Pore Structure and Fractal Characteristics of Tight Sandstone: A Case Study for Huagang Formation in the Xihu Sag, East China Sea Basin, China
Jin Dong,
Zhilong Huang (),
Jinlong Chen,
Tianjun Li,
Jing Zhao,
Yongshuai Pan and
Tong Qu
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Jin Dong: Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing 100083, China
Zhilong Huang: College of Geosciences, China University of Petroleum, Beijing 102249, China
Jinlong Chen: College of Geosciences, China University of Petroleum, Beijing 102249, China
Tianjun Li: College of Geosciences, China University of Petroleum, Beijing 102249, China
Jing Zhao: College of Geosciences, China University of Petroleum, Beijing 102249, China
Yongshuai Pan: College of Geosciences, China University of Petroleum, Beijing 102249, China
Tong Qu: College of Geosciences, China University of Petroleum, Beijing 102249, China
Energies, 2023, vol. 16, issue 4, 1-24
Abstract:
Various experiments, including routine petrophysical measurements, thin section and scanning electronic microscope (SEM), high-pressure mercury intrusion (HPMI), and nuclear magnetic resonance (NMR), were performed to characterize the microscopic pore structure of tight sandstone in the Huagang Formation (E 3 h), Xihu Sag, East China Sea Basin, China. Specifically, NMR was used to investigate the dynamic variation of fractal dimensions during centrifugation, and the comparison of HPMI and NMR were used to clarify the difference of fractal dimensions. The results showed that there were four types of pores observed in thin section and SEM images: primary intergranular pores, intergranular dissolution pores, intragranular dissolution pores, and micropores within clay aggregates. The geometric shape and pore size of different pore types showed huge differences, indicating the formation of complex and diverse pore structures in the E 3 h formation. The flow capability of the reservoir was dominated by large pores, while the storage capacity was determined by small pores. The dynamic variation of fractal dimensions calculated by NMR data showed the water residing in the pore structure with low fractal dimensions was removed preferentially, and the pore structure of the resided water was always more complicated than the pore structure of removed water, which indicated the flow capability of the reservoir was affected by the complexity of the pore structure. Based on the comparison of the fractal dimension data from HPMI and NMR, it was found that the variation trends of the fractal dimensions were consistent, as the radius of the pore throat increased, the fractal dimensions increased, and the pore structure became more complicated. Both fractal dimensions of macropores (D mac ) and movable-fluid pores (D mov ) can reflect the flow capability of reservoir effectively, but the correlations between fractal dimensions from HMPI and NMR were poor, which could be due to the different working mechanism in these methods.
Keywords: East China Sea Basin; tight sandstone reservoir; pore structure; HPMI; NMR with centrifugation; fractal analysis (search for similar items in EconPapers)
JEL-codes: Q Q0 Q4 Q40 Q41 Q42 Q43 Q47 Q48 Q49 (search for similar items in EconPapers)
Date: 2023
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