--> --> Abstract: Simulation of Hydrocarbon Source Rock Maturation by Hydrous Pyrolysis, by P. Yin, S. W. Boese, D. B. MacGowan, R. C. Surdam, and F. P. Miknis; #91017 (1992).
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ABSTRACT: Simulation of Hydrocarbon Source Rock Previous HitMaturationNext Hit by Hydrous Pyrolysis

YIN, PEIGUI, STEVEN W. BOESE, DONALD B. MACGOWAN, and RONALD C. SURDAM, University of Wyoming, Laramie, WY, and FRANCIS P. MIKNIS, Western Research Institute, Laramie, WY

Hydrous pyrolysis experiments were performed on samples of an immature brown coal from the Gippsland basin (southeastern Australia), for 72 hours at temperatures ranging from 270 to 350 degrees C. The produced liquid pyrolysate ("oil"), gases, and aqueous organic acid anions were quantified, and the geochemical properties of the "oil" were determined. The solid residue from experiments was studied using conventional pyrolysis, elemental analysis, vitrinite reflectance microscopy, and nuclear magnetic resonance. The Previous HitmaturationNext Hit stages of the solid residue with increasing experimental temperatures can be correlated with Previous HitmaturationNext Hit trends of the natural brown coal samples

in the Gippsland basin from near surface to a depth of 9000 ft. The "oil" derived from hydrous pyrolysis is poorer in saturates and richer in aromatics and NSO compounds than the natural oil produced from the Gippsland basin. The major carboxylic acid anions (e.g., acetate and propionate) generated during hydrous pyrolysis also are present within the produced waters in the Gippsland basin. The experimental results suggest that hydrous pyrolysis experiments can simulate the natural Previous HitmaturationTop of source rocks and can be used to estimate the genetic potential of specific source rock for both hydrocarbons and organic acid anions.


AAPG Search and Discovery Article #91017©1992 AAPG Rocky Mountain Section Meeting, Casper, Wyoming, September 13-16, 1992 (2009)