Two low-rank Turkish coals, Tunçbilek (TB) subbituminous and Göynük (GN) lignite, were
subjected to low-severity heat treatment with or without added water, under N2 or H2 atmospheres
at 285−330 °C, both as original coals and after demineralization with HCl(aq)/HF(aq) treatment.
The samples processed in H2−H2O combination seemed to be more dissociated or decomposed
than those processed in N2−H2O or under H2 without water. Gas analyses and spectroscopy of
samples clearly indicated an effect of water in enhancing decarboxylation reactions and that
oxygen rejection from the coals was mainly due to CO2 formation. Water also enhanced the
cleavage of aryl−ether bonds. These cleavage reactions are more pronounced in GN coal than in
TB coal, probably due to a higher concentration of activated ether structures in the former coal.
The disruption of noncovalent interactions is considered mainly responsible for the extensive
depolymerization of TB coal. The role of H2 in these heat treatment conditions is considered to
be predominantly hydrogenation of polyaromatic sites with the help of mineral matter and
scavenging radicals, which arose from cleavage of weak aliphatic ether bonds. The coal samples
treated in H2−H2O donated more hydrogen to anthracene during their co-pyrolysis, attributed
mainly to a reduced tendency of the treated samples to undergo radical-generating reactions.