| Title | Generation and expulsion process of the Chang 7 oil shale in the Ordos Basin based on temperature -based semi -open pyrolysis: Implications for in -situ conversion process |
| Authors | Ma, Weijiao Hou, Lianhua Luo, Xia Liu, Jinzhong Tao, Shizhen Guan, Ping Cai, Yuwen |
| Affiliation | Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Peoples R China Natl Nat Sci Fdn China, Beijing 100085, Peoples R China |
| Keywords | TRIASSIC YANCHANG FORMATION ORGANIC-MATTER HYDROUS PYROLYSIS GAS GENERATION CHINA IMPLICATIONS SOURCE-ROCK II KEROGEN PETROLEUM EVOLUTION SYSTEM |
| Issue Date | Jul-2020 |
| Publisher | JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING |
| Abstract | There is a substantial amount of oil shale resources in the seventh member of the Triassic Yanchang Formation (abbreviated as Chang 7) in the Ordos Basin, and its geological and geochemical characteristics are highly suitable for in-situ conversion process (ICP). A comprehensive characterization of its hydrocarbon generation, expulsion and retention features will help determine the optimum conditions for future field tests. However, typical thermal simulation experiments based on either open-system or closed-system are not applicable to provide data to construct the models. Therefore, in this study, eight parallel thermal simulation experiments, which were based on the newly designed temperature-based semi-open pyrolysis experiments were performed on the Chang 7 oil shale. The yields (including cumulative yields and net incremental yields) and compositional characteristics of the expelled oil, expelled gas, and retained oil were analyzed. Results show that the hydrocarbon expulsion has a coupling relationship with hydrocarbon generation that can be divided into four stages: (1) Slow hydrocarbon generation stage (300-320 degrees C, 0.53-0.55 %Ro). Minimal amounts of oil and gas are generated in this stage. The hydrocarbon expulsion efficiency increases rapidly. (2) Quick oil-generation stage (320-380 degrees C, 0.55-1.09 %Ro). The fast cracking of kerogen and thermal bitumen generates a large amount of oil. The hydrocarbon expulsion efficiency remains relatively stable. (3) The secondary oil cracking and quick gas-generation stage (380-420 degrees C, 1.09-1.66 %Ro). The oil yield begins to decrease after reaching its maximum and a large amount of hydrocarbon gas is generated. The oil generation capability of kerogen is basically exhausted. The hydrocarbon expulsion efficiency and gas/oil ratio increase rapidly at this stage. (4) The heavy hydrocarbon gas cracking stage (after 420 degrees C, 1.66 %Ro). The oil yield continues to decline, accompanied by the onset decline in the gas yield (except methane). At this time, the hydrocarbon expulsion efficiency continues to increase but at a rather low speed. Under the experimental conditions in this study, 1.24-1.66% Ro is considered a favorable thermal maturity interval, in which maximum oil production with relatively light components can be obtained and the hydrocarbon gas is abundant. |
| URI | http://hdl.handle.net/20.500.11897/588960 |
| ISSN | 0920-4105 |
| DOI | 10.1016/j.petrol.2020.107035 |
| Indexed | SCI(E) Scopus EI |
| Appears in Collections: | 地球与空间科学学院 |
