The changes in radical concentrations and species brought about by vac
uum and gas flow drying of New Vale lignite and Stockton bituminous co
al samples were studied. Vacuum drying produces a sudden increase in c
oncentration, flow drying a more gradual but ultimately greater one. F
or both coals the changes depend on a balance between decarboxylation,
which produces new radical sites, and removal of moisture from hetero
atomic sites within the coal macrostructure. This balance is influence
d by the drying method used. Exposure of dried samples to dry air prod
uces changes in radical concentration consistent with the findings of
previous oxidation studies of these coals.