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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MDPI AG
2021-11-01
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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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issn | 2073-4395 |
language | English |
last_indexed | 2024-03-10T05:47:33Z |
publishDate | 2021-11-01 |
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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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