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Heterogeneity Driven Trapping at the Pore-Network Scale in Edwards Brown Dolomite
Nihal Darraj1, Sojwal Manoorkar2, Catherine Spurin3
1Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, U.K.
Capillary barriers in geological formations enhance CO2 trapping by immobilizing the plume. These barriers, caused by pore-scale heterogeneity, reduce accessible pore volume and influence migration pathways, requiring integration into large-scale models.
Area of Science:
- Geological Carbon Storage
- Pore-Scale Physics
- Reservoir Engineering
Background:
- Residual trapping of CO2 is crucial for geological storage stability but challenging to model at field scales.
- Capillary trapping, influenced by pore-scale heterogeneity and capillary entry pressures, significantly impacts CO2 plume migration.
- Current continuum-scale models struggle to integrate the effects of micron-to-centimeter scale pore heterogeneity on trapping efficiency.
Purpose of the Study:
- To investigate the impact of pore-scale heterogeneity, specifically capillary barriers, on CO2 trapping efficiency and plume migration.
- To quantify how pore connectivity and throat geometry influence capillary entry pressures and snap-off mechanisms.
- To assess the necessity of incorporating pore-scale heterogeneity effects into upscaled models for heterogeneous formations.
Main Methods:
- Conducted flow experiments using brine and decane under capillary-dominated conditions (Ca = 2.6 × 10^-7).
- Acquired time-resolved 3D micro-CT images at 5.6 μm voxel size on a 12 mm by 60 mm rock sample.
- Analyzed segmented volumes using pore-network analysis and ganglia volume/count analysis to quantify trapped volumes.
Main Results:
- A downstream low-porosity region acted as a partial capillary barrier, remaining brine-saturated during decane injection.
- Pore-network analysis revealed limited connectivity (coordination number ~2), with over 30% of pores connected by two or fewer throats.
- Capillary barriers demonstrated enhanced trapping, with negligible displacement of the mobile phase and elevated trapped ganglia volume and count post-imbibition.
Conclusions:
- Capillary barriers significantly increase fluid immobilization while reducing accessible pore volume in heterogeneous formations.
- The presence of capillary barriers influences CO2 plume migration pathways, leading to enhanced trapping.
- Upscaled models for geological storage in heterogeneous formations must capture the effects of pore-scale capillary barriers for accurate predictions.
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