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张鹏, 黄宇琪, 杨军伟, 刘洪洋. 黔西北龙潭组页岩储层特征研究[J]. 煤炭科学技术, 2019, (4).
引用本文: 张鹏, 黄宇琪, 杨军伟, 刘洪洋. 黔西北龙潭组页岩储层特征研究[J]. 煤炭科学技术, 2019, (4).
ZHANG Peng, HUANG Yuqi, YANG Junwei, LIU Hongyang. Study on characteristics of shale reservoirs from Longtan Formation in northwest Guizhou[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (4).
Citation: ZHANG Peng, HUANG Yuqi, YANG Junwei, LIU Hongyang. Study on characteristics of shale reservoirs from Longtan Formation in northwest Guizhou[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (4).

黔西北龙潭组页岩储层特征研究

Study on characteristics of shale reservoirs from Longtan Formation in northwest Guizhou

  • 摘要: 以黔西北龙潭组页岩为研究对象,基于岩心有机地球化学、矿物组成、扫描电镜、比表面及孔径和低温N2脱附-吸附试验测试,研究了黔西北地区龙潭组页岩储层特征。结果表明:黔西北龙潭组页岩有机质丰度高,有机质类型为Ⅲ型,干酷根处于过成熟阶段,具有良好的生烃条件。页岩矿物组分以黏土矿物和石英为主,黏土矿物中以伊利石和伊/蒙混层含量最高;储层孔隙度低,孔隙类型多样,孔隙大小以中孔为主,脆性指数为57.6%,表明龙潭组泥页岩具有良好的脆性特征;通过N2吸附-脱附曲线发现,龙潭组页岩样品的分形维数D1=2.68~2.77(相对压力≤05),D2=2.70~2.89
    (相对压力>05),D1、D2数值均偏大,反映龙潭组页岩孔隙非均质较强,结构复杂。分形维数D1和D2与比表面积成较好的正相关关系,与页岩平均孔径成较好的负相关关系。

     

    Abstract: Based on the Longtan Formation shale in the northwestern Guizhou, the shale reservoir characteristics of Longtan Formation in the northwestern Guizhou were studied based on organic geochemistry, mineral composition, FE-SEM, specific surface and pore size, N2 desorption and isothermal adsorption etc. The results show that the shale of Longtan Formation in northwestern Guizhou has a high abundance of organic matter and a Type III Kerogen,which is in an over mature stage and has good hydrocarbon generation conditions. These shale samples mineral composition is mainly clay minerals and quartz, of which clay mineral compositions have the highest content of illite and Illonite/Montmor mixed layer; The brittleness index is 57.6%, indicating that the shale of Longtan Formation has good brittleness with low porosity, various pore types, and pore size is mainly mesopore; The N2 adsorption-desorption curve shows that the fractal dimensionD1 of Longtan Formation shale samples is 2.68~2.77(relative pressure≤0.5),D2 is 2.70~2.89(relative pressure>0.5). The values ofD1 andD2 are large, reflecting that the Longtan Formation shale has a heterogeneous pore heterogeneity and a complex structure. The fractal dimensionD1 andD2 have a good positive correlation with the specific surface area and a good negative correlation with the average pore size of the shale.

     

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