skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Comment on The kinetics of sterane biological marker release and degradation processes during the hydrous pyrolysis of vitrinite kerogen' by G. D. Abbott, G. Y. Wang, T. I. Eglinton, A. K. Home, and G. S. Petch

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
 [1]
  1. Centre for Petroleum and Environmental Organic Geochemistry, Perth (Australia)

In order to further develop understanding of the observable changes in sterane isomer ratios, Abbott et al. (1990) conducted a series of hydrous pyrolysis experiments on mineral-free vitrinite kerogen. Using a deuterated model compound, they found that direct chiral isomerization appears to be relatively unimportant. They derived a kinetic model comprising consecutive release and degradation processes for both isomers and, using a bi-exponential concentration-time function, they were able to determine Arrhenius parameters for four individual reactions. Abbott et al. (1990) claimed that these four reactions account for the change in sterane diastereomer ratios in hydrous pyrolysis experiments. Since it has been observed by a number of people that the so-called steraine isomerization is not a unidirectional reaction, an alternative reaction scheme would be most welcome. Although Abbott and coworkers do not claim that the published kinetic data hold true in the natural environments, the question arises as to whether the kinetic data obtained from these hydrous pyrolysis experiments are applicable to sedimentary processes which occur over geological time.

OSTI ID:
5097108
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Vol. 56:1; ISSN 0016-7037
Country of Publication:
United States
Language:
English