progressive heating up to 800° C in vacuum. The infrared (IR) spectra of the residuals
obtained at 100° C intervals from room temperature to 800° C show spectral changes
ascribed to transformations at the level of the organic and inorganic components.
Comparing these results with those previously obtained by heating the same coals in the
presence of air and examining their pyridinic extracts, it appears that the Sulcis coal with …