Evolution of pore-fracture system across different maturity levels and its implications for carbon dioxide sequestration in lacustrine shale

Authors

  • Xin Tian National Key Laboratory of Continental Shale Oil, Northeast Petroleum University, Daqing 163318, P. R. China
  • Zhejun Pan National Key Laboratory of Continental Shale Oil, Northeast Petroleum University, Daqing 163318, P. R. China
  • Yeping Ji Commonwealth Scientific and Industrial Research Organisation, Perth, WA 6151, Australia
  • Mehdi Ostadhassan National Key Laboratory of Continental Shale Oil, Northeast Petroleum University, Daqing 163318, P. R. China; Institute of Geosciences, Marine and Land Geomechanics and Geotectonics, Christian-Albrechts-Universität, Kiel 24118, Germany
  • Bo Liu National Key Laboratory of Continental Shale Oil, Northeast Petroleum University, Daqing 163318, P. R. China
  • Mengdi Sun National Key Laboratory of Continental Shale Oil, Northeast Petroleum University, Daqing 163318, P. R. China; Heilongjiang Provincial Key Laboratory of Continental Shale Oil, Daqing 163712, P. R. China (Email: sunmd@nepu.edu.cn)

Abstract

The geometry and topology of shale pore-fracture systems govern hydrocarbon migration and control the feasibility of geological carbon dioxide storage in shale reservoirs. This study examines lacustrine shale across a range of maturities by integrating (ultra) smallangle neutron scattering, repeated mercury intrusion capillary pressure, field-emission scanning electron microscopy, and computed tomography following Wood’s metal impregnation. The pore system is divided into four pore-size classes, and their volumes and connectivity are tracked with increasing thermal maturity. At low maturity, mechanical compaction and early cementation reduce the total pore volume and concentrate connected porosity in fractures. As maturity increases, newly formed organic-matter pores lead to a modest increase in total pore volume, while liquid hydrocarbons generated within the oil window occupy part of the pore space and weaken pore-fracture connectivity. At high maturity, the secondary cracking of liquid hydrocarbons to gas raises pore pressure, partially reopens previously sealed pores and fractures, and enhances both total pore volume and pore-fracture connectivity. These results indicate that mature to high-mature lacustrine shales provide more pore surface area, storage space, and connected pathways for the long-term storage of carbon dioxide than low-maturity shales.

Document Type: Original article

Cited as: Tian, X., Pan, Z., Ji, Y., Ostadhassan, M., Liu, B., Sun, M. Evolution of pore-fracture system across different maturity levels and its implications for carbon dioxide sequestration in lacustrine shale. Advances in Geo-Energy Research, 2026, 19(1): 82-96. https://doi.org/10.46690/ager.2026.01.07

DOI:

https://doi.org/10.46690/ager.2026.01.07

Keywords:

Pore-fracture connectivity, maturation gradient, fractal dimension, neutron scattering, carbon dioxide storage

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Published

2026-01-12

How to Cite

Tian, X., Pan, Z., Ji, Y., Ostadhassan, M., Liu, B., & Sun, M. (2026). Evolution of pore-fracture system across different maturity levels and its implications for carbon dioxide sequestration in lacustrine shale. Advances in Geo-Energy Research, 19(1), 82–96. https://doi.org/10.46690/ager.2026.01.07