Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols
The objective of this work was to evaluate the distribution pattern and composition of soil organic matter (SOM) and its physical pools of Leptosols periodically affected by fire over the last 100 years in South Brazil. Soil samples at 0-5, 5-10, and 10-15 cm depths were collected from the following...
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Embrapa Informação Tecnológica
2012-05-01
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Series: | Pesquisa Agropecuária Brasileira |
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Online Access: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-204X2012000500011&lng=en&tlng=en |
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doaj-0a204b2f3332413a88e0fd339364be562020-11-24T21:43:03ZengEmbrapa Informação TecnológicaPesquisa Agropecuária Brasileira1678-39212012-05-0147570771510.1590/S0100-204X2012000500011S0100-204X2012000500011Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian LeptosolsMariana da Luz Potes0Deborah Pinheiro Dick1Graciele Sarante Santana2Michely Tomazi3Cimélio Bayer4EmbrapaUniversidade Federal do Rio Grande do SulUniversidade Federal do Rio Grande do SulEmbrapaUniversidade Federal do Rio Grande do SulThe objective of this work was to evaluate the distribution pattern and composition of soil organic matter (SOM) and its physical pools of Leptosols periodically affected by fire over the last 100 years in South Brazil. Soil samples at 0-5, 5-10, and 10-15 cm depths were collected from the following environments: native pasture without burning in the last year and grazed with 0.5 livestock per hectare per year (1NB); native pasture without burning in the last 23 years and grazed with 2.0 livestock per hectare per year (23NB); and an Araucaria forest (AF). Physical fractionation was performed with the 0-5 and 5-10 cm soil layers. Soil C and N stocks were determined in the three depths and in the physical pools, and organic matter was characterized by infrared spectroscopy and thermogravimetry. The largest C stocks in all depths and physical pools were found under the AF. The 23NB environment showed the lowest soil C and N stocks at the 5-15 cm depth, which was related to the end of burning and to the higher grazing intensity. The SOM of the occluded light fraction showed a greater chemical recalcitrance in 1NB than in 23NB. Annual pasture burning does not affect soil C stocks up to 15 cm of depth.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-204X2012000500011&lng=en&tlng=enfrações físicasestoque de carbonocomposição químicarecalcitrância químicatermo-decomposição |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mariana da Luz Potes Deborah Pinheiro Dick Graciele Sarante Santana Michely Tomazi Cimélio Bayer |
spellingShingle |
Mariana da Luz Potes Deborah Pinheiro Dick Graciele Sarante Santana Michely Tomazi Cimélio Bayer Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols Pesquisa Agropecuária Brasileira frações físicas estoque de carbono composição química recalcitrância química termo-decomposição |
author_facet |
Mariana da Luz Potes Deborah Pinheiro Dick Graciele Sarante Santana Michely Tomazi Cimélio Bayer |
author_sort |
Mariana da Luz Potes |
title |
Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols |
title_short |
Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols |
title_full |
Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols |
title_fullStr |
Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols |
title_full_unstemmed |
Soil organic matter in fire-affected pastures and in an Araucaria forest in South-Brazilian Leptosols |
title_sort |
soil organic matter in fire-affected pastures and in an araucaria forest in south-brazilian leptosols |
publisher |
Embrapa Informação Tecnológica |
series |
Pesquisa Agropecuária Brasileira |
issn |
1678-3921 |
publishDate |
2012-05-01 |
description |
The objective of this work was to evaluate the distribution pattern and composition of soil organic matter (SOM) and its physical pools of Leptosols periodically affected by fire over the last 100 years in South Brazil. Soil samples at 0-5, 5-10, and 10-15 cm depths were collected from the following environments: native pasture without burning in the last year and grazed with 0.5 livestock per hectare per year (1NB); native pasture without burning in the last 23 years and grazed with 2.0 livestock per hectare per year (23NB); and an Araucaria forest (AF). Physical fractionation was performed with the 0-5 and 5-10 cm soil layers. Soil C and N stocks were determined in the three depths and in the physical pools, and organic matter was characterized by infrared spectroscopy and thermogravimetry. The largest C stocks in all depths and physical pools were found under the AF. The 23NB environment showed the lowest soil C and N stocks at the 5-15 cm depth, which was related to the end of burning and to the higher grazing intensity. The SOM of the occluded light fraction showed a greater chemical recalcitrance in 1NB than in 23NB. Annual pasture burning does not affect soil C stocks up to 15 cm of depth. |
topic |
frações físicas estoque de carbono composição química recalcitrância química termo-decomposição |
url |
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-204X2012000500011&lng=en&tlng=en |
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