The small angle X-ray scattering (SAXS) technique was used to determin
e the pore size distributions of some coals from western Canada and th
eir resulting chars. Chars were prepared by pyrolysis at 930 degrees C
in nitrogen until no further volatile matter was evolved. The distrib
ution peak of the minerals was identified by acid treatment. Assuming
that minerals dispersed in carbonaceous medium are not subject to sint
ering during pyrolysis, the mineral distribution peak was used as the
internal standard to convert each pore size distribution of a coal sam
ple and its char to the same scale. In this way, the changes in pore s
ize distribution that occur during pyrolysis were compared. It was fou
nd that for highly reactive chars from low rank coal samples, the tota
l pore volumes increased on pyrolysis. For poorly reactive chars from
high rank coals, however, the total pore volumes decreased from their
original coal counterparts.