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| Registros recuperados : 4 | |
| 4. |  | BRELURUT, A.; LOUAULT, F.; BENOIT, M.; TOURNADRE, H.; MONTARD, F. X. de; THERIEZ, M.; LIENARD, G.; DEDIEU, B.; LAIGNEL, G. Adaptation de contuites d`elevage ovin allaitant a une diminution du chargement. Exemple en moyenne montagne. Annales de Zootechnie, v.47, n.5-6, p.483-490, 1998.| Biblioteca(s): Embrapa Caprinos e Ovinos. |
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| Registros recuperados : 4 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
10/12/2014 |
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Data da última atualização: |
10/12/2014 |
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Tipo da produção científica: |
Resumo em Anais de Congresso |
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Autoria: |
TEIXEIRA, W. |
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Afiliação: |
WENCESLAU GERALDES TEIXEIRA, CNPS. |
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Título: |
How to predict soil water holding capacity using physically based equations? |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
In: WORKSHOP ON POROUS MEDIA, 1., 2014, Rio de Janeiro. Program & abstracts. Rio de Janeiro: Instituto Nacional de Matemática Pura e Aplicada, 2014. p. 17-18. |
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Idioma: |
Inglês |
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Conteúdo: |
The soil surface and porosity govern the capacity of soil to hold water. In soil science, many functions were developed to estimate parameters of equations to describe soil water retention and soil hydraulic properties. These functions were created using statistical techniques based in soil properties parameters less laborious and cheaply obtained than the direct measurements of soil hydraulic parameters. These functions are called pedotransfer functions (PTF) and fill the gap between the available soil data and the properties required for modeling soil water fluxes. The physically based equations approach to obtain functions of water retention and hydraulic conductivity of the porous media (soils) may be advantageous, as the predictors will not be select by statistical procedures and be strongly influenced by the available data base and technique used, moreover the predictors will have also a physical meaning. Examples of physically based equations to predict soil water content in function of dielectric conductivity in soils is given and the demand of physically based equation to predict soil water hold capacity and soil hydraulic conductivity is addressed. |
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Palavras-Chave: |
Capacidade de retenção de água no solo; Equação de base física. |
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Thesagro: |
Retenção de água no solo. |
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Thesaurus NAL: |
Soil water retention. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/113440/1/Interpore-p.17-18-2014.pdf
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Marc: |
LEADER 01823nam a2200157 a 4500
001 2002101
005 2014-12-10
008 2014 bl uuuu u00u1 u #d
100 1 $aTEIXEIRA, W.
245 $aHow to predict soil water holding capacity using physically based equations?$h[electronic resource]
260 $aIn: WORKSHOP ON POROUS MEDIA, 1., 2014, Rio de Janeiro. Program & abstracts. Rio de Janeiro: Instituto Nacional de Matemática Pura e Aplicada, 2014. p. 17-18.$c2014
520 $aThe soil surface and porosity govern the capacity of soil to hold water. In soil science, many functions were developed to estimate parameters of equations to describe soil water retention and soil hydraulic properties. These functions were created using statistical techniques based in soil properties parameters less laborious and cheaply obtained than the direct measurements of soil hydraulic parameters. These functions are called pedotransfer functions (PTF) and fill the gap between the available soil data and the properties required for modeling soil water fluxes. The physically based equations approach to obtain functions of water retention and hydraulic conductivity of the porous media (soils) may be advantageous, as the predictors will not be select by statistical procedures and be strongly influenced by the available data base and technique used, moreover the predictors will have also a physical meaning. Examples of physically based equations to predict soil water content in function of dielectric conductivity in soils is given and the demand of physically based equation to predict soil water hold capacity and soil hydraulic conductivity is addressed.
650 $aSoil water retention
650 $aRetenção de água no solo
653 $aCapacidade de retenção de água no solo
653 $aEquação de base física
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Registro original: |
Embrapa Solos (CNPS) |
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