Use este identificador para citar ou linkar para este item: http://repositorio.ufla.br/jspui/handle/1/45907
Título: Funções de pedotransferência para retenção de água nos principais solos dos tabuleiros costeiros brasileiros
Título(s) alternativo(s): Funções de pedotransferência para retenção de água nos principais solos dos tabuleiros costeiros brasileiros
Palavras-chave: Banco de dados
Funções de pedotransferência
Ponto de murcha permanente
Database
Permanent wilting point
Field capacity
Data do documento: Jul-2015
Editor: Editora da Universidade Federal de Lavras
Citação: SILVA, E. da et al. Funções de pedotransferência para retenção de água nos principais solos dos tabuleiros costeiros brasileiros. Ciência e Agrotecnologia, Lavras, v. 39, n. 4, p. 331-338, jul./ago. 2015.
Resumo: Pedotransfer functions (PTFs) are equations used to estimate soil characteristics difficult to determine from other easily obtained ones. Water retention in soil is used in several agronomic and environmental applications, but its direct determination is time consuming and onerous, therefore PTFs are alternatives to obtaining this information more quickly and economically. The aims of this study were to generate a database and develop PTFs for water retention at potentials of -33 kPa (field capacity) and -1500 kPa (permanent wilting point) for Yellow Argisol and Yellow Latosol from the Brazilian Coastal Plains region. The Coastal Plains soils are mostly developed from Barreiras formation (pre-weathered sediments) and their main uses are sugarcane, livestock, forestry and fruticulture. The database to generate the PTFs was composed from the selection of information derived from scientific works and soil survey reports of the region. Specific PTFs were generated for each soil class, in their respective A and B horizons and for solum, through multiple regression by stepwise package of R language programming. Due to the small pedological variability (small number of soil classes containing great geographical expression) and mineralogical uniformity, usually observed in this environment, non-stratification of soil classes to create general PTFs presented similar or superior results compared to equations for each soil class. The adjustment of data demonstrated that water retention values at -33 kPa and -1500 kPa potentials can be estimated with adequate accuracy for the main soils of the Brazilian Coastal Plains through PTFs mainly from particle size distribution and secondarily from organic matter data.
URI: http://repositorio.ufla.br/jspui/handle/1/45907
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