Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils

The composition of black carbon (BC) was studied up to now using laboratory experiments, which often fail to reproduce conditions occurring in natural fires. We sampled plant material and two BC fractions produced during slash and burn agriculture from two adjacent sites. A coarse fraction (CF), mos...

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Main Authors: Rumpel, C., González Perez, J.A., Bardoux, G., Largeau, C., González Vila, F.J., Valentin, Christian
Format: Journal Article
Language:Inglés
Published: 2007
Subjects:
Online Access:https://hdl.handle.net/10568/40889
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author Rumpel, C.
González Perez, J.A.
Bardoux, G.
Largeau, C.
González Vila, F.J.
Valentin, Christian
author_browse Bardoux, G.
González Perez, J.A.
González Vila, F.J.
Largeau, C.
Rumpel, C.
Valentin, Christian
author_facet Rumpel, C.
González Perez, J.A.
Bardoux, G.
Largeau, C.
González Vila, F.J.
Valentin, Christian
author_sort Rumpel, C.
collection Repository of Agricultural Research Outputs (CGSpace)
description The composition of black carbon (BC) was studied up to now using laboratory experiments, which often fail to reproduce conditions occurring in natural fires. We sampled plant material and two BC fractions produced during slash and burn agriculture from two adjacent sites. A coarse fraction (CF), most probably derived from twigs and stems, was differentiated from lighter, fluffy fine material (FF). The samples were analysed for elemental and isotopic composition and their reactivity using acid hydrolysis and acid dichromate oxidation. The chemical composition of the samples was studied by 13C CPMAS NMR spectroscopy and analytical pyrolysis. The lignin content of the samples was determined after CuO oxidation. The two BC fractions were higher in carbon than the plant material. On an ash-free basis the CF and FF sampled from the two different sites had remarkably similar elemental contents. Stable isotope ratios of carbon showed enrichment or depletion depending on the morphological fraction under C3 vegetation. The ratios tended to be depleted in 13C with regards to the plant material in both fractions for samples taken under C4 vegetation. The reactivity of BC towards dichromate oxidation and acid hydrolysis was lower for CF compared to FF. 13C CPMAS NMR spectroscopy showed that BC fractions were aromatic but could also show substantial contribution from alkyl and O-alkyl C. Analytical pyrolysis and CuO oxidation indicated that part of the lignin backbone was remaining in all BC
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spelling CGSpace408892023-02-15T12:13:48Z Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils Rumpel, C. González Perez, J.A. Bardoux, G. Largeau, C. González Vila, F.J. Valentin, Christian forest soils nitrogen carbon shifting cultivation forest fires wildfires The composition of black carbon (BC) was studied up to now using laboratory experiments, which often fail to reproduce conditions occurring in natural fires. We sampled plant material and two BC fractions produced during slash and burn agriculture from two adjacent sites. A coarse fraction (CF), most probably derived from twigs and stems, was differentiated from lighter, fluffy fine material (FF). The samples were analysed for elemental and isotopic composition and their reactivity using acid hydrolysis and acid dichromate oxidation. The chemical composition of the samples was studied by 13C CPMAS NMR spectroscopy and analytical pyrolysis. The lignin content of the samples was determined after CuO oxidation. The two BC fractions were higher in carbon than the plant material. On an ash-free basis the CF and FF sampled from the two different sites had remarkably similar elemental contents. Stable isotope ratios of carbon showed enrichment or depletion depending on the morphological fraction under C3 vegetation. The ratios tended to be depleted in 13C with regards to the plant material in both fractions for samples taken under C4 vegetation. The reactivity of BC towards dichromate oxidation and acid hydrolysis was lower for CF compared to FF. 13C CPMAS NMR spectroscopy showed that BC fractions were aromatic but could also show substantial contribution from alkyl and O-alkyl C. Analytical pyrolysis and CuO oxidation indicated that part of the lignin backbone was remaining in all BC 2007 2014-06-13T14:48:37Z 2014-06-13T14:48:37Z Journal Article https://hdl.handle.net/10568/40889 en Limited Access Rumpel, C.; Gonzalez-Perez, J. A.; Bardoux, G.; Largeau, C.; Gonzalez-Vila, F. J.; Valentin, Christian. 2007. Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils. Organic Geochemistry, 38:911?920.
spellingShingle forest soils
nitrogen
carbon
shifting cultivation
forest fires
wildfires
Rumpel, C.
González Perez, J.A.
Bardoux, G.
Largeau, C.
González Vila, F.J.
Valentin, Christian
Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title_full Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title_fullStr Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title_full_unstemmed Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title_short Composition and reactivity of morphologically distinct charred materials left after slash-and- burn practices in agricultural tropical soils
title_sort composition and reactivity of morphologically distinct charred materials left after slash and burn practices in agricultural tropical soils
topic forest soils
nitrogen
carbon
shifting cultivation
forest fires
wildfires
url https://hdl.handle.net/10568/40889
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