A key
factor for the petroleum potential of source rock is the
degree of chemical and physical structure evolution of its kerogen
fraction through a range of maturation processes. In this study, various
high-field, solid-state NMR methods have been applied to a series
of kerogen isolates (type I) over a defined maturity range (vitrinite
reflectance R
0 from 0.98 to 1.86%). Results
obtained from 13C MAS NMR show that the sp2/sp3-hybridized carbon ratio of kerogen, here defined as the aromatic/aliphatic
ratio, increases with increasing maturity. 1H MAS NMR spectra
contain partly overlapping aliphatic and aromatic resonances with
distinct transverse relaxation behavior. In Hahn-echo experiments,
the aromatic signal decays more slowly than the aliphatic signal,
indicating that for these systems, transverse 1H relaxation
is rather controlled by local distances between hydrogen atoms than
by molecular mobility. Similar relaxation differences are also found
in static (nonspinning) 1H Hahn-echo NMR experiments, here
used to discriminate between phases with different proton mobilities
and/or densities in the kerogen samples and, ultimately, between aromatic
and aliphatic fractions. The distributions of the static transverse
relaxation time (T
2), extracted from the
Hahn-echo decays, are characterized by a short-T
2 peak (∼10 μs) and a long-T
2 peak (∼100 μs). The ratio between these two
peaks correlates well with the aliphatic-to-aromatic signal intensity
ratios in MAS NMR spectra of the corresponding kerogen samples, suggesting
that a net decrease in kerogen proton densityoccurring during
maturationis also reflected by 1H NMR relaxation.
For the investigated kerogen isolates, the long-T
2 peak in the T
2 distribution
can be considered an indicator of aromatic content, which can be directly
detected by measuring 1H T
2 relaxation.