Research Article
Mesoscale Assessment of CO2 Storage Potential and Geological Suitability for Target Area Selection in the Sichuan Basin
Table 6
Index system for geological suitability assessment to select suitable targets for deep saline aquifer CO2 storage.
| Level one index | Weight | Level two index | Weight | Level three index | Weight | Good | General | Poor | Key veto factor |
| Reservoir conditions and storage potential | 0.50 | Characteristic of the best reservoir | 0.60 | Lithology | 0.07 | Clastic | Mix of clastic and carbonate | Carbonate | | Single layer thickness h/m | 0.11 | ≥80 | 30 ≤ h < 80 | 10 ≤ h < 30 | <10 | Sedimentary facies | 0.36 | River, delta | Turbidity, alluvial fan | Beach bar, reef | | Average porosity /% | 0.20 | ≥15 | 10 ≤ < 15 | 5 ≤ < 10 | <5 | Average permeability /mD | 0.27 | ≥50 | 10 ≤ k < 50 | 1 ≤ k < 10 | <1 | Storage potential | 0.40 | Storage potential per unit area G (104 t/km2) | 1.00 | ≥100 | 10 ≤ G < 100 | <10 | |
| Geological safety | 0.50 | Characteristic of the main caprock | 0.62 | Lithology | 0.30 | Evaporites | Argillite | Shale and dense limestone | | Thickness h/m | 0.53 | ≥100 | 50 ≤ h < 100 | 10 ≤ h < 50 | <10 | Depth D/m | 0.11 | 1000 ≤ D ≤ 2700 | <1000 | >2700 | | Buffer caprock above the main caprock | 0.06 | Multiple sets | Single set | None | | Hydrodynamic conditions | 0.24 | Hydrodynamic conditions | 1.00 | Groundwater high-containment area | Groundwater containment area | Groundwater semicontainment area | Groundwater open area | Seismic activity | 0.14 | Peak ground acceleration | 0.50 | <0.05 g | 0.05 g, 0.10 g | 0.15 g, 0.20 g, 0.30 g | ≥0.40 g | Development degree of fractures | 0.50 | Simple | Moderate | Complex | Within 25 km of active faults |
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