Molecular models of vitrinites (obtained from obvious tree remains) from th
e Upper Freeport and Lewiston-Stockton coal seams are presented. Utilizing
pure telocollinite reduced the complexity of the model and resulted in more
realistic molecular structures than from whole coal analyses. The structur
es presented are in agreement with experimentally determined bulk chemical
parameters. These were easily achieved with current software and computatio
nal expense. However, it was more difficult to produce model structure's wh
ich have calculated physical parameters (of the global minimum structure de
termined from molecular mechanics and dynamics) in agreement with experimen
tally determined parameters. For these bituminous vitrinites, the addition
of physical parameters severely constrained the type of model structures th
at could be produced. The molecular structures presented are covalently lin
ked aromatic and hydroaromatic structures with a distribution of cross-link
densities. Despite being very close in maturation las determined from vitr
inite reflectance) the structural differences have a significant impact on
behavior. The current models are not yet consistent with some behavioral as
pects such as solvent swelling. It is suggested that a greater molecular sc
ale is needed before multiple facets of coals behavior can be explained.