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| Registros recuperados : 16 | |
| 2. |  | COELHO, E. F.; COELHO FILHO, M. A.; MAGALHAES, A. F. de J.; OLIVEIRA, A. S. de. Irrigação e fertirrigação na cultura de citros. In: SOUSA, V. F. de; MAROUELLI, W. A.; COELHO, E. F.; PINTO, J. M.; COELHO FILHO, M. A. (Ed.). Irrigação e fertirrigação em fruteiras e hortaliças. Brasília, DF: Embrapa Informação Tecnológica, 2011. Cap. 14, p. 413-439.| Biblioteca(s): Embrapa Mandioca e Fruticultura. |
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| 3. | | OLIVEIRA, A. S. de; COELHO FILHO, M. A.; COELHO, E. F.; PAZ, V. P. da S. Irrigação em fruticultura. In: SANTOS-SEREJO, J. A. dos; DANTAS, J. L. L.; SAMPAIO, C. V.; COELHO, Y. da S. (Ed.). Fruticultura tropical: espécies regionais e exóticas. Brasília, DF: Embrapa Informação Tecnológica, 2009. p. 45-58.| Biblioteca(s): Embrapa Mandioca e Fruticultura. |
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| 8. | | MAROUELLI, W. A.; OLIVEIRA, A. S. de; COELHO, E. F.; NOGUEIRA, L. C.; SOUSA, V. F. de. Manejo da água de irrigação. In: SOUSA, V. F. de; MAROUELLI, W. A.; COELHO, E. F.; PINTO, J. M.; COELHO FILHO, M. A. (Ed.). Irrigação e fertirrigação em fruteiras e hortaliças. Brasília, DF: Embrapa Informação Tecnológica, 2011. Cap. 5, p. 158-232.| Biblioteca(s): Embrapa Cocais; Embrapa Hortaliças; Embrapa Mandioca e Fruticultura. |
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| 10. | | BORGES, V. P.; OLIVEIRA, A. S. de; COELHO FILHO, M. A.; SILVA, T. S. M. da; PAMPONET, B. M. Avaliação de modelos de estimativa da radiação solar incidente em Cruz das Almas, Bahia. Revista Brasileira de Engenharia Agrícola e Ambiental, v.14, n.1, p. 74–80, jan., 2010.| Biblioteca(s): Embrapa Algodão; Embrapa Mandioca e Fruticultura. |
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| 14. | | SILVEIRA, F. G. F. da; SOUZA, L. da S.; OLIVEIRA, A. S. de; SOUZA, L. D.; PEREIRA, F. A. de C.; SILVA, F. T. dos S. Redistribuição da água e capacidade de campo em latossolo amarelo distrocoeso, em Cruz das Almas, Bahia. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 33., 2011, Uberlândia. Solos nos biomas brasileiros: sustentabilidade e mudanças climáticas: anais. Uberlândia: SBCS; UFU; ICIAG, 2011. 1 CD-ROM.| Biblioteca(s): Embrapa Mandioca e Fruticultura. |
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| 15. | | FARIAS, P. dos S. de; SOUZA, L. da S.; PAIVA, A. DE Q.; OLIVEIRA, Á. S. de; SOUZA, L. D.; LEDO, C. A. da S. Hourly, daily, and monthly soil temperature fluctuations in a drought tolerant crop. Revista Brasileira de Ciência do Solo, v. 42, e0170221, 2018.| Biblioteca(s): Embrapa Mandioca e Fruticultura. |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Mandioca e Fruticultura. Para informações adicionais entre em contato com cnpmf.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Mandioca e Fruticultura. |
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Data corrente: |
19/09/2018 |
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Data da última atualização: |
21/09/2018 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
FARIAS, P. dos S. de; SOUZA, L. da S.; PAIVA, A. DE Q.; OLIVEIRA, Á. S. de; SOUZA, L. D.; LEDO, C. A. da S. |
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Afiliação: |
POLIANNA DOS SANTOS DE FARIAS, UFRB; LUCIANO DA SILVA SOUZA, UFRB; ARLICÉLIO DE QUEIROZ PAIVA, UESC; ÁUREO SILVA DE OLIVEIRA, UFRB; LAERCIO DUARTE SOUZA, CNPMF; CARLOS ALBERTO DA SILVA LEDO, CNPMF. |
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Título: |
Hourly, daily, and monthly soil temperature fluctuations in a drought tolerant crop. |
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Ano de publicação: |
2018 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, v. 42, e0170221, 2018. |
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ISSN: |
1806-9657 |
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DOI: |
10.1590/18069657rbcs20170221 |
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Idioma: |
Inglês |
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Conteúdo: |
Soil temperature is a physical property of great agricultural importance in the soil-plant relationship and in energy exchange with the atmosphere. This study was conducted in a degraded Cambissolo Háplico Ta Eutrófico (Cambisol; Inceptisol) in the Irecê Identity Territory, Bahia, Brazil, aiming to evaluate the hourly, daily, and monthly fluctuations of soil temperature at depth, and soil thermal diffusivity in the castor bean crop. Hourly soil temperature data from February 4, 2014, to September 30, 2015, were obtained by using thermocouple sensors (copper-constantan) horizontally installed at 0.05, 0.10, and 0.20 m depths. Soil thermal diffusivity was estimated by phase and amplitude methods. Results showed that, for most days, the soil temperature was at the level recommended for castor bean. The maximum and minimum hourly and daily soil temperatures were observed in October and July, respectively, and the maximum soil temperature values occurred at 4 p.m. (0.05 m), 5 p.m. (0.10 m), and 7 p.m. (0.20 m). Soil temperature variability is low, requiring few measurement points to estimate this factor in an area. The amplitude method led to soil thermal diffusivity values compatible with results in the literature. The absence of a relationship between thermal diffusivity and soil moisture was attributed to the clay-loam soil texture, predominance of micropores, and iron oxides allowing greater approximation to the soil particles, with high thermal diffusivity even under low soil moisture conditions. MenosSoil temperature is a physical property of great agricultural importance in the soil-plant relationship and in energy exchange with the atmosphere. This study was conducted in a degraded Cambissolo Háplico Ta Eutrófico (Cambisol; Inceptisol) in the Irecê Identity Territory, Bahia, Brazil, aiming to evaluate the hourly, daily, and monthly fluctuations of soil temperature at depth, and soil thermal diffusivity in the castor bean crop. Hourly soil temperature data from February 4, 2014, to September 30, 2015, were obtained by using thermocouple sensors (copper-constantan) horizontally installed at 0.05, 0.10, and 0.20 m depths. Soil thermal diffusivity was estimated by phase and amplitude methods. Results showed that, for most days, the soil temperature was at the level recommended for castor bean. The maximum and minimum hourly and daily soil temperatures were observed in October and July, respectively, and the maximum soil temperature values occurred at 4 p.m. (0.05 m), 5 p.m. (0.10 m), and 7 p.m. (0.20 m). Soil temperature variability is low, requiring few measurement points to estimate this factor in an area. The amplitude method led to soil thermal diffusivity values compatible with results in the literature. The absence of a relationship between thermal diffusivity and soil moisture was attributed to the clay-loam soil texture, predominance of micropores, and iron oxides allowing greater approximation to the soil particles, with high thermal diffusivity even under low soi... Mostrar Tudo |
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Thesagro: |
Solo. |
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Thesaurus NAL: |
Soil. |
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Categoria do assunto: |
-- |
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Marc: |
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100 1 $aFARIAS, P. dos S. de
245 $aHourly, daily, and monthly soil temperature fluctuations in a drought tolerant crop.$h[electronic resource]
260 $c2018
520 $aSoil temperature is a physical property of great agricultural importance in the soil-plant relationship and in energy exchange with the atmosphere. This study was conducted in a degraded Cambissolo Háplico Ta Eutrófico (Cambisol; Inceptisol) in the Irecê Identity Territory, Bahia, Brazil, aiming to evaluate the hourly, daily, and monthly fluctuations of soil temperature at depth, and soil thermal diffusivity in the castor bean crop. Hourly soil temperature data from February 4, 2014, to September 30, 2015, were obtained by using thermocouple sensors (copper-constantan) horizontally installed at 0.05, 0.10, and 0.20 m depths. Soil thermal diffusivity was estimated by phase and amplitude methods. Results showed that, for most days, the soil temperature was at the level recommended for castor bean. The maximum and minimum hourly and daily soil temperatures were observed in October and July, respectively, and the maximum soil temperature values occurred at 4 p.m. (0.05 m), 5 p.m. (0.10 m), and 7 p.m. (0.20 m). Soil temperature variability is low, requiring few measurement points to estimate this factor in an area. The amplitude method led to soil thermal diffusivity values compatible with results in the literature. The absence of a relationship between thermal diffusivity and soil moisture was attributed to the clay-loam soil texture, predominance of micropores, and iron oxides allowing greater approximation to the soil particles, with high thermal diffusivity even under low soil moisture conditions.
650 $aSoil
650 $aSolo
700 1 $aSOUZA, L. da S.
700 1 $aPAIVA, A. DE Q.
700 1 $aOLIVEIRA, Á. S. de
700 1 $aSOUZA, L. D.
700 1 $aLEDO, C. A. da S.
773 $tRevista Brasileira de Ciência do Solo$gv. 42, e0170221, 2018.
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