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| Registros recuperados : 5.357 | |
| 122. |  | ANDRADE, C. G. C.; SILVA, M. L. da; TORRES, C. M. M. E.; RUSCHEL, A. R.; SILVA, L. F. da; ANDRADE, D. F. C. de; REIS, L. P. Crescimento diamétrico e tempo de passagem de Minquartia guianensis após manejo na Floresta Nacional do Tapajós. Pesquisa Florestal Brasileira, Colombo, v. 37, n. 91, p. 299-309, jul./set. 2017.| Biblioteca(s): Embrapa Amazônia Oriental; Embrapa Florestas. |
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| 123. | | ANDRADE, D. F. C. de; GAMA, J. R. V.; SANTOS, F. G.; MELO, M. S.; ESPAD, A. L. V.; KANASHIRO, M. O que aprendemos sobre manejo madeireiro de florestas nativas na Amazônia brasileira. In: GAMA, J. R. V.; ANDRADE, D. F. C. de (org.). Ciência Aplicada ao uso múltiplo da floresta no Baixo Rio Amazonas. Curitiba: Editora CRV, 2020. cap. 1, p. 29-50.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 131. | | ANDRADE, S. da C.; SOUZA, A. P. de; SILVA, E.; MACHADO, C. C.; LEITE, H. G.; NASCIMENTO, A. G. do; MINETTI, L. J. Analise dos principais impactos ambientais decorrentes da colheita e do transporte da madeira em dois comprimentos de tora. Revista Arvore, Vicosa, v.23, n.3, p.327-332, jul./set. 1999.| Biblioteca(s): Embrapa Florestas. |
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| 132. | | ANDRADE, S. da C.; SOUZA, A. P. de; SILVA, E.; NASCIMENTO, A. G. do; MACHADO, C. C.; LEITE, H. G.; MINETTI, L. J. Analise dos efeitos de compactacao do solo sobre a regeneracao das cepas de eucalipto. Revista Arvore, Vicosa, v. 24, n. 3, p. 261-268, 2000.| Biblioteca(s): Embrapa Florestas. |
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| Registros recuperados : 5.357 | |
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Registro Completo
|
Biblioteca(s): |
Embrapa Semiárido. |
|
Data corrente: |
07/10/2022 |
|
Data da última atualização: |
13/01/2023 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
B - 1 |
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Autoria: |
ARAÚJO, C. de A.; LIRA, J. B. de; MAGALHÃES, A. L. R.; SILVA, T. G. F. da; GOIS, G. C.; ANDRADE, A. P. de; ARAUJO, G. G. L. de; CAMPOS, F. S. |
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Afiliação: |
CLEYTON DE ALMEIDA ARAÚJO, UNIVASF; JACIELE BESERRA DE LIRA, UFPB, Areia, PB; ANDRÉ LUIZ RODRIGUES MAGALHÃES, UFRPE; THIERES GEORGE FREIRE DA SILVA, UFRPE, Garanhuns, PE; GLAYCIANE COSTA GOIS, UNIVASF; ALBERÍCIO PEREIRA DE ANDRADE, UFRPE, Garanhuns, PE; GHERMAN GARCIA LEAL DE ARAUJO, CPATSA; FLEMING SENA CAMPOS, Bolsista CNPq. |
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Título: |
Pearl millet cultivation with brackish water and organic fertilizeralters soil properties. |
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Ano de publicação: |
2021 |
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Fonte/Imprenta: |
Ciência Animal Brasileira, v. 22, e-70056, 2021. |
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ISSN: |
1809-6891 |
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DOI: |
10.1590/1809-6891v22e-70056 |
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Idioma: |
Inglês |
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Conteúdo: |
Semi-arid regions are characterized by high evapotranspiration and low rainfall, favoring the accumulation of salts when irrigated with brackish water. The aim of this study was to evaluate the effect of pearl millet cultivation with brackish water levels and fertilized with organic fertilizer on the chemical and physical properties of the soil. A split plot randomized block design was adopted, in a factorial arrangement, with three repetitions. Plots consisted of four irrigation levels (25, 50, 75 and 100% crop evapotranspiration) and subplots consisted of four levels of organic fertilizer (0; 15; 30 and 45 Mg ha-1). At the end of the pearl millet production cycle, soil was collected from layers 0-0.20 m and 0.20-0.40 m, for physical (soil bulk density, particle density and porosity) and chemical (EC, pH, K, Na, Ca, Mg, H + Al, SB, CEC, V) properties. There was no effect of interaction of brackish water levels and organic fertilizer levels on soil chemical properties. Brackish water reduced potassium on layer 0.20-0.40 m. A negative linear effect was found for density in the 0.20-0.40 m layer under different levels of organic fertilizer. Brackish water levels and organic fertilizer levels in the cultivation of pearl millet does not alter soil chemical and physical properties at the 0-0.20 m layer. However, the use of brackish water reduces the concentration of potassium in the soil and the application of organic fertilizer reduces soil density at the 0.20-0.40 m layer. |
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Palavras-Chave: |
Agricultura biossalina; Biosaline agriculture; Saturação por bases. |
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Thesagro: |
Água Salobra; Milheto; Pastagem; Pennisetum Glaucum. |
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Thesaurus NAL: |
Base saturation; Organic fertilizers. |
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Categoria do assunto: |
L Ciência Animal e Produtos de Origem Animal |
|
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1147209/1/Pearl-millet-cultivation-with-brackish-water-and-organic-fertilizeralters-soil-properties-2021.pdf
|
|
Marc: |
LEADER 02487naa a2200337 a 4500
001 2147209
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008 2021 bl uuuu u00u1 u #d
022 $a1809-6891
024 7 $a10.1590/1809-6891v22e-70056$2DOI
100 1 $aARAÚJO, C. de A.
245 $aPearl millet cultivation with brackish water and organic fertilizeralters soil properties.$h[electronic resource]
260 $c2021
520 $aSemi-arid regions are characterized by high evapotranspiration and low rainfall, favoring the accumulation of salts when irrigated with brackish water. The aim of this study was to evaluate the effect of pearl millet cultivation with brackish water levels and fertilized with organic fertilizer on the chemical and physical properties of the soil. A split plot randomized block design was adopted, in a factorial arrangement, with three repetitions. Plots consisted of four irrigation levels (25, 50, 75 and 100% crop evapotranspiration) and subplots consisted of four levels of organic fertilizer (0; 15; 30 and 45 Mg ha-1). At the end of the pearl millet production cycle, soil was collected from layers 0-0.20 m and 0.20-0.40 m, for physical (soil bulk density, particle density and porosity) and chemical (EC, pH, K, Na, Ca, Mg, H + Al, SB, CEC, V) properties. There was no effect of interaction of brackish water levels and organic fertilizer levels on soil chemical properties. Brackish water reduced potassium on layer 0.20-0.40 m. A negative linear effect was found for density in the 0.20-0.40 m layer under different levels of organic fertilizer. Brackish water levels and organic fertilizer levels in the cultivation of pearl millet does not alter soil chemical and physical properties at the 0-0.20 m layer. However, the use of brackish water reduces the concentration of potassium in the soil and the application of organic fertilizer reduces soil density at the 0.20-0.40 m layer.
650 $aBase saturation
650 $aOrganic fertilizers
650 $aÁgua Salobra
650 $aMilheto
650 $aPastagem
650 $aPennisetum Glaucum
653 $aAgricultura biossalina
653 $aBiosaline agriculture
653 $aSaturação por bases
700 1 $aLIRA, J. B. de
700 1 $aMAGALHÃES, A. L. R.
700 1 $aSILVA, T. G. F. da
700 1 $aGOIS, G. C.
700 1 $aANDRADE, A. P. de
700 1 $aARAUJO, G. G. L. de
700 1 $aCAMPOS, F. S.
773 $tCiência Animal Brasileira$gv. 22, e-70056, 2021.
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Embrapa Semiárido (CPATSA) |
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