Remote Sensing · 2018 · 96 citations · 64 references
Natural SciencesEarth SciencesSoil SciencesRemote SensingSoil ScienceSoil SensingRemote Sensing For Soil SurveyRemote Sensing Image AnalysisRemote Sensing ImagerySoil SurveyingSoil TextureMultispectral Image AnalysisMultispectral SensingRemote Sensing Of Soil TextureRemote Sensing-based Soil MappingSoil PropertiesSoil Property EstimationSoil Texture EstimationSpectral Signatures
Soil mapping demands large-scale surveys that are costly and time consuming. It is necessary to identify strategies with reduced costs to obtain detailed information for soil mapping. We aimed to compare multispectral satellite image and relief parameters for the quantification and mapping of clay and sand contents. The Temporal Synthetic Spectral (TESS) reflectance and Synthetic Soil Image (SYSI) approaches were used to identify and characterize texture spectral signatures at the image level. Soil samples were collected (0–20 cm depth, 919 points) from an area of 14,614 km2 in Brazil for reference and model calibration. We compared different prediction approaches: (a) TESS and SYSI; (b) Relief-Derived Covariates (RDC); and (c) SYSI plus RDC. The TESS method produced highly similar behavior to the laboratory convolved data. The sandy textural class showed a greater increase in average spectral reflectance from Band 1 to 7 compared with the clayey class. The prediction using SYSI produced a better result for clay (R2 = 0.83; RMSE = 65.0 g kg−1) and sand (R2 = 0.86; RMSE = 79.9 g kg−1). Multispectral satellite images were more stable for the identification of soil properties than relief parameters.
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