3.9 Article

Spectral Mixture Modeling of an ASTER Bare Soil Synthetic Image Using a Representative Spectral Library to Map Soils in Central-Brazil

Journal

AGRIENGINEERING
Volume 5, Issue 1, Pages 156-172

Publisher

MDPI
DOI: 10.3390/agriengineering5010011

Keywords

soil classification; pedology; reflectance spectroscopy; MESMA algorithm

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Pedological maps in suitable scales are scarce in most countries due to high surveying costs. This study aimed to develop a digital soil map by extrapolating multispectral data from a source area to a target area using the ASTER time series modeling technique. The soil profiles were analyzed and classified, and the soil spectra were interpreted to identify typical features of tropical soils. Cluster analysis grouped the soil spectra by soil texture, forming a spectral library. The ASTER time series was processed to generate a bare soil synthetic image, and the spectral library was modeled on the synthetic image to create a digital soil map.
Pedological maps in suitable scales are scarce in most countries due to the high costs involved in soil surveying. Therefore, methods for surveying and mapping must be developed to overpass the cartographic material obtention. In this sense, this work aims at assessing a digital soil map (DSM) built by multispectral data extrapolation from a source area to a target area using the ASTER time series modeling technique. For that process, eight representative toposequences were established in two contiguous micro-watersheds, with a total of 42 soil profiles for analyses and classification. We found Ferralsols, Plinthosols, Regosols, and a few Cambisols, Arenosols, Gleisols, and Histosols, typical of tropical regions. In the laboratory, surface soil samples were submitted to spectral readings from 0.40 mu m to 2.50 mu m. The soil spectra were morphologically interpreted, identifying shapes and main features typical of tropical soils. Soil texture grouped the curves by cluster analysis, forming a spectral library (SL). In parallel, an ASTER time series (2001, 2004, and 2006) was processed, generating a bare soil synthetic soil image (SySI) covering 39.7% of the target area. Multiple Endmember Spectral Mixture Analysis modeled the SL on the SySI generating DSM with 73% of Kappa index, in which identified about 77% is covered by rhodic Ferralsols. Besides the overestimation, the DSM represented the study area's pedodiversity. Given the discussion raised, we consider including subsoil data and other features using other sensors in operations modeled by machine learning algorithms to improve results.

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