The morphological changes in lignite coal at two different pressures, using
small angle x-ray scattering, have been investigated. All the scattering p
rofiles are interpreted in terms of surface fractal morphology. It is obser
ved that the surface fractal dimension does not change appreciably under th
e experimental pressure range, while the volume of micro-cracks and inter-p
article pore space is reduced with increasing pressure. By and large, the c
onstant value of the surface fractal dimension of all the specimens, as cal
culated from the scattering profiles, indicates that the roughness on the p
ore coal interface remains almost unaffected under the experimental pressur
e range. The validity of single scattering approximation for this experimen
t has also been confirmed by the observation of the identical nature of the
small angle scattering profiles with respect to change of wave lengths, na
mely, 0.154 nm. (Cu K-alpha) and 0.072 nm (Mo K-alpha), of the probing radi
ation. (C) 2001 Kluwer Academic Publishers.