Biochars influence differential distribution and chemical composition of soil organic matter

In the present study, three soils (Ferralsol, Luvisol topsoil, and Luvisol subsoil) were amended with biochars (charcoal, hydrothermal carbonization coal (HTC) of bark, and low-temperature conversion coal of sewage sludge), wheat straw and a control (no amendment) and incubated over a period of 365...

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Main Authors: M.F. Qayyum, D. Steffens, H.P. Reisenauer, S. Schubert
Format: Article
Language:English
Published: Czech Academy of Agricultural Sciences 2014-08-01
Series:Plant, Soil and Environment
Subjects:
Online Access:https://pse.agriculturejournals.cz/artkey/pse-201408-0001_biochars-influence-differential-distribution-and-chemical-composition-of-soil-organic-matter.php
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author M.F. Qayyum
D. Steffens
H.P. Reisenauer
S. Schubert
author_facet M.F. Qayyum
D. Steffens
H.P. Reisenauer
S. Schubert
author_sort M.F. Qayyum
collection DOAJ
description In the present study, three soils (Ferralsol, Luvisol topsoil, and Luvisol subsoil) were amended with biochars (charcoal, hydrothermal carbonization coal (HTC) of bark, and low-temperature conversion coal of sewage sludge), wheat straw and a control (no amendment) and incubated over a period of 365 days. Each amendment was applied at a rate of 11.29 g C/kg soil. After incubation, the soils were analyzed to retrieve three density fractions (free fraction (FF), intra-aggregate fraction (IAF), and heavy fraction) which were analyzed for total carbon (TC) contents and scanned by fourier transform infrared spectroscopy (FTIR). The biochars and straw significantly increased the TC contents of soils as compared to control. Among soil organic matter (SOM) density fractions, higher TC contents were documented in the FF and IAF from biochar treatments as compared to the straw. The FTIR spectra of the FF from the charcoal and HTC treatments showed the presence of aluminosilicate minerals on surfaces of SOM. There were slight changes in the FF of straw and HTC treatments as compared to spectra of original amendments. The study suggests that the stability of charcoal and HTC in soils is due to the recalcitrant nature of biochar followed by occlusion into soil micro-aggregates.
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spelling doaj.art-2df54096e70c40d0b9a1ee248ba9dde22023-02-23T03:46:08ZengCzech Academy of Agricultural SciencesPlant, Soil and Environment1214-11781805-93682014-08-0160833734310.17221/768/2013-PSEpse-201408-0001Biochars influence differential distribution and chemical composition of soil organic matterM.F. Qayyum0D. Steffens1H.P. Reisenauer2S. Schubert3Institute of Plant Nutrition, Research Centre for BioSystems, Land Use and Nutrition, Justus Liebig University, Giessen, GermanyInstitute of Plant Nutrition, Research Centre for BioSystems, Land Use and Nutrition, Justus Liebig University, Giessen, GermanyInstitute of Organic Chemistry, Justus Liebig University, Giessen, GermanyInstitute of Plant Nutrition, Research Centre for BioSystems, Land Use and Nutrition, Justus Liebig University, Giessen, GermanyIn the present study, three soils (Ferralsol, Luvisol topsoil, and Luvisol subsoil) were amended with biochars (charcoal, hydrothermal carbonization coal (HTC) of bark, and low-temperature conversion coal of sewage sludge), wheat straw and a control (no amendment) and incubated over a period of 365 days. Each amendment was applied at a rate of 11.29 g C/kg soil. After incubation, the soils were analyzed to retrieve three density fractions (free fraction (FF), intra-aggregate fraction (IAF), and heavy fraction) which were analyzed for total carbon (TC) contents and scanned by fourier transform infrared spectroscopy (FTIR). The biochars and straw significantly increased the TC contents of soils as compared to control. Among soil organic matter (SOM) density fractions, higher TC contents were documented in the FF and IAF from biochar treatments as compared to the straw. The FTIR spectra of the FF from the charcoal and HTC treatments showed the presence of aluminosilicate minerals on surfaces of SOM. There were slight changes in the FF of straw and HTC treatments as compared to spectra of original amendments. The study suggests that the stability of charcoal and HTC in soils is due to the recalcitrant nature of biochar followed by occlusion into soil micro-aggregates.https://pse.agriculturejournals.cz/artkey/pse-201408-0001_biochars-influence-differential-distribution-and-chemical-composition-of-soil-organic-matter.phpcarbon stabilizationc sequestrationfourier transform infrared spectroscopydensity fractionation
spellingShingle M.F. Qayyum
D. Steffens
H.P. Reisenauer
S. Schubert
Biochars influence differential distribution and chemical composition of soil organic matter
Plant, Soil and Environment
carbon stabilization
c sequestration
fourier transform infrared spectroscopy
density fractionation
title Biochars influence differential distribution and chemical composition of soil organic matter
title_full Biochars influence differential distribution and chemical composition of soil organic matter
title_fullStr Biochars influence differential distribution and chemical composition of soil organic matter
title_full_unstemmed Biochars influence differential distribution and chemical composition of soil organic matter
title_short Biochars influence differential distribution and chemical composition of soil organic matter
title_sort biochars influence differential distribution and chemical composition of soil organic matter
topic carbon stabilization
c sequestration
fourier transform infrared spectroscopy
density fractionation
url https://pse.agriculturejournals.cz/artkey/pse-201408-0001_biochars-influence-differential-distribution-and-chemical-composition-of-soil-organic-matter.php
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AT hpreisenauer biocharsinfluencedifferentialdistributionandchemicalcompositionofsoilorganicmatter
AT sschubert biocharsinfluencedifferentialdistributionandchemicalcompositionofsoilorganicmatter