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Registro Completo |
Biblioteca(s): |
Embrapa Acre; Embrapa Agrobiologia; Embrapa Amapá. |
Data corrente: |
26/12/2001 |
Data da última atualização: |
06/06/2019 |
Autoria: |
NOGUEIRA, F. D.; SILVA, E. de B.; GUIMARÃES, P. T. G. (ed.). |
Título: |
Adubação potassica do cafeeiro: sulfato de potássio. |
Ano de publicação: |
2001 |
Fonte/Imprenta: |
Washington: Sulphate of Potash Information Board, 2001. |
Páginas: |
81 p. |
Idioma: |
Português |
Conteúdo: |
Funções do potássio, do enxôfre e do cloro nas culturas em geral. Potássio. Importância do potássio na eficiência do uso da água. Fotossíntese. Transporte de açúcares. Transporte de água e nutrientes. Ativação de enzimas. Enxofre. Cloro. Potássio, enxofre e cloro no solo. Comportamento do potássio no solo. Comportamento do SO2- 4 e do Cl- no solo. Potássio, enxofre e cloro para o cafeeiro. Resposta do cafeeiro à adubação potássica. Resposta do cafeeiro à adubação com enxofre. Efeitos do cloro sobre o cafeeiro. Índice salino. Efeito do cloro. Qualidade. |
Palavras-Chave: |
Coffee; Potassium sulphate. |
Thesagro: |
Adubação; Café; Cloro; Enxofre; Fertilidade do Solo; Potássio; Sulfato de Potássio. |
Thesaurus Nal: |
fertilizers; soil fertility. |
Categoria do assunto: |
-- |
Marc: |
LEADER 01300nam a2200277 a 4500 001 1346772 005 2019-06-06 008 2001 bl uuuu 00u1 u #d 100 1 $aNOGUEIRA, F. D. 245 $aAdubação potassica do cafeeiro$bsulfato de potássio. 260 $aWashington: Sulphate of Potash Information Board$c2001 300 $a81 p. 520 $aFunções do potássio, do enxôfre e do cloro nas culturas em geral. Potássio. Importância do potássio na eficiência do uso da água. Fotossíntese. Transporte de açúcares. Transporte de água e nutrientes. Ativação de enzimas. Enxofre. Cloro. Potássio, enxofre e cloro no solo. Comportamento do potássio no solo. Comportamento do SO2- 4 e do Cl- no solo. Potássio, enxofre e cloro para o cafeeiro. Resposta do cafeeiro à adubação potássica. Resposta do cafeeiro à adubação com enxofre. Efeitos do cloro sobre o cafeeiro. Índice salino. Efeito do cloro. Qualidade. 650 $afertilizers 650 $asoil fertility 650 $aAdubação 650 $aCafé 650 $aCloro 650 $aEnxofre 650 $aFertilidade do Solo 650 $aPotássio 650 $aSulfato de Potássio 653 $aCoffee 653 $aPotassium sulphate 700 1 $aSILVA, E. de B. 700 1 $aGUIMARÃES, P. T. G.
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Registro original: |
Embrapa Amapá (CPAF-AP) |
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| Acesso ao texto completo restrito à biblioteca da Embrapa Suínos e Aves. Para informações adicionais entre em contato com cnpsa.biblioteca@embrapa.br. |
Registro Completo
Biblioteca(s): |
Embrapa Suínos e Aves. |
Data corrente: |
07/06/2016 |
Data da última atualização: |
09/06/2016 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
NICOLOSO, R. da S.; RICE, C. W.; AMADO, T. J. C. |
Afiliação: |
RODRIGO DA SILVEIRA NICOLOSO, CNPSA; Kansas State University; TELMO JORGE CARNEIRO AMADO, UFSM. |
Título: |
Kinetic to saturation model for simulation of soil organic carbon increase to steady state. |
Ano de publicação: |
2016 |
Fonte/Imprenta: |
Soil Science Society of America Journal, v. 80, n. 1, p. 147-156, 2016. |
DOI: |
10.2136/sssaj2015.04.0163 |
Idioma: |
Inglês |
Conteúdo: |
The use of mathematical models predicting SOC dynamics can provide relevant information about the C storage potential of agricultural soils. We evaluated three mathematical models (first-order kinetic, C saturation, and a proposed kinetic to saturation) predicting SOC dynamics and steady-state SOC of a Hapludoll from central Kansas. The study was based on a long-term experiment (17 yr) assessing soil tillage systems (chisel tillage [CT] and notill [NT]) and N fertilizer sources (168 kg N ha?1 as NH4NO3 [MF], cattle manure [OF], and a control treatment without N [CO]. The soil under NT (0?5 cm) had significant SOC accumulation (>0.23 Mg C ha?1 yr?1) regardless of fertilization source, while the CT soil had negligible changes in SOC (<0.12 Mg C ha?1 yr?1) without the addition of organic fertilizer as an external C source. Organic fertilization increased the original SOC by 56 and 192%, reaching steady state at 15.9 and 28.0 Mg ha?1 in CT and NT soils, respectively. The SOC predicted by all three models had significant correlations (r > 0.80, p < 0.05) with measured SOC. However, the C saturation model overestimated the measured SOC under C-depleted conditions, failing RMSE and lack-of-fit tests, while the first-order kinetic model overestimated NT OF steady-state SOC by up to 58% in relation to the maximum SOC storage capacity determined for NT soils. The SOC predicted by the kinetic to saturation model agreed with both measured SOC and the maximum SOC storage capacity of NT soils. The kinetic to saturation model can be used for long-term simulation of SOC dynamics in soils that are either C depleted or close to saturation. MenosThe use of mathematical models predicting SOC dynamics can provide relevant information about the C storage potential of agricultural soils. We evaluated three mathematical models (first-order kinetic, C saturation, and a proposed kinetic to saturation) predicting SOC dynamics and steady-state SOC of a Hapludoll from central Kansas. The study was based on a long-term experiment (17 yr) assessing soil tillage systems (chisel tillage [CT] and notill [NT]) and N fertilizer sources (168 kg N ha?1 as NH4NO3 [MF], cattle manure [OF], and a control treatment without N [CO]. The soil under NT (0?5 cm) had significant SOC accumulation (>0.23 Mg C ha?1 yr?1) regardless of fertilization source, while the CT soil had negligible changes in SOC (<0.12 Mg C ha?1 yr?1) without the addition of organic fertilizer as an external C source. Organic fertilization increased the original SOC by 56 and 192%, reaching steady state at 15.9 and 28.0 Mg ha?1 in CT and NT soils, respectively. The SOC predicted by all three models had significant correlations (r > 0.80, p < 0.05) with measured SOC. However, the C saturation model overestimated the measured SOC under C-depleted conditions, failing RMSE and lack-of-fit tests, while the first-order kinetic model overestimated NT OF steady-state SOC by up to 58% in relation to the maximum SOC storage capacity determined for NT soils. The SOC predicted by the kinetic to saturation model agreed with both measured SOC and the maximum SOC storage capacity of NT s... Mostrar Tudo |
Thesagro: |
Carbono; Composto orgânico; Manejo do solo. |
Categoria do assunto: |
-- |
Marc: |
LEADER 02268naa a2200193 a 4500 001 2046541 005 2016-06-09 008 2016 bl uuuu u00u1 u #d 024 7 $a10.2136/sssaj2015.04.0163$2DOI 100 1 $aNICOLOSO, R. da S. 245 $aKinetic to saturation model for simulation of soil organic carbon increase to steady state.$h[electronic resource] 260 $c2016 520 $aThe use of mathematical models predicting SOC dynamics can provide relevant information about the C storage potential of agricultural soils. We evaluated three mathematical models (first-order kinetic, C saturation, and a proposed kinetic to saturation) predicting SOC dynamics and steady-state SOC of a Hapludoll from central Kansas. The study was based on a long-term experiment (17 yr) assessing soil tillage systems (chisel tillage [CT] and notill [NT]) and N fertilizer sources (168 kg N ha?1 as NH4NO3 [MF], cattle manure [OF], and a control treatment without N [CO]. The soil under NT (0?5 cm) had significant SOC accumulation (>0.23 Mg C ha?1 yr?1) regardless of fertilization source, while the CT soil had negligible changes in SOC (<0.12 Mg C ha?1 yr?1) without the addition of organic fertilizer as an external C source. Organic fertilization increased the original SOC by 56 and 192%, reaching steady state at 15.9 and 28.0 Mg ha?1 in CT and NT soils, respectively. The SOC predicted by all three models had significant correlations (r > 0.80, p < 0.05) with measured SOC. However, the C saturation model overestimated the measured SOC under C-depleted conditions, failing RMSE and lack-of-fit tests, while the first-order kinetic model overestimated NT OF steady-state SOC by up to 58% in relation to the maximum SOC storage capacity determined for NT soils. The SOC predicted by the kinetic to saturation model agreed with both measured SOC and the maximum SOC storage capacity of NT soils. The kinetic to saturation model can be used for long-term simulation of SOC dynamics in soils that are either C depleted or close to saturation. 650 $aCarbono 650 $aComposto orgânico 650 $aManejo do solo 700 1 $aRICE, C. W. 700 1 $aAMADO, T. J. C. 773 $tSoil Science Society of America Journal$gv. 80, n. 1, p. 147-156, 2016.
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