CHARACTERIZING MOLECULAR STRUCTURE OF KEROGEN AND ITS HETEROGENEITIES IN MARCELLUS SHALE: IMPACTS ON HYDROCARBON GENERATION AND PRODUCTION
The structural parameters of kerogen were determined using 13C MultiCP/MAS NMR and MultiCP NMR/DD (dipolar dephasing). The average unit structural models of kerogen at different maturity stages were reconstructed using these structural parameters. The models indicate that with increasing maturity, from oil window to wet gas window, there is a gradual increase in the aromatic C%, bridgehead C%, and a gradual decrease in aliphatic C% and aliphatic carbon chain length (Cn’). However, we observe a drastic increase in the bridgehead C% for the sample lying in the dry gas window, indicating a collapse of kerogen interlayers. Comparison of kerogen structural units of Marcellus shale with Duvernay shale and Eagle Ford shale also shows that large heterogeneities can also exist within a particular kerogen type and maturity in different shales. Our data demonstrates that the current kerogen structural models based on kerogen “type” do not incorporate these structural heterogeneities, and could potentially result in inaccurate estimation of 1) HC generation potential (GIP/OIP) of shale and, 2) physico-chemical properties of shale such as its porosity, sorption capacity, elastic and fracture properties, which controls flow and recovery of HC’s.