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Registro Completo |
Biblioteca(s): |
Embrapa Soja. |
Data corrente: |
27/12/2021 |
Data da última atualização: |
30/03/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
DUARTE, A. N. M.; SOARES FILHO, C. V.; CARVALHO, C. L. M. de; TEIXEIRA FILHO, M. C. M.; NOGUEIRA, M. A.; HUNGRIA, M.; ISHIY, A. G.; VALVANO, I. M. |
Afiliação: |
AMÁRIO NUNO MEIRELES DUARTE, Universidade Estadual Paulista, UNESP, Ilha Solteira, SP.; CECÍLIO VIEGA SOARES FILHO, Universidade Estadual Paulista, UNESP, Araçatuba, SP.; CAROLINE LOPES MONTEIRO DE CARVALHO, Universidade Estadual Paulista, UNESP, Araçatuba, SP.; MARCELO CARVALHO MINHOTO TEIXEIRA FILHO, Universidade Estadual Paulista, UNESP, Ilha Solteira, SP.; MARCO ANTONIO NOGUEIRA, CNPSO; MARIANGELA HUNGRIA DA CUNHA, CNPSO; AMANDA GONÇALVES ISHIY, Universidade Estadual Paulista, UNESP, Araçatuba, SP.; ISADORA MANDOLESI VALVANO, Universidade Estadual Paulista, UNESP, Araçatuba, SP. |
Título: |
Inoculation with plant growth-promoting bacteria and reduction of nitrogen fertilizer in herbage accumulation and nutritional value of Mavuno grass. |
Ano de publicação: |
2021 |
Fonte/Imprenta: |
International Journal for Innovation Education and Research, v. 9, n. 3, p. 16-34, 2021. |
ISSN: |
2411-2933 |
DOI: |
https://doi.org/10.31686/ijier.vol9.iss3.2962 |
Idioma: |
Inglês |
Palavras-Chave: |
Bactérias diazotróficas; Diazotrophic bacteria; Urochloa spp. |
Thesagro: |
Bactéria; Fixação de Nitrogênio; Gramínea Forrageira; Gramínea Tropical; Proteína Bruta. |
Thesaurus Nal: |
Crude protein; Fertilizers; Forage grasses; Tropical forests; Urochloa. |
Categoria do assunto: |
F Plantas e Produtos de Origem Vegetal |
Marc: |
LEADER 01224naa a2200373 a 4500 001 2138418 005 2022-03-30 008 2021 bl uuuu u00u1 u #d 022 $a2411-2933 024 7 $ahttps://doi.org/10.31686/ijier.vol9.iss3.2962$2DOI 100 1 $aDUARTE, A. N. M. 245 $aInoculation with plant growth-promoting bacteria and reduction of nitrogen fertilizer in herbage accumulation and nutritional value of Mavuno grass.$h[electronic resource] 260 $c2021 650 $aCrude protein 650 $aFertilizers 650 $aForage grasses 650 $aTropical forests 650 $aUrochloa 650 $aBactéria 650 $aFixação de Nitrogênio 650 $aGramínea Forrageira 650 $aGramínea Tropical 650 $aProteína Bruta 653 $aBactérias diazotróficas 653 $aDiazotrophic bacteria 653 $aUrochloa spp 700 1 $aSOARES FILHO, C. V. 700 1 $aCARVALHO, C. L. M. de 700 1 $aTEIXEIRA FILHO, M. C. M. 700 1 $aNOGUEIRA, M. A. 700 1 $aHUNGRIA, M. 700 1 $aISHIY, A. G. 700 1 $aVALVANO, I. M. 773 $tInternational Journal for Innovation Education and Research$gv. 9, n. 3, p. 16-34, 2021.
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Biblioteca(s): |
Embrapa Florestas. |
Data corrente: |
14/11/2019 |
Data da última atualização: |
14/11/2019 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
VELOSO, M. G.; DIECKOW, J.; ZANATTA, J. A.; PERGHER, M.; BAYER, C.; HIGA, R. C. V. |
Afiliação: |
Murilo G. Veloso, UFPR; Jeferson Dieckow, UFPR; JOSILEIA ACORDI ZANATTA, CNPF; Maico Pergher, UFPR; Cimélio Bayer, UFRGS; Rosana Clara Victoria Higa, Pesquisadora aposentada da Embrapa Florestas. |
Título: |
Long-term loblolly pine land use reduces methane and net greenhouse gas emissions in a subtropical Cambisol, despite increasing nitrous oxide. |
Ano de publicação: |
2019 |
Fonte/Imprenta: |
Annals of Forest Science, v. 7, n. 3, article 86, Sept. 2019. |
DOI: |
10.1007/s13595-019-0871-6 |
Idioma: |
Inglês |
Conteúdo: |
& Key message In loblolly pine land use of 17?32 years following forest clearing, CH4 consumption and N2O emission diminished by 17 years, due to high soilmoisture (~ 80%WFPS, N2O intoN2), but increased by 32 years, where medium moisture favoured methanotrophy and denitrification into N2O. Soil greenhouse gases (GHG) emission was positive by 17 years, but negative by 32, when soil sequestered carbon. & Context Much of the role of planted forests in the gaseous soil-atmosphere exchanges in the subtropics remains to be evaluated. & Aims To assess the impacts of loblolly pine (Pinus taeda L.) on soil nitrous oxide (N2O) and methane (CH4) fluxes in a subtropical Cambisol. & Methods Fluxes were monitored over 1 year with static chambers, in forest stands under natural forest (NF) and pine plantation for 17 (P17) and 32 years (P32). & Results The NF soil showed the lowestN2O emission and the highest CH4 consumption, because of the lowest water-filled pore space (WFPS, < 40%) and highest soil macroporosity. In P17, N2O emission was still low, but CH4 consumption diminished sixfold, possibly because of the predominance of methanotrophy, favoured by the highest WFPS (~ 80%) and lowest macroporosity that together with low mineral N concentration also did not favour the formation of N2O. In P32, the improved soil mineral N, macroporosity and intermediate WFPS (~ 60%) increased CH4 consumption and also N2O emission, in an environment supposedly favourable to methanotrophy and also to N2O production. Considering soil organic carbon (SOC) from a concurrent study, the net GHG emission (Mg Ceq ha?1 year?1) was 2.8 in P17 and ?1.1 in P32. Menos& Key message In loblolly pine land use of 17?32 years following forest clearing, CH4 consumption and N2O emission diminished by 17 years, due to high soilmoisture (~ 80%WFPS, N2O intoN2), but increased by 32 years, where medium moisture favoured methanotrophy and denitrification into N2O. Soil greenhouse gases (GHG) emission was positive by 17 years, but negative by 32, when soil sequestered carbon. & Context Much of the role of planted forests in the gaseous soil-atmosphere exchanges in the subtropics remains to be evaluated. & Aims To assess the impacts of loblolly pine (Pinus taeda L.) on soil nitrous oxide (N2O) and methane (CH4) fluxes in a subtropical Cambisol. & Methods Fluxes were monitored over 1 year with static chambers, in forest stands under natural forest (NF) and pine plantation for 17 (P17) and 32 years (P32). & Results The NF soil showed the lowestN2O emission and the highest CH4 consumption, because of the lowest water-filled pore space (WFPS, < 40%) and highest soil macroporosity. In P17, N2O emission was still low, but CH4 consumption diminished sixfold, possibly because of the predominance of methanotrophy, favoured by the highest WFPS (~ 80%) and lowest macroporosity that together with low mineral N concentration also did not favour the formation of N2O. In P32, the improved soil mineral N, macroporosity and intermediate WFPS (~ 60%) increased CH4 consumption and also N2O emission, in an environment supposedly favourable to methanotrophy and also to N2... Mostrar Tudo |
Palavras-Chave: |
Ammonium; GHGintensity; Nitrate; Southern Brazil. |
Thesagro: |
Nitrato; Reflorestamento; Temperatura. |
Thesaurus NAL: |
Reforestation; Temperature. |
Categoria do assunto: |
-- |
Marc: |
LEADER 02544naa a2200301 a 4500 001 2114380 005 2019-11-14 008 2019 bl uuuu u00u1 u #d 024 7 $a10.1007/s13595-019-0871-6$2DOI 100 1 $aVELOSO, M. G. 245 $aLong-term loblolly pine land use reduces methane and net greenhouse gas emissions in a subtropical Cambisol, despite increasing nitrous oxide.$h[electronic resource] 260 $c2019 520 $a& Key message In loblolly pine land use of 17?32 years following forest clearing, CH4 consumption and N2O emission diminished by 17 years, due to high soilmoisture (~ 80%WFPS, N2O intoN2), but increased by 32 years, where medium moisture favoured methanotrophy and denitrification into N2O. Soil greenhouse gases (GHG) emission was positive by 17 years, but negative by 32, when soil sequestered carbon. & Context Much of the role of planted forests in the gaseous soil-atmosphere exchanges in the subtropics remains to be evaluated. & Aims To assess the impacts of loblolly pine (Pinus taeda L.) on soil nitrous oxide (N2O) and methane (CH4) fluxes in a subtropical Cambisol. & Methods Fluxes were monitored over 1 year with static chambers, in forest stands under natural forest (NF) and pine plantation for 17 (P17) and 32 years (P32). & Results The NF soil showed the lowestN2O emission and the highest CH4 consumption, because of the lowest water-filled pore space (WFPS, < 40%) and highest soil macroporosity. In P17, N2O emission was still low, but CH4 consumption diminished sixfold, possibly because of the predominance of methanotrophy, favoured by the highest WFPS (~ 80%) and lowest macroporosity that together with low mineral N concentration also did not favour the formation of N2O. In P32, the improved soil mineral N, macroporosity and intermediate WFPS (~ 60%) increased CH4 consumption and also N2O emission, in an environment supposedly favourable to methanotrophy and also to N2O production. Considering soil organic carbon (SOC) from a concurrent study, the net GHG emission (Mg Ceq ha?1 year?1) was 2.8 in P17 and ?1.1 in P32. 650 $aReforestation 650 $aTemperature 650 $aNitrato 650 $aReflorestamento 650 $aTemperatura 653 $aAmmonium 653 $aGHGintensity 653 $aNitrate 653 $aSouthern Brazil 700 1 $aDIECKOW, J. 700 1 $aZANATTA, J. A. 700 1 $aPERGHER, M. 700 1 $aBAYER, C. 700 1 $aHIGA, R. C. V. 773 $tAnnals of Forest Science$gv. 7, n. 3, article 86, Sept. 2019.
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