4.6 Article

Influence of different CO2 phase states on fluid flow pathways in coal: insights from image reconstruction and fractal study

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SPRINGER HEIDELBERG
DOI: 10.1007/s10064-023-03322-0

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CO2 geological sequestration; CO2 leakage; CO2-water-coal interactions; Fractal dimension of tortuosity; Preferential flow pathways

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The changes in CO2 phase state have significant implications for evaluating the leakage risk during CO2 sequestration in water-bearing coal seams. The study investigated the effects of different CO2 phase states on fluid flow pathways in water-bearing coal and found that supercritical CO2 (ScCO2) treatment was more effective than subcritical CO2 (SubCO2) treatment in reducing coal heterogeneity and increasing permeability. The analysis also revealed that ScCO2 treatment had a greater impact on the size, quantity, and location of preferential flow pathways in coal compared to SubCO2 treatment.
The CO2 phase state changes during the long-term interaction with coal seams. A proper understanding of the influence of different CO2 phase states in water-bearing coal seams is of great significance in evaluating the leakage risk during CO2 sequestration. The evolution of fluid flow pathways in water-bearing coal subjected to the treatment of different CO2 phase states was investigated by using X-ray computed tomography (CT) technology, fractal dimension, and three-dimensional (3D) pore-scale flow modeling. The results show that the supercritical CO2 (ScCO2) treatment reduced the coal heterogeneity by 12.69% and increased the absolute permeability by 58.75%. Conversely, only 0.71% of coal heterogeneity reduction occurred after subcritical CO2 (SubCO(2)) treatment, increasing the absolute permeability by 24.91%. The reduction in the tortuosity fractal dimension after ScCO2 treatment was 2.69% larger than that of SubCO(2) treatment, indicating that ScCO2 treatment was more favorable for improving the transport capacity of flow pathways. The pressure field distributions in the pore network model (PNM) were determined by coal heterogeneity and influenced by the number of flow pathways. The effect of ScCO2 treatment on the size, quantity, and location of preferential flow pathways in coal is more significant than that of SubCO(2) treatment. Moreover, the proportion of preferential flow pathways in ScCO2-treated coal was less than 50%, much lower than that of the throats in PNMs. In contrast, the proportion of preferential flow pathways in SubCO(2)-treated coal was approximately 30% higher than that in ScCO2-treated coal. The distribution of preferential flow pathways also indicated that not all pores with larger radii participated in preferential flow. Furthermore, more than 50% of the pathways in the ScCO2-treated coal did not contribute to fluid flow, and could affect the stability of the coal seam.

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