Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments

The soils of cold regions store up to 60% of all organic carbon on the planet. As a result of climate change, this organic matter can be biodegraded by microorganisms and thereby make an additional contribution to carbon balance. Nowadays, there are fragmentary data on organic C stocks in high-latit...

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Published in:Agronomy
Main Authors: Vyacheslav Polyakov, Evgeny Abakumov, Evgeny Lodygin, Roman Vasilevich
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/agronomy13061483
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author Vyacheslav Polyakov
Evgeny Abakumov
Evgeny Lodygin
Roman Vasilevich
author_facet Vyacheslav Polyakov
Evgeny Abakumov
Evgeny Lodygin
Roman Vasilevich
author_sort Vyacheslav Polyakov
collection MDPI Open Access Publishing
container_issue 6
container_start_page 1483
container_title Agronomy
container_volume 13
description The soils of cold regions store up to 60% of all organic carbon on the planet. As a result of climate change, this organic matter can be biodegraded by microorganisms and thereby make an additional contribution to carbon balance. Nowadays, there are fragmentary data on organic C stocks in high-latitude soils and single works on the analysis of the quality of buried organic matter. This paper presents the first data on the molecular weight distributions of humic acids (HAs) extracted from soils and sediments in Yedoma. Molecular weight distributions of HAs preparations were obtained on an AKTAbasic 10 UPS chromatographic system (Amersham Biosciences, Sweden) using a SuperdexTM 200 10/300 GL column (with cross-linked dextran gel, fractionation range for globular proteins 10–600 kDa). As a result of the study, it was found that the buried soil horizons are characterized by the highest content of low molecular weight fraction (with molecular mass (Mr) 1.4–1.9 kDa and molar fraction in the range of 54.3–67.1%). The high molecular weight fraction is concentrated mainly in the superficial horizons and decreases with depth (with Mr 299–346 kDa and molar fraction in the range of 3.4–9.8%). In the Yedoma sediments, the maximum content of the medium-molecular fraction is observed (with Mr 24.6 kDa and 39.6% of the molar fraction), which may indicate a low rate of organic matter transformation in the permafrost. The data obtained serve as a database of analysis in terms of modeling the global carbon cycle in the cold regions of the planet.
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permafrost
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geographic Delta River
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op_doi https://doi.org/10.3390/agronomy13061483
op_relation Soil and Plant Nutrition
https://dx.doi.org/10.3390/agronomy13061483
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spelling ftmdpi:oai:mdpi.com:/2073-4395/13/6/1483/ 2025-01-16T22:58:59+00:00 Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments Vyacheslav Polyakov Evgeny Abakumov Evgeny Lodygin Roman Vasilevich agris 2023-05-28 application/pdf https://doi.org/10.3390/agronomy13061483 EN eng Multidisciplinary Digital Publishing Institute Soil and Plant Nutrition https://dx.doi.org/10.3390/agronomy13061483 https://creativecommons.org/licenses/by/4.0/ Agronomy; Volume 13; Issue 6; Pages: 1483 transformation of SOM buried organic matter permafrost thawing cryosols Fluvisols Lena Delta river Text 2023 ftmdpi https://doi.org/10.3390/agronomy13061483 2023-08-01T10:15:15Z The soils of cold regions store up to 60% of all organic carbon on the planet. As a result of climate change, this organic matter can be biodegraded by microorganisms and thereby make an additional contribution to carbon balance. Nowadays, there are fragmentary data on organic C stocks in high-latitude soils and single works on the analysis of the quality of buried organic matter. This paper presents the first data on the molecular weight distributions of humic acids (HAs) extracted from soils and sediments in Yedoma. Molecular weight distributions of HAs preparations were obtained on an AKTAbasic 10 UPS chromatographic system (Amersham Biosciences, Sweden) using a SuperdexTM 200 10/300 GL column (with cross-linked dextran gel, fractionation range for globular proteins 10–600 kDa). As a result of the study, it was found that the buried soil horizons are characterized by the highest content of low molecular weight fraction (with molecular mass (Mr) 1.4–1.9 kDa and molar fraction in the range of 54.3–67.1%). The high molecular weight fraction is concentrated mainly in the superficial horizons and decreases with depth (with Mr 299–346 kDa and molar fraction in the range of 3.4–9.8%). In the Yedoma sediments, the maximum content of the medium-molecular fraction is observed (with Mr 24.6 kDa and 39.6% of the molar fraction), which may indicate a low rate of organic matter transformation in the permafrost. The data obtained serve as a database of analysis in terms of modeling the global carbon cycle in the cold regions of the planet. Text lena delta permafrost MDPI Open Access Publishing Delta River ENVELOPE(-103.371,-103.371,78.769,78.769) Agronomy 13 6 1483
spellingShingle transformation of SOM
buried organic matter
permafrost thawing
cryosols
Fluvisols Lena Delta river
Vyacheslav Polyakov
Evgeny Abakumov
Evgeny Lodygin
Roman Vasilevich
Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title_full Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title_fullStr Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title_full_unstemmed Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title_short Molecular Weight Distribution of Humic Acids Isolated from Buried Soils and Yedoma Sediments
title_sort molecular weight distribution of humic acids isolated from buried soils and yedoma sediments
topic transformation of SOM
buried organic matter
permafrost thawing
cryosols
Fluvisols Lena Delta river
topic_facet transformation of SOM
buried organic matter
permafrost thawing
cryosols
Fluvisols Lena Delta river
url https://doi.org/10.3390/agronomy13061483