There are two models for interpretation of the internal structure of c
oals, One of them supposes that the coal structure is similar to the a
ctive carbons having macro- and micropores defined by Dubinin, The sec
ond model supposes that the molecules sorbed in the coal are present i
n a molecular lattice structure. The authors have measured the sorptio
n isotherms and isobars of different gases (nitrogen, methane, carbon
dioxide) in coals, They have calculated the equivalent specific surfac
e areas and their temperature dependences, The results have been compa
red to similar data calculated from methanol-water and methanol-benzen
e excess isotherms. It was found that the surface areas calculated fro
m gas sorption isotherms and metanol water excess isotherms are compar
able. From the methanol-benzene excess isotherms approximately one ord
er of magnitude higher surface areas were obtained. This finding was a
ttributed to the lamellar structure of Mecsek coal and to the intercal
ated clay minerals.