Semigelatinous interfacial films, which may influence the fluid mechan
ic and mass transfer properties of coal tar in porous media, have been
observed to form in coal tar-water systems when coal tars are aged in
water under quiescent conditions for a few days. Samples of the inter
facial film were isolated after aging for a period of 1 year and compa
red to the bulk coal tar using GC/MS,C-13-NMR, H-1-NMR, and FTIR techn
iques. The results showed that these films were very similar in organi
c composition to the bulk coal tar with no significant enrichment, dep
letion, or polymerization of tar components. The notable difference in
the composition of the film material was the presence of water bound
to coal tar constituents by weak, reversible bonds. FTIR analysis of a
sample of coal tar film kept in contact with deuterated water showed
that the water molecules bound to the coal tar constituents would slow
ly interchange with water molecules that were not bound. Similar bondi
ng of water molecules and coal tar constituents was observed in coal t
ar-water emulsions. These results suggest that the semigelatinous film
formed at the coal tar-water interface is similar to a thin emulsion
layer.