Variabilidade espacial do fósforo e das frações granulométricas de um Latossolo Vermelho Amarelo1

This study was conducted to study the spatial variability of phosphorus, estimating it through cokriging taking as covariables the size fractions of soil. The study was conducted at the experimental farm INCAPER-ES. The soil was sampled in the canopy projection of culture and depth of 0-0.20 meters...

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Detalles Bibliográficos
Autores: Silva, Samuel De Assis, Lima, Julião Soares De Souza, Souza, Gustavo Soares De, Oliveira, Rone Batista De [UNESP], Silva, Alessandra Fagioli Da [UNESP]
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2010
País:Brasil
Institución:Universidade Estadual Paulista (UNESP)
Repositorio:Repositório Institucional da UNESP
Idioma:portugués
OAI Identifier:oai:repositorio.unesp.br:11449/211909
Acceso en línea:http://dx.doi.org/10.5935/1806-6690.20100001
http://hdl.handle.net/11449/211909
Access Level:acceso abierto
Palabra clave:Geostatistics
Soils
Match content
Oxisols
Interpolation
Geoestatística
Solos
Teor de Fósforo
Latossolos
Interpolação
Descripción
Sumario:This study was conducted to study the spatial variability of phosphorus, estimating it through cokriging taking as covariables the size fractions of soil. The study was conducted at the experimental farm INCAPER-ES. The soil was sampled in the canopy projection of culture and depth of 0-0.20 meters in an irregular mesh with 109 points. The data were initially submitted to a descriptive analysis and correlation. Through geostatistics was made the adjustment of the variograms. The P showed significant correlation with the sand and clay fractions indicating that areas with higher concentrations of clay have lower availability of this nutrient. Both fractions have equal performance as co-variable in the estimate of the levels of P in the soil.