THE CONVERSION OF OIL INTO GAS IN PETROLEUM RESERVOIRS .1. COMPARATIVE KINETIC INVESTIGATION OF GAS GENERATION FROM CRUDE OILS OF LACUSTRINE, MARINE AND FLUVIODELTAIC ORIGIN BY PROGRAMMED-TEMPERATURE CLOSED-SYSTEM PYROLYSIS

Citation
Hj. Schenk et al., THE CONVERSION OF OIL INTO GAS IN PETROLEUM RESERVOIRS .1. COMPARATIVE KINETIC INVESTIGATION OF GAS GENERATION FROM CRUDE OILS OF LACUSTRINE, MARINE AND FLUVIODELTAIC ORIGIN BY PROGRAMMED-TEMPERATURE CLOSED-SYSTEM PYROLYSIS, Organic geochemistry, 26(7-8), 1997, pp. 467-481
Citations number
61
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
01466380
Volume
26
Issue
7-8
Year of publication
1997
Pages
467 - 481
Database
ISI
SICI code
0146-6380(1997)26:7-8<467:TCOOIG>2.0.ZU;2-R
Abstract
The thermal alteration of reservoired petroleum upon burial was simula ted comparatively by closed-system programmed-temperature pyrolysis of produced crude oils of lacustrine, fluviodeltaic, marine elastic and marine carbonate origin using the microscale sealed vessel (MSSV) tech nique. Bulk kinetics of oil-to-gas cracking and accompanying compositi onal changes were studied at heating rates of 0.1, 0.7 and 5.0 K/min. The oil type related variations of experimental cracking temperatures were small compared to those related to heating rate, but the high-tem perature shift of gas evolution curves with increasing rate of heating turned out to be more pronounced for the marine than for the non-mari ne oils. Accordingly the kinetic frequency factors were derived to be higher for gas generation from the lacustrine and fluviodeltaic oils ( A approximate to 4.10(19) min(-1)) than from the marine oils (A approx imate to 2.10(18) min(-1)) and the min gas potential vs. activation en ergy distributions were calculated to be centered around 71-72 kcal/mo l for the former and around 67 kcal/mol for the latter. These kinetic parameters and compositional observations give some evidence that gas generation is accompanied by the formation of aromatic compounds in th e case of the marine oils whereas alkene intermediates seem to be invo lved in the case of the non-marine high wax oils. Under geological hea ting conditions (e.g. 5 K/My), the onset of gas generation and peak ga s generation are extrapolated to occur at about 180 degrees C and 225 degrees C for the high wax oils. The marine oils turn out to be slight ly less stable with peak gas generation at 215 degrees C and the onset of decomposition reactions predicted at about 170 degrees C. In the a bsence of reservoir bitumen and minerals severe oil-to-gas cracking is very unlikely to take place at temperatures less than 160 degrees C, whatever the crude oil type or the geological heating rate. (C) 1997 E lsevier Science Ltd.