SPATIAL VARIABILITY OF SOIL MOISTURE AND ELECTRICAL CONDUCTIVITY IN AN ALLUVIAL VALLEY USING GEOPHYSICAL TECHNIQUES

• Autor(es): Lins, Frederico Abraão Costa ; Lopes, Iug ; Montenegro, Abelardo Antônio de Assunção
• Data: 2020
• Origem: Oasisbr
• Tipo de Documento: Artigo científico
• Idioma: Português

Descrição

The methods of electromagnetic induction in precision agriculture have high potential in applications aimed at studying the spatial variability of soil salinity and moisture. The objective of this paper was to verify the performance of EM38® in an alluvial valley in the semiarid region for the purpose of application for precision agriculture, and to evaluate the dynamics and spatial dependence of soil moisture and electrical conductivity at different depths along the profile. The study area is located in the municipality of Parnamirim, Pernambuco State, on the Advanced Campus of Irrigated Agriculture in Parnamirim from the Federal Rural University of Pernambuco. Two regular meshes were adopted, one of 10 x 10 m for measuring the apparent soil electrical conductivity (ECa) estimated with the EM38® device and another of 20 x 10 m for soil sampling, to determine soil moisture, salinity, silt and clay contents in the 0-0.3 m, 0.3-0.6 m and 0.6-0.9 m layers. Direct and indirect information was used in geostatistical analysis, construction of semivariograms and map kriging. The Degree of Spatial Dependence of the evaluated attributes varied from strong to moderate. Higher soil moisture in the deepest layer was found, whereas the highest ECa was found in the 0.3-0.6 m layer. The EM38® proved to be efficient in estimating the soil electrical conductivity, and enabled the validation of a previously calibrated regression model for the same area, in a period of soil water restriction.

The methods of electromagnetic induction in precision agriculture have high potential in applications aimed at studying the spatial variability of soil salinity and moisture. The objective of this paper was to verify the performance of EM38® in an alluvial valley in the semiarid region for the purpose of application for precision agriculture, and to evaluate the dynamics and spatial dependence of soil moisture and electrical conductivity at different depths along the profile. The study area is located in the municipality of Parnamirim, Pernambuco State, on the Advanced Campus of Irrigated Agriculture in Parnamirim from the Federal Rural University of Pernambuco. Two regular meshes were adopted, one of 10 x 10 m for measuring the apparent soil electrical conductivity (ECa) estimated with the EM38® device and another of 20 x 10 m for soil sampling, to determine soil moisture, salinity, silt and clay contents in the 0-0.3 m, 0.3-0.6 m and 0.6-0.9 m layers. Direct and indirect information was used in geostatistical analysis, construction of semivariograms and map kriging. The Degree of Spatial Dependence of the evaluated attributes varied from strong to moderate. Higher soil moisture in the deepest layer was found, whereas the highest ECa was found in the 0.3-0.6 m layer. The EM38® proved to be efficient in estimating the soil electrical conductivity, and enabled the validation of a previously calibrated regression model for the same area, in a period of soil water restriction.

Os métodos de indução eletromagnética na agricultura de precisão possuem alto potencial em aplicações voltadas para estudos da variabilidade espacial da salinidade e umidade do solo. O objetivo deste trabalho foi verificar o desempenho do EM38® em vale aluvial no semiárido para fins de aplicação de agricultura de precisão, e avaliar a dinâmica e dependência espacial da umidade e da condutividade elétrica em diferentes profundidades do solo. A área de estudo está localizada no município de Parnamirim, Pernambuco, no Campus Avançado de Agricultura Irrigada de Parnamirim da Universidade Federal Rural de Pernambuco. Duas malhas regulares foram adotadas, uma de 10 x 10 m para amostragem de condutividade elétrica aparente do solo (CEa) estimada com o aparelho EM38® e outra de 20 x 10 m para amostragem de solo, para determinação da umidade, salinidade, silte e argila nas camadas de 0-0,3 m, 0,3-0,6 m e 0,6-0,9 m. Informações diretas e indiretas foram utilizadas nas análises geoestatísticas, construção de semivariogramas e krigagem de mapas. O Grau de Dependência Espacial dos atributos avaliados variou entre forte e moderado. Maior umidade na camada mais profunda do solo foi constatada, as maiores CEa foram encontradas na camada 0,3-0,6 m. O EM38® mostrou-se eficiente na estimativa da condutividade elétrica do solo, e possibilitou a validação de modelo de regressão previamente calibrado na mesma área, em período com restrição hídrica no solo.