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 | Acesso ao texto completo restrito à biblioteca da Embrapa Instrumentação. Para informações adicionais entre em contato com cnpdia.biblioteca@embrapa.br. |
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Registro Completo |
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Biblioteca(s): |
Embrapa Instrumentação. |
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Data corrente: |
09/01/2023 |
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Data da última atualização: |
29/11/2024 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
MONTES, C. R.; MERDY, P.; SILVA, W. T. L. da; ISHIDA, D.; MELFI, A. J.; SANTIN, R. C.; LUCAS Y. |
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Afiliação: |
CELIA R. MONTES, UNIVERSIDADE DE SAO PAULO; PATRICIA MERDY, UNIVERSIT´E DE TOULON; WILSON TADEU LOPES DA SILVA, CNPDIA; DÉBORA ISHIDA, UNIVERSIDADE DE SAO PAULO; ADOPHO J. MELFI, UNIVERSIDADE DE SAO PAULO; ROBERTA C. SANTIN, UNIVERSIDADE DE SAO PAULO. |
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Título: |
Mineralization of soil organic matter from equatorial giant podzols submitted to drier pedoclimate: A drainage topochronosequence study. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
Catena, v. 222, 106837. |
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Páginas: |
1 - 10 |
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ISSN: |
0341-8162 |
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DOI: |
https://doi.org/10.1016/j.catena.2022.106837 |
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Idioma: |
Inglês |
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Conteúdo: |
Podzol soils are an important carbon pool in the Amazon, due to the high organic matter (OM) content in their topsoil horizons and deep Bh. To quantify the evolution of the stock and the lability of this carbon pool in the hypothesis of the onset of drier climates, we studied a soil toposequence at the end of which the incision of a river meander lowered the water table, as would result from a drier climate, allowing oxidation the Bh horizons. The soil OM was quantified and characterized (physical fractionation, humification indexes, 14C average age) and its lability under oxic conditions was estimated by measuring respiration during a 660-days experiment. Podzol genesis time was calculated by constraining the carbon fluxes using both C stock and 14C average age. The results confirmed that the studied podzols store large amounts of carbon (62.8 kgC m− 2 on average). They resulted from a long genesis time, probably greater than 30?50 ky. Topsoil OM is very labile with a residence time of about 100 y; Bh OM is highly humified with a high C/N (62.7 on average) related to low respiration rates. The measured respiration rates were used to estimate the C emission that would result from drier climates at 55 gC m− 2 y− 1 on average during the first 100 y, which would correspond, by extrapolation, to 8.5 1012 gC y− 1 for all Amazonian podzols. |
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Palavras-Chave: |
Amazon podzol; Humification index; Soil carbon storage and loss; Soil formation rate. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02219naa a2200277 a 4500
001 2150786
005 2024-11-29
008 2023 bl uuuu u00u1 u #d
022 $a0341-8162
024 7 $ahttps://doi.org/10.1016/j.catena.2022.106837$2DOI
100 1 $aMONTES, C. R.
245 $aMineralization of soil organic matter from equatorial giant podzols submitted to drier pedoclimate$bA drainage topochronosequence study.$h[electronic resource]
260 $c2023
300 $a1 - 10
520 $aPodzol soils are an important carbon pool in the Amazon, due to the high organic matter (OM) content in their topsoil horizons and deep Bh. To quantify the evolution of the stock and the lability of this carbon pool in the hypothesis of the onset of drier climates, we studied a soil toposequence at the end of which the incision of a river meander lowered the water table, as would result from a drier climate, allowing oxidation the Bh horizons. The soil OM was quantified and characterized (physical fractionation, humification indexes, 14C average age) and its lability under oxic conditions was estimated by measuring respiration during a 660-days experiment. Podzol genesis time was calculated by constraining the carbon fluxes using both C stock and 14C average age. The results confirmed that the studied podzols store large amounts of carbon (62.8 kgC m− 2 on average). They resulted from a long genesis time, probably greater than 30?50 ky. Topsoil OM is very labile with a residence time of about 100 y; Bh OM is highly humified with a high C/N (62.7 on average) related to low respiration rates. The measured respiration rates were used to estimate the C emission that would result from drier climates at 55 gC m− 2 y− 1 on average during the first 100 y, which would correspond, by extrapolation, to 8.5 1012 gC y− 1 for all Amazonian podzols.
653 $aAmazon podzol
653 $aHumification index
653 $aSoil carbon storage and loss
653 $aSoil formation rate
700 1 $aMERDY, P.
700 1 $aSILVA, W. T. L. da
700 1 $aISHIDA, D.
700 1 $aMELFI, A. J.
700 1 $aSANTIN, R. C.
700 1 $aLUCAS Y.
773 $tCatena$gv. 222, 106837.
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