Coal Geology & Exploration
Abstract
Objective CO2 breakthrough pressure, a core parameter for characterizing the sealing performance of saline aquifers as cap rocks, holds important scientific significance and application value for ensuring the safety of CO2 geological storage engineering and assessing its storage potential. However, there is a lack of systematic studies on the variation patterns and mechanisms of breakthrough pressure under different occurrence phases of CO2 (supercritical, liquid, and gaseous) currently. Accordingly, universal and reliable conclusions are yet to be reached. Methods This study conducted experiments on a natural low-permeability unsaturated sandstone core. Using the step-by-step method, 13 groups of breakthrough pressure experiments were carried out under different CO2 phases to deeply explore the variation patterns of CO2 breakthrough pressure under these phases. Results and Conclusions The results indicate that the CO2 phase is not directly correlated with the magnitude of the CO2 breakthrough pressure. Under the experimental conditions of this study, the CO2 breakthrough pressure at any phase transition point was higher than that under a single phase. Under the condition of a single CO2 phase, the CO2 breakthrough pressure decreased with an increase in pressure, exhibiting an exponential relationship with the latter. Pressure produced the greatest impact on the breakthrough pressure of supercritical CO2 but posed the smallest impact on that of gaseous CO2. The influence of pressure on CO2 breakthrough pressure is caused by the synergistic effect of the interfacial tension of the CO2-water system and the wettability (the contact angle) of the CO2-water-rock system, as well as the two-phase density difference and viscosity ratio. Sensitivity analysis results show that the viscosity ratio was a significant factor affecting the CO2 breakthrough pressure, with a total contribution rate of up to 39.9%. Analysis of the lg Ca-lg M displacement stability diagram further confirmed that viscosity acted as a dominant factor affecting the experimental results of this study. Comparison with the formation pressure data and practical application to engineering sites in basins reveal that the experimental conditions of this study are consistent with actual engineering. The results of this study serve as an important reference for accurately evaluating the storage capacity of saline aquifers and guiding target siting for CO2 geologic geological storage.
Keywords
CO2 phase, breakthrough pressure, viscous force, CO2 geologic storage, saline aquifer
DOI
10.12363/issn.1001-1986.25.04.0247
Recommended Citation
DAN Wendong, LI Yi, WANG Fugang,
et al.
(2025)
"An experimental study on the breakthrough pressure of different CO2 phases against cap rocks for carbon storage in saline aquifers,"
Coal Geology & Exploration: Vol. 53:
Iss.
10, Article 14.
DOI: 10.12363/issn.1001-1986.25.04.0247
Available at:
https://cge.researchcommons.org/journal/vol53/iss10/14
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