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Propagation of rock fracture subjected to fluid injection using 4D X-ray computed tomography
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Zizhuo Maa, c, e, Yibo Wanga, c, *, Liang Zhaob, c, Xinglin Leid, Yikang Zhenga, c, Shaojiang Wua, c, Qingfeng Xuea, c
Journal of Rock Mechanics and Geotechnical Engineering | 2026, 18(5) : 3640 - 3653
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Journal of Rock Mechanics and Geotechnical Engineering | 2026, 18(5): 3640-3653
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Propagation of rock fracture subjected to fluid injection using 4D X-ray computed tomography
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Zizhuo Maa, c, e, Yibo Wanga, c, *, Liang Zhaob, c, Xinglin Leid, Yikang Zhenga, c, Shaojiang Wua, c, Qingfeng Xuea, c
Affiliations
  • aKey Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
  • bState Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
  • cCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China
  • dGeological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Ibaraki, Japan
  • eKey Laboratory of Oil & Gas Reservoir Geophysics, SINOPEC, Beijing, 100083, China
  • Zizhuo Ma received her BSc degree in exploration technology and engineering from Jilin University and her PhD degree in solid geophysics from the Institute of Geology and Geophysics, Chinese Academy of Sciences. She is currently working at the Geophysical Technology Research Institute of Sinopec Petroleum Exploration and Production Research Institute. Her research interests include multiphysics monitoring and analysis of hydraulic fracture propagation processes, rock elastic properties measurement and modeling.

Published: 2026-05-25 doi: 10.1016/j.jrmge.2025.08.024
Outline
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During unconventional energy extraction, substantial volumes of fluid are injected into low-permeability reservoirs to facilitate hydraulic fracturing, creating an extensive network of fractures that enhance fluid mobility. However, such large-scale fluid injection can lead to the initiation and propagation of fractures, potentially triggering detectable seismic events that pose risks to human life and infrastructure. To better understand these processes, in situ dynamic scanning imaging of hydraulic fracture propagation and water-rock interactions in tight sandstones has been conducted using X-ray computed tomography (CT). Our experimental findings reveal that fluid infiltration weakens rock strength, thereby promoting rock failure. Under the influence of fluid injection, microfractures undergo a continuous cycle of generation, expansion, and coalescence, ultimately forming interconnected hydrological pathways. These pathways are critical for the sustained propagation of fractures within the rock. CT imaging highlights a positive feedback loop between fracture growth and the enhancement of fluid diffusion. Notably, the rock at the dry-wet interface of the fluid front is particularly susceptible to fracturing. Additionally, the rates of fracturing vary among different fractures and tend to progressively decrease as the fractures extend deeper into the rock.

Fluid injection  /  Sandstone failure process  /  In situ 4D X-ray computed tomography  /  Real-time direct identification of rock fracture propagation  /  Water-rock interaction analysis  /  Hydraulic connection channel
Zizhuo Ma, Yibo Wang, Liang Zhao, Xinglin Lei, Yikang Zheng, Shaojiang Wu, Qingfeng Xue. Propagation of rock fracture subjected to fluid injection using 4D X-ray computed tomography[J]. Journal of Rock Mechanics and Geotechnical Engineering, 2026 , 18 (5) : 3640 -3653 . DOI: 10.1016/j.jrmge.2025.08.024
  • National Science Fund for Distinguished Young Scholars(42025403)
  • National Key R&D Program of China(2021YFA0716800)
Year 2026 volume 18 Issue 5
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Article Info
doi: 10.1016/j.jrmge.2025.08.024
  • Receive Date:2025-01-02
  • Online Date:2026-06-17
  • Published:2026-05-25
Article Data
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History
  • Received:2025-01-02
  • Revised:2025-07-23
  • Accepted:2025-08-22
Funding
National Science Fund for Distinguished Young Scholars(42025403)
National Key R&D Program of China(2021YFA0716800)
Affiliations
    aKey Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
    bState Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
    cCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China
    dGeological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Ibaraki, Japan
    eKey Laboratory of Oil & Gas Reservoir Geophysics, SINOPEC, Beijing, 100083, China

Corresponding:

* Corresponding author. Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China. E-mail address: (Y. Wang).
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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