Hydrocarbon generation and retention potential of Chang 7 organic-rich shale in the Ordos Basin, China

Author:

Sayid Mohamed Awad1ORCID,Yao Zhi-Gang2,Li Rongxi13,Saif Mohammed Maged Ahmed4

Affiliation:

1. School of Earth Sciences and Resources, Chang'an University, Xi'an, Shaanxi, China

2. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an, Shaanxi, China

3. Key Laboratory of West Mineral Resources and Geological Engineering of the Ministry of Education, Chang'an University, Xi'an, Shaanxi, China

4. School of Chemical Engineering and Technology, Xi'an Shiyou University, Xi'an, Shaanxi, China

Abstract

This study investigates the hydrocarbon generation and retention potential of Chang 7 organic-rich shale, with an emphasis on the producibility of retained hydrocarbons, using a sample set chosen to represent a maturity spectrum of 0.54–0.9% R o and organic matter of type II and mixed type II–III. Based on the present-day hydrogen index (HI pd ), the sample sets were divided into three sections: Upper, Middle and Lower. The three sections have a high hydrocarbon generation potential, with an average original total organic carbon (TOC o ) content of 12.27, 3.10 and 5.13 wt%, of which 49.39, 23.62 and 49.86 wt% represents generative organic carbon (GOC), and an original hydrogen index (HI o ) of 581.27, 278.05 and 586.82 HC g −1 rock in the Upper, Middle, and Lower sections, respectively. The bulk of the analysed samples exhibited moderate–high oil saturation, yet the oil crossover effect was only observed in two organic-rich samples, indicating organic-rich shale-oil resource systems. The sorption capacity of organic matter controls oil retention in the Chang 7 shale system, where the oil saturation index increases with increasing maturity in the oil window until a maximum retention capacity of about 82–83 mgHC g −1 TOC is reached at a vitrinite reflectance of 0.8% and thereafter decreases with further maturity. Supplementary material: A detailed spreadsheet of the back-calculated original geochemical parameters using the mass-balance method of Jarvie (2012 a ) is available at https://doi.org/10.6084/m9.figshare.c.6387577

Publisher

Geological Society of London

Subject

Earth and Planetary Sciences (miscellaneous),Economic Geology,Geochemistry and Petrology,Geology,Fuel Technology

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