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    Volume 47 Issue 2
    Feb.  2022
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    Article Contents
    Wang Zimeng, Jiang Yuqiang, Fu Yonghong, Lei Zhian, Xu Changhai, Yuan Jingzhou, Wen Ran, Wang Zhanlei, Gu Yifan, Yin Xingping, 2022. Characterization of Pore Structure and Heterogeneity of Shale Reservoir from Wufeng Formation-Sublayers Long-11 in Western Chongqing Based on Nuclear Magnetic Resonance. Earth Science, 47(2): 490-504. doi: 10.3799/dqkx.2021.076
    Citation: Wang Zimeng, Jiang Yuqiang, Fu Yonghong, Lei Zhian, Xu Changhai, Yuan Jingzhou, Wen Ran, Wang Zhanlei, Gu Yifan, Yin Xingping, 2022. Characterization of Pore Structure and Heterogeneity of Shale Reservoir from Wufeng Formation-Sublayers Long-11 in Western Chongqing Based on Nuclear Magnetic Resonance. Earth Science, 47(2): 490-504. doi: 10.3799/dqkx.2021.076

    Characterization of Pore Structure and Heterogeneity of Shale Reservoir from Wufeng Formation-Sublayers Long-11 in Western Chongqing Based on Nuclear Magnetic Resonance

    doi: 10.3799/dqkx.2021.076
    • Received Date: 2021-07-09
    • Publish Date: 2022-02-25
    • Select the organic-rich shale of the Wufeng Formation-sublayers Long-11 in western Chongqing to carry out field emission scanning electron microscopy, nuclear magnetic resonance and X-ray diffraction experiments. Based on image processing and multifractal theory, the pore structure of the shale reservoir was analyzed. Characteristics and heterogeneity. The results show that: (1) Scanning electron microscopy analysis shows that the average pore size of organic pores in the study area is too small. The number of organic pores < 50 nm accounted for 82%, and the number of organic pores >100 nm accounted for 52%; (2)According to the NMR T2 spectrum peak shape, it is divided into categories Ⅰ~Ⅲ, which are single-peak, double-peak and three-peak respectively. The shale reservoir of type Ⅲ has larger pore size and porosity, and has better storage conditions and seepage capacity; (3)Based on the multifractal theory to characterize the heterogeneity of the reservoir, the higher the quartz content, the lower the clay content, the weaker the heterogeneity, which in turn controls the porosity and permeability. The relationship between multifractal parameters and mineral components and physical property parameters effectively characterizes the pore structure of the reservoir and provides a new perspective for the evaluation of its heterogeneity.

       

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