| Title | Characterization of Microstructures in Lacustrine Organic-Rich Shale Using Micro-CT Images: Qingshankou Formation in Songliao Basin |
| Authors | Cao, Yan Wu, Qi Jin, Zhijun Zhu, Rukai |
| Affiliation | Peking Univ, Inst Energy, Beijing 100871, Peoples R China Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China Peking Univ, Coll Engn, State Key Lab Turbulence & Complex Syst, Beijing 100871, Peoples R China PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China |
| Keywords | PORE STRUCTURE CHARACTERIZATION OIL-SHALE LABORATORY CHARACTERIZATION PERMEABILITY MEASUREMENTS HYDROCARBON GENERATION GAS-ADSORPTION ORDOS BASIN GULONG SAG POROSITY NETWORKS |
| Issue Date | Sep-2022 |
| Publisher | ENERGIES |
| Abstract | In order to explore the development characteristics and influencing factors of microscale pores in lacustrine organic-rich muddy shale, this study selected five shale samples with different mineral compositions from the Qingshankou Formation in the Songliao Basin. The oil content and mineralogy of the shale samples were obtained by pyrolysis and X-ray diffraction analysis, respectively, while the porosity of the samples was computed by micro-CT imaging. Next, based on the CT images, the permeability of each sample was calculated by the Avizo software. Results showed that the continuous porosity of Qingshankou shale in the Songliao Basin was found between 0.84 and 7.79% (average 4.76%), the total porosity between 1.87 and 12.03% (average 8.28%), and the absolute permeability was calculated between 0.061 and 2.284 x 10(-3) mu m(2). The total porosity of the samples has a good positive correlation with the continuous porosity and permeability. This means higher values of total porosity suggested better continuous porosity and permeability. Both total porosity and continuous porosity are positively correlated with the content of clay minerals. Moreover, the oil content of the samples (the S-1 peak from programmed pyrolysis) exhibits a good positive correlation with the total porosity, continuous porosity, permeability, and clay mineral content. Therefore, pores that are developed by clay minerals are the main storage space for oil and flow conduits as well. Clay minerals were found to be the main controlling factor in the porosity, permeability, and the amount of oil content in the pores in the study area. |
| URI | http://hdl.handle.net/20.500.11897/655008 |
| DOI | 10.3390/en15186712 |
| Indexed | EI SCI(E) |
| Appears in Collections: | 地球与空间科学学院 工学院 湍流与复杂系统国家重点实验室 |
