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| 13. |  | WOLF, M. A.; ZECH, W.; SCHROTH, G. Biometrical data, biomass allocation, and nutritional data of 4-year-old Bactris gasipaes (Kunth) in an agroforestry system in central Amazonia. In: SHIFT WORKSHOP, 3., 1998, Manaus. Program, abstracts of presentations and posters... Hamburg: GKSS, 1998. p. C37.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 18. | | SCHROTH, G.; MOTA, M. do S. S. da; JEROZOLIMSKI, A. Agroforestry and the conservation on forest cover and biodiversity tropical landscapes - on-Site and of-Site effects and synergies with environmental lefislation. In: CONGRESSO BRASILEIRO DE SISTEMAS AGROFLORESTAIS, 6., 2006, Campos dos Goytacazes, RJ. Sistemas agroflorestais: bases científicas para o desenvolvimento sustentável: resumos. Campos dos Goytacazes: Universidade Estadual do Norte Fluminense Darcy Ribeiro; Salvador: Sociedade Brasileira de Sistemas Agroflorestais, 2006. p. 67-86. Editado por: GAMA-RODRIGUES, A. C. da; BARROS, N. F. de; GAMA-RODRIGUES, E. F. da; FREITAS, M. S. M.; VIANA, A. P.; JASMIN, J. M.; MARCIANO, C. R.; CARNEIRO, J. G. A.| Biblioteca(s): Embrapa Florestas. |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
18/08/2014 |
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Data da última atualização: |
06/01/2015 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
TEIXEIRA, W. G.; SCHROTH, G.; MARQUES, J. D.; HUWE, B. |
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Afiliação: |
WENCESLAU GERALDES TEIXEIRA, CNPS; Sustainable Agriculture Department, Rainforest Alliance, Wageningen, The Netherlands.; Jean Dalmo Marques, Federal Institute of Education, Science and Technology of the Amazonas – IFAM.; Bernd Huwe, Soil Physics Department, University of Bayreuth, Bayreuth, Germany. |
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Título: |
Unsaturated soil hydraulic conductivity in the central Amazon: field evaluations. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
In: TEIXEIRA, W. G.; CEDDIA, M. B.; OTTONI, M. V.; DONAGEMMA, G. K. (Ed.). Application of soil physics in environmental analyses: measuring, modelling and data integration. New York: Springer, 2014. p. 283-306. |
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Idioma: |
Inglês |
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Conteúdo: |
Determination of hydraulic properties may be required to solve many questions in agriculture and environmental research. Hydraulic properties are spatially and temporally variable, consequently, reliable soil hydraulic characterization is complex and time-consuming. Furthermore, many hydraulic properties are better represented by functions (i.e., unsaturated hydraulic conductivity and soil water retentivity) rather than by the mean values. The variability due to the presence of macropores or soil cracks commonly found in some soil classes in the tropics can enhance the naturally high soil hydraulic variability. A tension infiltrometer is an equipment that can be used to evaluate near-saturated hydraulic conductivity and sorptivity. In structured soil, small changes in soil tension, near the saturation, lead to dramatic changes of the infiltration rates. In this chapter, firstly, a discussion about soil hydraulic parameters and methods more appropriate to evaluate them on tropical soils is provided. Specific sources of errors and procedures to avoid or alleviate them are pointed out. Secondly, unsaturated hydraulic conductivity measurements carried out using a tension infiltrometer are used to compare different land use systems in the Central Amazon. The scaling theory and the statistical techniques of piecewise continuous regression are briefly described and used to analyze the results. Tension infiltrometers show to be relatively cheap, robust and a simple field method to evaluate unsaturated hydraulic conductivity in tropical soils. Since K near saturation is highly variable, the data were better analyzed using the relative hydraulic conductivity and the scaling theory. These small values of the tension in the breakpoint that divide the fluxes dominated by gravity reflect the importance to evaluate unsaturated hydraulic onductivities near saturation. MenosDetermination of hydraulic properties may be required to solve many questions in agriculture and environmental research. Hydraulic properties are spatially and temporally variable, consequently, reliable soil hydraulic characterization is complex and time-consuming. Furthermore, many hydraulic properties are better represented by functions (i.e., unsaturated hydraulic conductivity and soil water retentivity) rather than by the mean values. The variability due to the presence of macropores or soil cracks commonly found in some soil classes in the tropics can enhance the naturally high soil hydraulic variability. A tension infiltrometer is an equipment that can be used to evaluate near-saturated hydraulic conductivity and sorptivity. In structured soil, small changes in soil tension, near the saturation, lead to dramatic changes of the infiltration rates. In this chapter, firstly, a discussion about soil hydraulic parameters and methods more appropriate to evaluate them on tropical soils is provided. Specific sources of errors and procedures to avoid or alleviate them are pointed out. Secondly, unsaturated hydraulic conductivity measurements carried out using a tension infiltrometer are used to compare different land use systems in the Central Amazon. The scaling theory and the statistical techniques of piecewise continuous regression are briefly described and used to analyze the results. Tension infiltrometers show to be relatively cheap, robust and a simple field method to e... Mostrar Tudo |
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Palavras-Chave: |
Agroforestry system; Amazon; Bactris gassipaes; Ferralsol; Infiltration; Peach palm; Piecewise equation; Scaling; Tension infiltrometer. |
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Thesagro: |
Theobroma Grandiflorum. |
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Thesaurus NAL: |
saturated hydraulic conductivity; soil water content; unsaturated hydraulic conductivity. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02954naa a2200313 a 4500
001 1992789
005 2015-01-06
008 2014 bl uuuu u00u1 u #d
100 1 $aTEIXEIRA, W. G.
245 $aUnsaturated soil hydraulic conductivity in the central Amazon$bfield evaluations.$h[electronic resource]
260 $c2014
520 $aDetermination of hydraulic properties may be required to solve many questions in agriculture and environmental research. Hydraulic properties are spatially and temporally variable, consequently, reliable soil hydraulic characterization is complex and time-consuming. Furthermore, many hydraulic properties are better represented by functions (i.e., unsaturated hydraulic conductivity and soil water retentivity) rather than by the mean values. The variability due to the presence of macropores or soil cracks commonly found in some soil classes in the tropics can enhance the naturally high soil hydraulic variability. A tension infiltrometer is an equipment that can be used to evaluate near-saturated hydraulic conductivity and sorptivity. In structured soil, small changes in soil tension, near the saturation, lead to dramatic changes of the infiltration rates. In this chapter, firstly, a discussion about soil hydraulic parameters and methods more appropriate to evaluate them on tropical soils is provided. Specific sources of errors and procedures to avoid or alleviate them are pointed out. Secondly, unsaturated hydraulic conductivity measurements carried out using a tension infiltrometer are used to compare different land use systems in the Central Amazon. The scaling theory and the statistical techniques of piecewise continuous regression are briefly described and used to analyze the results. Tension infiltrometers show to be relatively cheap, robust and a simple field method to evaluate unsaturated hydraulic conductivity in tropical soils. Since K near saturation is highly variable, the data were better analyzed using the relative hydraulic conductivity and the scaling theory. These small values of the tension in the breakpoint that divide the fluxes dominated by gravity reflect the importance to evaluate unsaturated hydraulic onductivities near saturation.
650 $asaturated hydraulic conductivity
650 $asoil water content
650 $aunsaturated hydraulic conductivity
650 $aTheobroma Grandiflorum
653 $aAgroforestry system
653 $aAmazon
653 $aBactris gassipaes
653 $aFerralsol
653 $aInfiltration
653 $aPeach palm
653 $aPiecewise equation
653 $aScaling
653 $aTension infiltrometer
700 1 $aSCHROTH, G.
700 1 $aMARQUES, J. D.
700 1 $aHUWE, B.
773 $tIn: TEIXEIRA, W. G.; CEDDIA, M. B.; OTTONI, M. V.; DONAGEMMA, G. K. (Ed.). Application of soil physics in environmental analyses: measuring, modelling and data integration. New York: Springer, 2014. p. 283-306.
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