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| 5. |  | CARVALHO, A. M.; BUSTAMANTE, M. M. C. Decomposição de resíduos vegetais e efeitos em carbono, nitrogênio e fósforo do solo sob sistemas convencional e plantio direto. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 28.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 12.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 10.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 7., 2008, Londrina. FertBio 2008: desafios para o uso do solo com eficiência e qualidade ambiental: anais. Londrina: SBCS: Embrapa Soja: IAPAR: UEL, 2008. 1 CD-ROM.| Biblioteca(s): Embrapa Cerrados. |
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| Registros recuperados : 126 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Unidades Centrais. |
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Data corrente: |
06/11/2003 |
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Data da última atualização: |
26/10/2018 |
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Autoria: |
NARDOTO, G. B.; BUSTAMANTE, M. M. da C. |
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Afiliação: |
Gabriela Bielefeld Nardoto, Universidade de São Paulo - USP/Centro de Energia Nuclear na Agricultura - CENA; Mercedes Maria da Cunha Bustamante, Universidade de Brasília - UnB/Departamento de Ecologia. |
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Título: |
Effects of fire on soil nitrogen dynamics and microbial biomass in savannas of Central Brazil. |
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Ano de publicação: |
2003 |
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Fonte/Imprenta: |
Pesquisa Agropecuária Brasileira, Brasília, DF, v. 38, n. 8, p. 955-962, ago. 2003 |
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Idioma: |
Inglês |
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Notas: |
Título em português: Efeitos do fogo na dinâmica do nitrogênio no solo e biomassa microbiana em área de Cerrado. |
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Conteúdo: |
The objective of this work was to study the effects of fire on net N mineralization and soil microbial biomass in burned and unburned cerrado stricto sensu sites. The study was carried out from April 1998 to April 2000. The pH values were significantly higher in the burned site while soil moisture content was significantly higher in the unburned site (P<0.05). The soil C/N ratio was 22/1 and the available NO3-N ranged between 1.5 and 2.8 mg kg-1 dry weight. However, the NH4-N concentration ranged between 3 and 34 mg kg-1 dry weight in the burned site and between 3 and 22 mg kg-1 dry weight in the unburned site. The NH4-N increased after fire, but no significant changes were observed for NO3-N (P<0.05). The NO3-N accumulation occurred in short periods during the rainy season. The rates of net N mineralization increased during the rainy season while reductions in soil microbial biomass were observed at both sites. This suggested that the peak in microbial activities occurred with the first rain events, with an initial net immobilization followed by net mineralization. Both sites presented the same pattern for mineralization/immobilization, however, the amount of inorganic-N cycled annually in unburned site was 14.7 kg ha-1 per year while the burned site presented only 3.8 kg ha-1 of inorganic-N, one year after the burning. |
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Palavras-Chave: |
mineralização do nitrogênio; nitrogen mineralization. |
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Thesagro: |
Composto Inorgânico; Nitrificação; Queimada. |
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Thesaurus NAL: |
burning; inorganic compounds; nitrification. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/108533/1/Effects.pdf
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Marc: |
LEADER 02193naa a2200241 a 4500
001 1109187
005 2018-10-26
008 2003 bl uuuu u00u1 u #d
100 1 $aNARDOTO, G. B.
245 $aEffects of fire on soil nitrogen dynamics and microbial biomass in savannas of Central Brazil.
260 $c2003
500 $aTítulo em português: Efeitos do fogo na dinâmica do nitrogênio no solo e biomassa microbiana em área de Cerrado.
520 $aThe objective of this work was to study the effects of fire on net N mineralization and soil microbial biomass in burned and unburned cerrado stricto sensu sites. The study was carried out from April 1998 to April 2000. The pH values were significantly higher in the burned site while soil moisture content was significantly higher in the unburned site (P<0.05). The soil C/N ratio was 22/1 and the available NO3-N ranged between 1.5 and 2.8 mg kg-1 dry weight. However, the NH4-N concentration ranged between 3 and 34 mg kg-1 dry weight in the burned site and between 3 and 22 mg kg-1 dry weight in the unburned site. The NH4-N increased after fire, but no significant changes were observed for NO3-N (P<0.05). The NO3-N accumulation occurred in short periods during the rainy season. The rates of net N mineralization increased during the rainy season while reductions in soil microbial biomass were observed at both sites. This suggested that the peak in microbial activities occurred with the first rain events, with an initial net immobilization followed by net mineralization. Both sites presented the same pattern for mineralization/immobilization, however, the amount of inorganic-N cycled annually in unburned site was 14.7 kg ha-1 per year while the burned site presented only 3.8 kg ha-1 of inorganic-N, one year after the burning.
650 $aburning
650 $ainorganic compounds
650 $anitrification
650 $aComposto Inorgânico
650 $aNitrificação
650 $aQueimada
653 $amineralização do nitrogênio
653 $anitrogen mineralization
700 1 $aBUSTAMANTE, M. M. da C.
773 $tPesquisa Agropecuária Brasileira, Brasília, DF$gv. 38, n. 8, p. 955-962, ago. 2003
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Embrapa Unidades Centrais (AI-SEDE) |
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