Emissivity of agricultural soil attributes in southeastern Brazil via terrestrial and satellite sensors

Autor(es)

Salazar, Diego F. U. ^[1] ; Dematte, Jose A. M. ^[1] ; Vicente, Luiz E. ^[2] ; Guimaraes, Clecia C. B. ^[1] ; Sayao, Veridiana M. ^[1] ; Cerri, Carlos E. P. ^[1] ; Padilha, Manuela C. de C. ^[1] ; Mendes, Wanderson De S. ^[1]

Afiliação do(s) autor(es)

^[1] Univ Sao Paulo, Coll Agr Luiz de Queiroz, Dept Soil Sci, Av Padua Dias, 11 Piracicaba, Cx Postal 09, BR-13416900 Sao Paulo - Brazil

^[2] Embrapa Enviroment, Low Carbon Agr Platform, Cx Postal 69, BR-13820000 Sao Paulo - Brazil

• Tipo de documento: Artigo Científico
• Fonte: Geoderma; v. 361, MAR 1 2020.
• Citações Web of Science: 2

Resumo

Soil texture and organic carbon (OC) content influence the spectral response. These attributes are relevant for the preservation and proper management of land use in the pursuit of a sustainable agriculture. Laboratory and satellite sensors have been applied as a powerful tool for studying so is, but their analysis using these sensors has mainly focused on the visible (Vis), near infrared (NIR) and shortwave infrared (SWIR) regions of the electro-magnetic spectrum, with few studies in the Medium Infrared (MIR). The aim of this study was to identify the spectral pattern of soils with different granulometry (sand and clay) and OC content using laboratory and satellite sensors in the MIR region, specifically in the Thermal Infrared (TIR) range (ASTER, Landsat satellites). The study performed qualitative and quantitative analyses of clay, OC and sand fractions (fine and coarse). The study area is located in the region of Piracicaba, Sao Paulo, Brazil, where collected 150 soil samples (0-20 cm depth). Soil texture was determined by the pipette method and OC via dry combustion. Reflectance and emissivity (epsilon) spectral data were obtained with the Fourier Transform Infrared (FT-IR) Alpha sensor (Bruker Optics Corporation). An image ``ASTER 05{''} from July 15, 2017 was acquired with values of epsilon. Samples were separated by textural classes and the spectral behavior in the TIR region was described. The data obtained by the laboratory sensor were resampled to the satellite sensor bands. The behavior between spectra of both sensors was similar and had significant correlation with the studied attributes, mainly sand. For the partial least squares regression (PLSR) models, six strategies were used (MIR, MIR\_ASTER, ASTER, TIR, TIR Correlation Index (TIR\_CID), and MIR Correlation Index (MIR\_CID)), which consisted in the use of all sensors bands, or by the selection of bands that presented the most significant correlations with each one of the attributes. Models presented a good performance in the prediction of all attributes using the whole MIR. In the TIR region, the models for total sand content and for fine and coarse fractions were good. Models created with ASTER sensor data were not as promising as those with laboratory ones. The use of specific bands was useful in estimating some attributes in the MIR and TIR, improving the predictive performance and validation of models. Therefore, the discrimination of soil attributes with satellite sensors can be improved with the identification of specific bands, as observed in the results with laboratory sensors. (AU)

• Processo FAPESP: 14/22262-0 - Geotecnologias no mapeamento digital pedológico detalhado e biblioteca espectral de solos do Brasil: desenvolvimento e aplicações
• Beneficiário: José Alexandre Melo Demattê
• Modalidade de apoio: Auxílio à Pesquisa - Temático