Ls. Galvao et al., Variations in reflectance of tropical soils: Spectral-chemical compositionrelationships from AVIRIS data, REMOT SEN E, 75(2), 2001, pp. 245-255
The relationships between Airborne Visible. Infrared Imaging Spectrometer (
AVIRIS) surface reflectance values and constituents (total iron, organic ma
tter, TiO2, Al2O3, and SiO2) of samples representative of three important s
oil types from central Brazil [Terra Roxa Estruturada (S-TE), Latossolo Ver
melho-Escuro (S-LE), and Areia Quartzosa (S-AQ)] were analyzed. End member
spectra for green vegetation (GVd), nonphotosynthetic vegetation (NPV), wat
er (W), and the three soil types were selected by inspecting scatter plots
derived from the principal components analysis (PCA) of 140 AVIRIS bands. T
hey were then used to compose a six end member unmixing model to characteri
ze the spectral reflectance variations associated with the different scene
components, the spatial distribution of the soil types, and the effects of
spectral mixing on the spectral-chemical composition relationships. Finally
, regression equations fitted to soil constituents and their highly correla
ted spectral bands were used to produce maps showing the chemical variabili
ty in the scene for areas dominated by the presence of exposed soils, as in
dicated by the results from the unmixing model. The results showed a very g
ood agreement between the spatial variability of the soil types and of the
soil constituents. The largest squared correlation results were obtained fo
r Fe2O3, TiO2, and Al2O3, but the relationships were affected in the transi
tion from the red to the near-infrared interval by the presence of nonsoil
residues (e.g., senescent vegetation or litter) over the soil surfaces. In
comparison with the light and loamy sand S-AQ, the dark-red clay S-TE and S
-LE presented higher contents of Fe2O3, Al2O3, and TiO2, and consequently l
ower overall reflectance in the scene, because of the presence of greater a
mounts of opaque minerals. The prediction of these constituents from remote
sensing data and their close association with the spatial distribution of
the different soil types demonstrate the importance of the present investig
ation for soil mapping and soil erosion studies. (C) Elsevier Science Inc.,
2001. All Rights Reserved.