Thermal simulation experiment study of the hydrocarbon generation characteristics of low maturity shale

被引:0
作者
Guo S. [1 ]
Mao W. [1 ]
Ma X. [1 ]
机构
[1] School of Energy Resources, China University of Geosciences(Beijing), Beijing
关键词
R[!sub]o[!/sub; Rock pyrolysis; Shale; Thermal simulation; Total hydrocarbon generation rate;
D O I
10.13745/j.esf.yx.2016-12-34
中图分类号
学科分类号
摘要
This paper analyzes the hydrocarbon generation and pyrolysis parameters by altering maturity of the shale samples through an autoclave thermal simulation experiment. Research shows that as the temperature increases, Ro can be divided into three stages, namely the slow, medium and rapid increase stages. As Ro increases, gaseous hydrocarbon production rate increases throughout while liquid hydrocarbon production rate decreases in the late stage. Pyrolysis hydrocarbon (S2) content is reduced rapidly as liquid hydrocarbons transform into gaseous hydrocarbons, but the amount of total hydrocarbons actually increases. When Ro reaches 0.65% and 1.0% approximately, there are two hydrocarbon generation peaks. This reflects three stages in the evolution of hydrocarbon generation of the low mature shale, i. e., the initial thermal degradation stage, thermal degradation-thermal cracking stage and thermal cracking stage. The relationship between Ro and total hydrocarbon production rate is an exponential curve, correlating roughly with thermal maturity according to the doublet peak of hydrocarbon generation. The research therefore determines the lower limit of Ro for the prospecting and favorable areas of shale gas in the continental basins of China to be 0.65% and 1.0%, respectively. © 2017, Editorial Office of Earth Science Frontiers. All right reserved.
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页码:365 / 369
页数:4
相关论文
共 12 条
[1]  
Guo S.B., Experimental study on isothermal adsorption of methane gas on three shale samples from Upper Paleozoic strata of the Ordos Basin, Journal of Petroleum Science and Engineering, 110, pp. 132-138, (2013)
[2]  
Zha M., Zhao Y.J., Mao C.L., A study on hydrocarbon generating potential and kinetics of source rock pyrolysis, Chinese Journal of Geochemistry, 14, pp. 257-263, (1995)
[3]  
Wang Q., Zou H., Hao F., Et al., Modeling hydrocarbon generation from the Paleogene source rocks in Liaodong Bay, Bohai Sea: a study on gas potential of oil-prone source rocks, Organic Geochemistry, 76, pp. 204-219, (2014)
[4]  
Jiang H., Pang X., Shi H., Et al., Source rock characteristics and hydrocarbon expulsion potential of the Middle Eocene Wenchang formation in the Huizhou depression, Pearl River Mouth Basin, South China Sea, Marine and Petroleum Geology, 67, pp. 635-652, (2015)
[5]  
Hakimi M.H., Abdullah W.H., Thermal maturity history and petroleum generation modelling for the Upper Jurassic Madbi source rocks in the Marib-Shabowah Basin, western Yemen, Marine and Petroleum Geology, 59, pp. 202-216, (2015)
[6]  
Ma X., Zheng J., Zheng G., Et al., Influence of pyrite on hydrocarbon generation during pyrolysis of type-III kerogen, Fuel, 167, pp. 329-336, (2016)
[7]  
Lopatin N.V., Zubairaev S.L., Kos I.M., Et al., Unconventional oil accumulations in the Upper Jurassic Bazhenov black shale formation, West Siberian Basin: a self-sourced reservoir system, Journal of Petroleum Geology, 26, 2, pp. 225-244, (2003)
[8]  
Waples D.W., Time and temperature in petroleum formation: application of Lopatin's method to petroleum exploration, AAPG Bulletin, 64, 6, pp. 916-926, (1980)
[9]  
Middleton M.F., Falvey D.A., Maturity modeling in the Otway Basin, Australia, AAPG Bulletin, 67, pp. 271-279, (1983)
[10]  
Burnham A.K., Sweeney J.J., A chemical kinetic model of vitrinite maturation and reflectance, Geochimica et Cosmochimica Acta, 53, pp. 2649-2657, (1989)