Effects of thermal maturation on stable organic carbon isotopes as determined by hydrous pyrolysis of Woodford Shale

Details Effects of thermal maturation on stable organic carbon isotopes as determined by hydrous pyrolysis of Woodford Shale Effects of thermal maturation on stable organic carbon isotopes as determined by hydrous pyrolysis of Woodford Shale

Aug 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983gecoa..47.1471l&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 47, Issue 8, pp.1471-1479

Computer Science

9

Scientific paper

Acquiring crude oils that have been expelled from the same rock unit at different levels of thermal maturation is currently not feasible in the natural system. This prevents direct correlation of compositional changes between the organic matter retained in a source rock and its expelled crude oil at different levels of thermal maturation. Alleviation of this deficiency in studying the natural system requires the use of laboratory experiments. Natural generation of petroleum from amorphous type-II kerogen in the Woodford Shale may be simulated by hydrous pyrolysis, which involves heating crushed rock in contact with water at subcritical temperatures (<374°C). Four distinct stages of petroleum generation are observed from this type of pyrolysis; (1) pre-oil generation, (2) incipient-oil generation, (3) primary-oil generation, and (4) post-oil generation. The effects of thermal maturation on the 13 C values of kerogen, bitumen, and expelled oil-like pyrolysate from the Woodford Shale have been studied through these four stages of petroleum generation. Similar to the natural system, the kerogens isolated from the pyrolyzed rock showed no significant change in 13 C. This suggests that the 13 C value of kerogens may be useful in kerogen typing and oil-to-source rock correlations. 13 C values of bitumens extracted from the pyrolyzed rock showed an initial decrease during the incipient-oil generation stage, followed by depletion during the primary- and post-oil generation stages. This reversal is not favorable for geochemical correlation or maturity evaluation. Saturated and polar components of the bitumen show the greatest 13 C variations with increasing thermal maturation. The difference between the 13 C of these two components gives a unidirectional trend that serves as a general indicator of thermal maturation and is referred to as the bitumen isotope index (BII). 13 C values of the expelled pyrolysates show a unidirectional increase with increasing thermal maturation. The constancy and similarity of 13 C values of the aromatic components in the expelled pyrolysates and bitumens, with increasing thermal maturation, encourages their use in oil-to-oil and oil-to-source rock correlations. Isotopic type-curves for expelled pyrolysates indicate that they may be useful in oil-to- oil correlations, but have a limited use in oil-to-source rock correlations.

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