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| Registros recuperados : 151 | |
| 32. |  | AITA, C.; GIACOMINI, S. J.; PUJOL, S. B.; NICOLOSO, R. da S.; CORRÊA, J. C. Aproveitamento dos dejetos de suínos e bovinos como fertilizantes:impactos ambientais e estratégias de mitigação. In: PALHARES, J. C. P.; GLEBER, L. (Ed.). Gestão ambiental na agropecuária. Brasília, DF: Embrapa, v. 2, p. 199-282.| Biblioteca(s): Embrapa Suínos e Aves. |
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| 35. | | MATTEI, R. M.; GROHSKOPF, M. A.; CORREA, J. C.; RAIZER, D.; NICOLOSO, R. da S. Cinco anos de produtividade de milho adubado com cama de aves ou fertilizantes mineral em plantio direto. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 32.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 16.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 14.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 11., 2016, Goiânia. Rumo aos novos desafios: [anais]. Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2016. Fertbio 2016.| Biblioteca(s): Embrapa Suínos e Aves. |
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| 37. | | CORREA, J. C.; GROHSKOPF, M. A.; BENITES, V. de M.; NICOLOSO, R. da S.; RAIZER, D. Fertilizantes organominerais e minerais como fonte der fósforo na cultura do milho. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 32.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 16.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 14.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 11., 2016, Goiânia. Rumo aos novos desafios: [anais]. Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2016. Fertbio 2016.| Biblioteca(s): Embrapa Suínos e Aves. |
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| 38. | | CORREA, J. C.; GROHSKOPF, M. A.; BENITES, V. de M.; NICOLOSO, R. da S.; RAIZER, D. Fertilizantes organominerais e minerais como fonte de fósforo na cultura do milho. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 32.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 16.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 14.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 11., 2016, Goiânia. Rumo aos novos desafios: anais. Goiânia: SBCS, Núcleo Regional Centro-Oeste, 2016. FertBio 2016.| Biblioteca(s): Embrapa Solos. |
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| Registros recuperados : 151 | |
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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
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Biblioteca(s): |
Embrapa Suínos e Aves. |
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Data corrente: |
07/06/2016 |
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Data da última atualização: |
09/06/2016 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
NICOLOSO, R. da S.; RICE, C. W.; AMADO, T. J. C. |
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Afiliação: |
RODRIGO DA SILVEIRA NICOLOSO, CNPSA; Kansas State University; TELMO JORGE CARNEIRO AMADO, UFSM. |
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Título: |
Kinetic to saturation model for simulation of soil organic carbon increase to steady state. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Soil Science Society of America Journal, v. 80, n. 1, p. 147-156, 2016. |
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DOI: |
10.2136/sssaj2015.04.0163 |
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Idioma: |
Inglês |
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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 |
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Thesagro: |
Carbono; Composto orgânico; Manejo do solo. |
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Categoria do assunto: |
-- |
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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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