Black Carbon and Its Effect on Carbon Sequestration in Soil

The properties of black carbon (BC) are described very differently in the literature, even when determined by the same methodological procedure. To clarify this discrepancy, BC was investigated in the clay Cambisols of southern Bohemia, Czech Republic, in groups of soils with lower and higher deposi...

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Main Authors: Marek Kopecký, Ladislav Kolář, Radka Váchalová, Petr Konvalina, Jana Batt, Petr Mráz, Ladislav Menšík, Trong Nghia Hoang, Miroslav Dumbrovský
Format: Article
Language:English
Published: MDPI AG 2021-11-01
Series:Agronomy
Subjects:
Online Access:https://www.mdpi.com/2073-4395/11/11/2261
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author Marek Kopecký
Ladislav Kolář
Radka Váchalová
Petr Konvalina
Jana Batt
Petr Mráz
Ladislav Menšík
Trong Nghia Hoang
Miroslav Dumbrovský
author_facet Marek Kopecký
Ladislav Kolář
Radka Váchalová
Petr Konvalina
Jana Batt
Petr Mráz
Ladislav Menšík
Trong Nghia Hoang
Miroslav Dumbrovský
author_sort Marek Kopecký
collection DOAJ
description The properties of black carbon (BC) are described very differently in the literature, even when determined by the same methodological procedure. To clarify this discrepancy, BC was investigated in the clay Cambisols of southern Bohemia, Czech Republic, in groups of soils with lower and higher deposition of its atmospheric fallout. The BC determination was performed according to a modified method of Kuhlbusch and Crutzen (1995). The amount of the free light fraction, the occluded light fraction of soil organic matter and its ratio, the amount of heavy soil fraction DF, and its soil organic matter DFOM were determined. Other soil characteristics were identified. It was found that there are two very different types of BC in soils. Historical BC from biomass fires, and new, anthropogenic, from the furnace and transport fumes. Historical BC has a significant effect on the organic matter of the heavy soil fraction, on the ratio of the free and occluded soil organic matter fraction, and the number of water-resistant soil aggregates. Anthropogenic BC does not have this effect. Because this form of BC is not significantly stabilized by the colloidal mineral fraction, it is necessary to take general data on BC’s high stability and resistance to mineralization in the soil with circumspection.
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spelling doaj.art-e56dfd3784f24f03a90bce135f802a132023-11-22T22:02:57ZengMDPI AGAgronomy2073-43952021-11-011111226110.3390/agronomy11112261Black Carbon and Its Effect on Carbon Sequestration in SoilMarek Kopecký0Ladislav Kolář1Radka Váchalová2Petr Konvalina3Jana Batt4Petr Mráz5Ladislav Menšík6Trong Nghia Hoang7Miroslav Dumbrovský8Faculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicCrop Research Institute, Division of Crop Management Systems, Drnovska 507-73, 16106 Prague 6, Czech RepublicFaculty of Agriculture, University of South Bohemia in Ceske Budejovice, Studentska 1668, 37005 Ceske Budejovice, Czech RepublicFaculty of Civil Engineering, Brno University of Technology, Zizkova 17, 60200 Brno, Czech RepublicThe properties of black carbon (BC) are described very differently in the literature, even when determined by the same methodological procedure. To clarify this discrepancy, BC was investigated in the clay Cambisols of southern Bohemia, Czech Republic, in groups of soils with lower and higher deposition of its atmospheric fallout. The BC determination was performed according to a modified method of Kuhlbusch and Crutzen (1995). The amount of the free light fraction, the occluded light fraction of soil organic matter and its ratio, the amount of heavy soil fraction DF, and its soil organic matter DFOM were determined. Other soil characteristics were identified. It was found that there are two very different types of BC in soils. Historical BC from biomass fires, and new, anthropogenic, from the furnace and transport fumes. Historical BC has a significant effect on the organic matter of the heavy soil fraction, on the ratio of the free and occluded soil organic matter fraction, and the number of water-resistant soil aggregates. Anthropogenic BC does not have this effect. Because this form of BC is not significantly stabilized by the colloidal mineral fraction, it is necessary to take general data on BC’s high stability and resistance to mineralization in the soil with circumspection.https://www.mdpi.com/2073-4395/11/11/2261anthropogenic black carbondensity fractionationhistorical black carbonwaterproof macro-aggregates
spellingShingle Marek Kopecký
Ladislav Kolář
Radka Váchalová
Petr Konvalina
Jana Batt
Petr Mráz
Ladislav Menšík
Trong Nghia Hoang
Miroslav Dumbrovský
Black Carbon and Its Effect on Carbon Sequestration in Soil
Agronomy
anthropogenic black carbon
density fractionation
historical black carbon
waterproof macro-aggregates
title Black Carbon and Its Effect on Carbon Sequestration in Soil
title_full Black Carbon and Its Effect on Carbon Sequestration in Soil
title_fullStr Black Carbon and Its Effect on Carbon Sequestration in Soil
title_full_unstemmed Black Carbon and Its Effect on Carbon Sequestration in Soil
title_short Black Carbon and Its Effect on Carbon Sequestration in Soil
title_sort black carbon and its effect on carbon sequestration in soil
topic anthropogenic black carbon
density fractionation
historical black carbon
waterproof macro-aggregates
url https://www.mdpi.com/2073-4395/11/11/2261
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