{"title":"准噶尔盆地卢卡沟页岩的石油生成、保留和排出过程:改良膨胀实验和盆地建模的制约因素","authors":"Shuyong Shi, Tian Liang, Yunpeng Wang, Yanrong Zou, Yun Shan, Ping’an Peng","doi":"10.1016/j.jseaes.2025.106628","DOIUrl":null,"url":null,"abstract":"<div><div>The solubility parameters of generated oil are determined by the relative ratios of different oil fractions and vary significantly at different maturation stages. However, previous swelling experiments based on single solvent could only represent the retention behavior for one of oil fractions, which has influence on the accurate evaluation of oil-retention capacity on residual kerogen. In this study, the kerogen of the Lower Permian Lucaogou (P<sub>1</sub>l) shale from the Junggar Basin was used to conduct the closed-system pyrolysis experiments and the kinetic parameters were obtained for the evaluation of oil-generation process. The swelling experiments were also performed to evaluate oil-retention amount on residual kerogen. Unlike previous swelling experiments, we chose the mixture of ethyl acetate and <em>iso</em>-octane as swelling solvents, and adjusted the relative ratios to bring the solubility parameter of each mixture close to the generated oil for each pyrolysis temperature as possible. The kinetic model oil generation-retention-expulsion (GRE model) was established based on the results of pyrolysis and swelling experiments. This kinetic model showed that the generated oil of the Lucaogou shale started to expel from the shale when the thermal maturity reached 0.92 %. Furthermore, the GRE model was applied to recover oil generation, retention and expulsion processes of the shale by PetroMod software. The results showed that the generated oil started to expel from the shale at the Late Jurassic (approximately 150 Ma). The current masses of generated, retained and expelled oil of the shale are 12.3, 6.3 and 6.0 × 10<sup>6</sup> tons/km<sup>2</sup>, respectively.</div></div>","PeriodicalId":50253,"journal":{"name":"Journal of Asian Earth Sciences","volume":"289 ","pages":"Article 106628"},"PeriodicalIF":2.7000,"publicationDate":"2025-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Oil generation, retention and expulsion processes of the Lucaogou shale in the Junggar Basin: Constraints from improved swelling experiment and basin modelling\",\"authors\":\"Shuyong Shi, Tian Liang, Yunpeng Wang, Yanrong Zou, Yun Shan, Ping’an Peng\",\"doi\":\"10.1016/j.jseaes.2025.106628\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The solubility parameters of generated oil are determined by the relative ratios of different oil fractions and vary significantly at different maturation stages. However, previous swelling experiments based on single solvent could only represent the retention behavior for one of oil fractions, which has influence on the accurate evaluation of oil-retention capacity on residual kerogen. In this study, the kerogen of the Lower Permian Lucaogou (P<sub>1</sub>l) shale from the Junggar Basin was used to conduct the closed-system pyrolysis experiments and the kinetic parameters were obtained for the evaluation of oil-generation process. The swelling experiments were also performed to evaluate oil-retention amount on residual kerogen. Unlike previous swelling experiments, we chose the mixture of ethyl acetate and <em>iso</em>-octane as swelling solvents, and adjusted the relative ratios to bring the solubility parameter of each mixture close to the generated oil for each pyrolysis temperature as possible. The kinetic model oil generation-retention-expulsion (GRE model) was established based on the results of pyrolysis and swelling experiments. This kinetic model showed that the generated oil of the Lucaogou shale started to expel from the shale when the thermal maturity reached 0.92 %. Furthermore, the GRE model was applied to recover oil generation, retention and expulsion processes of the shale by PetroMod software. The results showed that the generated oil started to expel from the shale at the Late Jurassic (approximately 150 Ma). The current masses of generated, retained and expelled oil of the shale are 12.3, 6.3 and 6.0 × 10<sup>6</sup> tons/km<sup>2</sup>, respectively.</div></div>\",\"PeriodicalId\":50253,\"journal\":{\"name\":\"Journal of Asian Earth Sciences\",\"volume\":\"289 \",\"pages\":\"Article 106628\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2025-04-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Asian Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1367912025001439\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Asian Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1367912025001439","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Oil generation, retention and expulsion processes of the Lucaogou shale in the Junggar Basin: Constraints from improved swelling experiment and basin modelling
The solubility parameters of generated oil are determined by the relative ratios of different oil fractions and vary significantly at different maturation stages. However, previous swelling experiments based on single solvent could only represent the retention behavior for one of oil fractions, which has influence on the accurate evaluation of oil-retention capacity on residual kerogen. In this study, the kerogen of the Lower Permian Lucaogou (P1l) shale from the Junggar Basin was used to conduct the closed-system pyrolysis experiments and the kinetic parameters were obtained for the evaluation of oil-generation process. The swelling experiments were also performed to evaluate oil-retention amount on residual kerogen. Unlike previous swelling experiments, we chose the mixture of ethyl acetate and iso-octane as swelling solvents, and adjusted the relative ratios to bring the solubility parameter of each mixture close to the generated oil for each pyrolysis temperature as possible. The kinetic model oil generation-retention-expulsion (GRE model) was established based on the results of pyrolysis and swelling experiments. This kinetic model showed that the generated oil of the Lucaogou shale started to expel from the shale when the thermal maturity reached 0.92 %. Furthermore, the GRE model was applied to recover oil generation, retention and expulsion processes of the shale by PetroMod software. The results showed that the generated oil started to expel from the shale at the Late Jurassic (approximately 150 Ma). The current masses of generated, retained and expelled oil of the shale are 12.3, 6.3 and 6.0 × 106 tons/km2, respectively.
期刊介绍:
Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance.
The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.