AVIRIS (Airborne Visible/Infrared Imaging Spectrometer) data collected in B
razil were used for the spectral characterization of a typical crop-pasture
scene, and for the evaluation of the Spectral Feature Fitting (SFF) techni
que for clay mineral identification in the image. A six-endmember linear sp
ectral unmixing model was applied, consisting of green and senescent vegeta
tion, water, and the soils Alfisol, Oxisol and Entisol. For mineral identif
ication of kaolinite, montmorillonite and gibbsite in the AVIRIS image, ref
erence spectra from the JPL/NASA spectral library were selected. Pixel and
reference spectra were normalized by the continuum removal method, in the 2
,100-2,330 nm interval, and then compared by the use of the SFF technique.
Kaolinite is the dominant mineral in the scene, whose identification is dep
endent on the soil type and on the spectral mixture at sub-pixel level. The
best results were obtained for soils with intermediate to high overall ref
lectance and for pixels with soil abundance values greater than 70%, due, r
espectively, to the lower amount of opaque substances of these soils and to
the reduction of spectral effects of the lignin-cellulose features. These
factors tend to obliterate the absorption bands of clay minerals.