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
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
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.