Volume 47 Issue 5
Sep.  2025
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ZHOU Bing, LUN Zengmin, ZHANG Jie, TANG Yongqiang, QI Yibin, XIAO Pufu, YIN Xia. Research status of self-sealing mechanisms of caprocks and fractures during CO2 geological storage[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(5): 1177-1184. doi: 10.11781/sysydz2025051177
Citation: ZHOU Bing, LUN Zengmin, ZHANG Jie, TANG Yongqiang, QI Yibin, XIAO Pufu, YIN Xia. Research status of self-sealing mechanisms of caprocks and fractures during CO2 geological storage[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(5): 1177-1184. doi: 10.11781/sysydz2025051177

Research status of self-sealing mechanisms of caprocks and fractures during CO2 geological storage

doi: 10.11781/sysydz2025051177
  • Received Date: 2025-05-15
  • Rev Recd Date: 2025-09-04
  • Available Online: 2025-05-15
  • Publish Date: 2025-09-28
  • Through a systematic review of the existing literature, the current research on the dynamic effects of material re-equilibration on caprock and fracture self-sealing patterns during CO2 geological storage is summarized. Laboratory experiments, field monitoring at well sites, and numerical simulation studies generally show that CO2 injection will not breach relatively thick caprocks in the short term, and even if the directly overlying caprock is breached, CO2 will be secondarily trapped and sealed by multi-layered caprock systems. The mechanisms of caprock self-sealing mainly include self-sealing due to injection of supercritical-phase CO2 into confined spaces, mechanical self-sealing resulting from rock pore structure compression or particle migration, and self-sealing induced by chemical reactions. Under the fluid and rock interaction mechanisms after CO2 injection, fractured or faulted systems tend to progressively develop self-sealing over time. Low CO2 flow rates and small fracture apertures are identified as the main factors in the formation of fracture/ fault self-sealing. However, the dynamic quantitative effects of CO2 physical diffusion and chemical reactions on caprocks and fractures under time-scale effects still require further detailed investigation. Currently, research on this dynamic process at home and abroad is gradually evolving toward a systematic approach that integrates multi-spatiotemporal scale coordination, multiple research methods, and multi-factor coupling, and it is increasingly becoming a hot topic in research on CO2 geological storage.

     

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