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| 144. |  | ANTONINI, J. C. dos A.; SILVA, E. M. DA; GRIEBELER, N. P.; SANO, E. E. Spatio-temporal modelling of the duration of the cotton cycle in the state of Goiás, Brazil. Engenharia Agrícola, Jaboticabal, v. 31, n. 4, p. 652-662, jul./ago. 2011.| Biblioteca(s): Embrapa Cerrados. |
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| 152. | | SILVA, E. M. da; LIMA, J. E. F. W.; AZEVEDO, J. A. de; RODRIGUES, L. N. Valores de tensão na determinação da curva de retenção de água de solos do Cerrado. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 41, n. 2, p. 323-330, fev. 2006 Título em inglês: Tension values to describe soil-water retention curve on Cerrado soils.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 154. | | LIMA, J. E. F. W.; SILVA, E. M. da; AZEVEDO, J. A. de. Uso racional da água na agricultura. In: PARRON, L. M.; AGUIAR, L. M. de S.; DUBOC, E.; OLIVEIRA-FILHO, E. C.; CAMARGO, A. J. A. de; AQUINO, F. de G. (Ed.). Cerrado: desafios e oportunidades para o desenvolvimento sustentável. Planaltina, DF: Embrapa Cerrados, 2008. cap. 3, p. 63-94.| Biblioteca(s): Embrapa Cerrados. |
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| 156. | | SANTOS, G. G.; SILVA, E. M. da; MARCHÃO, R. L.; SILVEIRA, P. M. da; BRUAND, A.; JAMES, F.; BECQUER, T. Analysis of physical quality of soil using the water retention curve: validity of the S-index. Comptes Rendus Géoscience, Paris, v. 343, n. 4, p. 295-301, April 2011.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 157. | | SANTOS, G. G.; SILVA, E. M. da; MARCHÃO, R. L.; SILVEIRA, P. M. da; BRUAND, A.; JAMES, F.; BECQUER, T. Analysis of physical quality of soil using the water retention curve: validity of the S-index. Comptes Rendus Geoscience, Paris, v. 343, n. 4, p. 295-301, April 2011.| Biblioteca(s): Embrapa Cerrados. |
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| 159. | | RIBEIRO, A. A.; SIMEÃO, M.; SANTOS, A. R. B.; SILVA, E. M. da; ANDRADE JUNIOR, A. S. de. Balanço hídrico climatológico para o município de Bom Jesus, Piauí. In: ENCONTRO MULTIDISCIPLINAR DO CPCE, 1.; SEMINÁRIO DE PÓS-GRADUAÇÃO DA UFPI, 1., 2014, Bom Jesus. Bom Jesus, PI: UFPI, 2014.| Biblioteca(s): Embrapa Meio-Norte. |
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Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
|
Data corrente: |
28/01/2008 |
|
Data da última atualização: |
23/11/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
Internacional - C |
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Autoria: |
GARCIA-MONTIEL, D. C.; COE, M. T.; CRUZ, M. P.; FERREIRA, J. N.; SILVA, E. M. da. |
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Afiliação: |
Diana C. Garcia-Montiel, UNB; Michael T. Coe, The woods Hole Research Center; Meyr P. Cruz, UNB; JOICE NUNES FERREIRA, CPATU; Euzebio M. da Silva, CPAC. |
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Título: |
Estimating seasonal changes in volumetric soil water content at landscape scales in a savanna ecosystem using two-dimensional resistivity profiling. |
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Ano de publicação: |
2008 |
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Fonte/Imprenta: |
Earth Interactions, v. 12, n. 2, p. 1-25, Mar. 2008. |
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DOI: |
http://dx.doi.org/10.1175/2007EI238.1 |
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Idioma: |
Inglês |
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Conteúdo: |
Water distributed in deep soil reservoirs is an important factor determining the ecosystem structure of water-limited environments, such as the seasonal tropical savannas of South America. In this study a two-dimensional (2D) geoelectrical profiling technique was employed to estimate seasonal dynamics of soil water content to 10-m depth along transects of 275 m in savanna vegetation during the period between 2002 and 2006. Methods were developed to convert resistivity values along these 2D resistivity profiles into volumetric water content (VWC) by soil depth. The 2D resistivity profiles revealed the following soil and aquifer structure characterizing the underground environment: 0?4 m of permanently unsaturated and seasonally droughty soil, less severely dry unsaturated soil at about 4?7 m, nearly permanently saturated soil between 7 and 10 m, mostly impermeable saprolite interspaced with fresh bedrock of parent material at about 10?30 m, and a region of highly conductive water-saturated material at 30 m and below. Considerable spatial variation of these relative depths is clearly demonstrated along the transects. Temporal dynamics in VWC indicate that the active zone of water uptake is predominantly at 0?7 m, and follows the seasonal cycles of precipitation and evapotranspiration. Uptake from below 7 m may have been critical for a short period near the beginning of the rainy season, although the seasonal variations in VWC in the 7?10-m layer are relatively small and lag the surface water recharge for about 6 months. Calculations using a simple 1-box water balance model indicate that average total runoff was 15?25 mm month?1 in the wet season and about 6?9 mm month?1 in the dry season. Modeled ET was about 75?85 mm month?1 in the wet season and 20?25 mm month?1 in the dry season. Variation in basal area and tree density along one transect was positively correlated with VWC of the 0?3-m and 0?7-m soil depths, respectively, during the wettest months. These multitemporal measurements demonstrate that the along-transect spatial differences in soil moisture are quasi-permanent and influence vegetation structure at the scale of tens to hundreds of meters. MenosWater distributed in deep soil reservoirs is an important factor determining the ecosystem structure of water-limited environments, such as the seasonal tropical savannas of South America. In this study a two-dimensional (2D) geoelectrical profiling technique was employed to estimate seasonal dynamics of soil water content to 10-m depth along transects of 275 m in savanna vegetation during the period between 2002 and 2006. Methods were developed to convert resistivity values along these 2D resistivity profiles into volumetric water content (VWC) by soil depth. The 2D resistivity profiles revealed the following soil and aquifer structure characterizing the underground environment: 0?4 m of permanently unsaturated and seasonally droughty soil, less severely dry unsaturated soil at about 4?7 m, nearly permanently saturated soil between 7 and 10 m, mostly impermeable saprolite interspaced with fresh bedrock of parent material at about 10?30 m, and a region of highly conductive water-saturated material at 30 m and below. Considerable spatial variation of these relative depths is clearly demonstrated along the transects. Temporal dynamics in VWC indicate that the active zone of water uptake is predominantly at 0?7 m, and follows the seasonal cycles of precipitation and evapotranspiration. Uptake from below 7 m may have been critical for a short period near the beginning of the rainy season, although the seasonal variations in VWC in the 7?10-m layer are relatively small and lag th... Mostrar Tudo |
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Thesagro: |
Água; Cerrado; Ecossistema. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02895naa a2200217 a 4500
001 1409265
005 2022-11-23
008 2008 bl uuuu u00u1 u #d
024 7 $ahttp://dx.doi.org/10.1175/2007EI238.1$2DOI
100 1 $aGARCIA-MONTIEL, D. C.
245 $aEstimating seasonal changes in volumetric soil water content at landscape scales in a savanna ecosystem using two-dimensional resistivity profiling.$h[electronic resource]
260 $c2008
520 $aWater distributed in deep soil reservoirs is an important factor determining the ecosystem structure of water-limited environments, such as the seasonal tropical savannas of South America. In this study a two-dimensional (2D) geoelectrical profiling technique was employed to estimate seasonal dynamics of soil water content to 10-m depth along transects of 275 m in savanna vegetation during the period between 2002 and 2006. Methods were developed to convert resistivity values along these 2D resistivity profiles into volumetric water content (VWC) by soil depth. The 2D resistivity profiles revealed the following soil and aquifer structure characterizing the underground environment: 0?4 m of permanently unsaturated and seasonally droughty soil, less severely dry unsaturated soil at about 4?7 m, nearly permanently saturated soil between 7 and 10 m, mostly impermeable saprolite interspaced with fresh bedrock of parent material at about 10?30 m, and a region of highly conductive water-saturated material at 30 m and below. Considerable spatial variation of these relative depths is clearly demonstrated along the transects. Temporal dynamics in VWC indicate that the active zone of water uptake is predominantly at 0?7 m, and follows the seasonal cycles of precipitation and evapotranspiration. Uptake from below 7 m may have been critical for a short period near the beginning of the rainy season, although the seasonal variations in VWC in the 7?10-m layer are relatively small and lag the surface water recharge for about 6 months. Calculations using a simple 1-box water balance model indicate that average total runoff was 15?25 mm month?1 in the wet season and about 6?9 mm month?1 in the dry season. Modeled ET was about 75?85 mm month?1 in the wet season and 20?25 mm month?1 in the dry season. Variation in basal area and tree density along one transect was positively correlated with VWC of the 0?3-m and 0?7-m soil depths, respectively, during the wettest months. These multitemporal measurements demonstrate that the along-transect spatial differences in soil moisture are quasi-permanent and influence vegetation structure at the scale of tens to hundreds of meters.
650 $aÁgua
650 $aCerrado
650 $aEcossistema
700 1 $aCOE, M. T.
700 1 $aCRUZ, M. P.
700 1 $aFERREIRA, J. N.
700 1 $aSILVA, E. M. da
773 $tEarth Interactions$gv. 12, n. 2, p. 1-25, Mar. 2008.
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