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We have worked with three sets of data:
- In the initial phase of the work, a limited database of seven
mineral spectra was used for study, along with six author-constructed
`non-spectra'. The wavelength range of the spectra was 2.0-2.4
microns and they are sampled at 0.01 micron intervals i.e.,
there are 41 bins per spectrum.
- Laboratory-measured high-resolution ozone spectra were used for
gas samples at temperatures of 200, 220, 240, 260, 280, and 300K. The
original wavelength range of 320-337 nm was sub-sampled into 35
equally-sized bins for this study: the sampling density is not as high
as can be achieved with a high-resolution spectrometer but is
sufficient to encode the general shapes of the curves.
- In the second phase of our work, a much larger database of spectra
was obtained from J. Price of the Beltsville Agricultural Research
Center, USA. This database, which is free to all, contains spectra of
soils, both wet and dry, vegetation, at various growing stages,
man-made materials, metals and minerals. The wavelength range of the
spectra is 0.4-2.5 microns and they are sampled at 0.01 micron
intervals i.e., there are 211 bins per spectrum. The various
subsets (i.e., soils, vegetation, minerals) of this database
were examined and it was decided that the mineral subset of this
database should be used. This subset was given to Price by JPL and
consists of 160 laboratory-measured (by Beckman spectrometer)
reflectance.
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