acidity, which in turn depends on LMW organic acids content, regulates the migration...

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Main Authors: Raudina, Tatiana V., Istigechev, Georgyi I., Loiko, Sergey V.
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.7878897
https://zenodo.org/record/7878897
id ftdatacite:10.5281/zenodo.7878897
record_format openpolar
spelling ftdatacite:10.5281/zenodo.7878897 2023-06-11T04:17:14+02:00 Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ... Raudina, Tatiana V. Istigechev, Georgyi I. Loiko, Sergey V. 2023 https://dx.doi.org/10.5281/zenodo.7878897 https://zenodo.org/record/7878897 en eng Zenodo https://zenodo.org/communities/actasibirica https://dx.doi.org/10.5281/zenodo.7878896 https://zenodo.org/communities/actasibirica Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess Soil acidity, zonal patterns, Histosols, soil waters, frozen mound and polygonal bogs, Western Siberia Lowland article-journal JournalArticle ScholarlyArticle 2023 ftdatacite https://doi.org/10.5281/zenodo.787889710.5281/zenodo.7878896 2023-05-02T11:11:08Z The formation of significant amounts of low molecular weight (LMW) water-soluble organic compounds, which are highly reactive compounds of a non-specific nature, is a feature of the biogeocenoses of the North. Soil acidity, which in turn depends on LMW organic acids content, regulates the migration ability of compounds in landscapes and the bioavailability of nutrients. With an increase in the active layer thickness of peat soils in Western Siberia in the course of climate warming, new portions of LMW water-soluble organic compounds will enter, which will be quickly processed by microorganisms into CH 4 and CO 2 . Five key sites were considered, located within thawed oligotrophic, frozen mound and polygonal bogs. The analysis of zonal patterns of acidity changes in the waters of peat soils indicates an increase in the pH in the series: northern taiga<forest tundra<southern tundra. A feature of the most acidic soils of the northern taiga is the high content of low molecular weight organic acids, the ... : This work was supported by the Russian Science Foundation (project number 21-77-00021). ... Article in Journal/Newspaper taiga Tundra Siberia DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Soil acidity, zonal patterns, Histosols, soil waters, frozen mound and polygonal bogs, Western Siberia Lowland
spellingShingle Soil acidity, zonal patterns, Histosols, soil waters, frozen mound and polygonal bogs, Western Siberia Lowland
Raudina, Tatiana V.
Istigechev, Georgyi I.
Loiko, Sergey V.
Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
topic_facet Soil acidity, zonal patterns, Histosols, soil waters, frozen mound and polygonal bogs, Western Siberia Lowland
description The formation of significant amounts of low molecular weight (LMW) water-soluble organic compounds, which are highly reactive compounds of a non-specific nature, is a feature of the biogeocenoses of the North. Soil acidity, which in turn depends on LMW organic acids content, regulates the migration ability of compounds in landscapes and the bioavailability of nutrients. With an increase in the active layer thickness of peat soils in Western Siberia in the course of climate warming, new portions of LMW water-soluble organic compounds will enter, which will be quickly processed by microorganisms into CH 4 and CO 2 . Five key sites were considered, located within thawed oligotrophic, frozen mound and polygonal bogs. The analysis of zonal patterns of acidity changes in the waters of peat soils indicates an increase in the pH in the series: northern taiga<forest tundra<southern tundra. A feature of the most acidic soils of the northern taiga is the high content of low molecular weight organic acids, the ... : This work was supported by the Russian Science Foundation (project number 21-77-00021). ...
format Article in Journal/Newspaper
author Raudina, Tatiana V.
Istigechev, Georgyi I.
Loiko, Sergey V.
author_facet Raudina, Tatiana V.
Istigechev, Georgyi I.
Loiko, Sergey V.
author_sort Raudina, Tatiana V.
title Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
title_short Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
title_full Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
title_fullStr Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
title_full_unstemmed Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia ...
title_sort spatial heterogeneity of soil acidity properties in peatlands of western siberia ...
publisher Zenodo
publishDate 2023
url https://dx.doi.org/10.5281/zenodo.7878897
https://zenodo.org/record/7878897
genre taiga
Tundra
Siberia
genre_facet taiga
Tundra
Siberia
op_relation https://zenodo.org/communities/actasibirica
https://dx.doi.org/10.5281/zenodo.7878896
https://zenodo.org/communities/actasibirica
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.787889710.5281/zenodo.7878896
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