Simulation investigation of vertical heterogeneity on co2 trapping in deep saline aquifers
| dc.contributor.advisor | Pourafshary, Peyman | |
| dc.contributor.advisor | Riazi, Masoud | |
| dc.contributor.author | Spivakova, Irina | |
| dc.date.accessioned | 2026-06-10T10:59:27Z | |
| dc.date.issued | 2026-05-21 | |
| dc.description.abstract | Geological storage of CO2 in deep saline aquifers has been widely proposed as a long-term mitigation option. However, the influence of vertical reservoir heterogeneity on CO2 trapping mechanisms remains insufficiently studied, representing a critical gap. This study uses high-resolution reservoir simulations to systematically quantify how vertical permeability trends influence CO2 trapping in deep saline aquifers. A vertical cross-section model with a 5-year CO2 injection followed by 195 years of monitoring, with heterogeneity levels from homogeneous to highly heterogeneous, explicitly comparing upward-decreasing vs upward-increasing permeability profiles, was developed using CMG software. The results show that permeability architecture ultimately affects trapping outcomes. Upward-decrease profiles create partial barriers that slow vertical migration, compartmentalize the CO2 plume, and increase residual trapping and dissolution, especially at high heterogeneity. In contrast, models with upward-increase permeability preserve vertical connectivity, which leads to a continuous plume with greater structural trapping but less long-term immobilization of CO2. Under high heterogeneity (VDP=0.93), the upward-decreased case immobilizes a large fraction of the injected CO2 (as residual and dissolved), whereas the upward-increased case retains a large connected gas cap. Permeability trends also affect injectivity: low-permeability layers near the well (coarsening-upward) raise the injection pressure, whereas a high-permeability base (fining-upward) maintains lower pressure. These findings provide practical guidance for site selection: in moderately heterogeneous sandstones (VDP ≈ 0.3-0.5), upward-increase trends favor efficient injection and enhanced CO2 dissolution within ~50 years; in highly heterogeneous reservoirs (VDP>0.5), upward-decrease trends support long-term (century-scale) CO2 trapping, though potentially at the cost of higher injection pressure. | |
| dc.identifier.citation | Spivakova, I. (2026). Simulation investigation of vertical heterogeneity on co2 trapping in deep saline aquifers. Nazarbayev University School of Mining and Geosciences | |
| dc.identifier.uri | https://nur.nu.edu.kz/handle/123456789/19048 | |
| dc.language.iso | en | |
| dc.publisher | Nazarbayev University School of Mining and Geosciences | |
| dc.rights | Attribution-NonCommercial-NoDerivs 3.0 United States | en |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/us/ | |
| dc.subject | PQDT_Master | |
| dc.title | Simulation investigation of vertical heterogeneity on co2 trapping in deep saline aquifers | |
| dc.type | Master`s thesis |
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