Solid-state
nuclear magnetic resonance (NMR) spectroscopy has been
widely used in organic geochemistry because of its utility in examining
the chemical structures present in sedimentary organic matter (kerogen).
Here, we present such an investigation of kerogens from the Paleogene
Shahejie Formation in the Dongpu Sag, Bohai Bay Basin, eastern China.
Results show that the NMR spectra and their parameters are sensitive
to kerogen type as defined by elemental ratios. The NMR spectra of
types I and II kerogens are similar and show that the dominant chemical
structures are aliphatic functional groups (e.g., methylene and methyl
carbons), followed by aromatic moieties, with relatively fewer structures
containing heteroatoms. In contrast, type III kerogen is considerably
different, having a much lower aliphatic than aromatic functional
group content and a higher degree of aromaticity. Based on this, a
formula is established in response to the source rock hydrogen index
and hydrocarbon generation potential. Our data suggest that the chemical
structural characteristics of lacustrine facies kerogens can be effectively
studied by NMR in good response to hydrocarbon geochemistry. This
implies that NMR is possibly a promising approach in lacustrine organic
geochemistry and provides complements to the challenging study of
paleoenvironment and organic matter accumulation in lacustrine systems
due to the heterogeneity of source rock deposition.