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

•Soil texture can be detected through its emissivity spectra.•Soil emissivity decreases as sand content of the samples increases.•Laboratory and satellite sensors have distinct accuracy in soil attributes modeling.•Qualitative analyses of soil spectra reveal relevant information of its composition....

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Veröffentlicht in:Geoderma 2020-03, Vol.361, p.114038, Article 114038
Hauptverfasser: Salazar, Diego F.U., Demattê, José A.M., Vicente, Luiz E., Guimarães, Clécia C.B., Sayão, Veridiana M., Cerri, Carlos E.P., de C. Padilha, Manuela C., Mendes, Wanderson De S.
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Sprache:eng
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Zusammenfassung:•Soil texture can be detected through its emissivity spectra.•Soil emissivity decreases as sand content of the samples increases.•Laboratory and satellite sensors have distinct accuracy in soil attributes modeling.•Qualitative analyses of soil spectra reveal relevant information of its composition. 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 electromagnetic 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, São 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 (Ɛ) 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 Ɛ. 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
ISSN:0016-7061
1872-6259
DOI:10.1016/j.geoderma.2019.114038