A methodology to determine the chemistry and kinetics of the
multiple reactions during
geological maturation was developed, with a special emphasis on the
representation of diagenesis
and oil formation processes. The methodology combines a unique
macromolecular and kinetic
model for hydrocarbon pyrolysis, the FG-DVC (functional
groupdevolatilization, vaporization,
cross-linking) model, with a method of analysis based on
thermogravimetric analysis with Fourier
transform infrared spectroscopy (TG-FTIR). TG-FTIR pyrolysis data
from several natural
maturation series of coals and kerogens were measured, systematic
trends with the degree of
maturation were identified, and empirical processes and reaction
kinetics during maturation
necessary to induce these trends were estimated. This approach
eliminates potential inaccuracies
when extrapolating kinetic parameters obtained from laboratory
experiments to geological
conditions. The FG-DVC pyrolysis model was modified to include
these maturation processes,
with aqueous chemistry providing a guide for such modifications.
The resulting FG-DVC
maturation model was then used to predict the maturation of several
immature samples through
the well-known time/temperature history of the basin. The FG-DVC
pyrolysis model was
subsequently used to predict the open-system pyrolysis decomposition of
the predicted maturation
residues, and the predictions were compared to TG-FTIR data of the
corresponding naturally
matured samples. For most of the series investigated, the model
gave good predictions of the
variations in oxygenated gas precursors, tar
T
max, and extractable yield with maturation.
Kinetics
derived from open-system pyrolysis for bridge breaking were found to be
applicable during
maturation. However, faster kinetics were necessary to describe
the removal of oxygenated gas
precursors. In addition, the removal of methane and tar was found
to be too slow during
maturation when using open-system pyrolysis kinetics. Artificial
maturation experiments using
confined pyrolysis were also performed for comparison. While the
evolution rates, during
subsequent pyrolysis of the maturation residues, of oxygenated gas
species are different from
those obtained from samples naturally matured, the yields compare
favorably with model
predictions. The trends for pyrolysis tar and methane from
artificially matured samples are
similar to those of natural samples but suggest different
kinetics.