TY - JOUR
T1 - Assessing storage injectivity and rock physics alteration during dry and wet CO2 injection for the storage prospect of the Gassum Formation in the Stenlille Aquifer, Denmark
AU - Rostami, Behzad
AU - Al-Masri, Wael F.
AU - Mohammadkhani, Samira
AU - Olsen, Dan
N1 - Publisher Copyright:
© 2025 American Chemical Society.
PY - 2025/3/6
Y1 - 2025/3/6
N2 - Saline aquifers are prime candidates for carbon dioxide (CO2) storage. However, some projects encounter challenges such as salt precipitation due to water evaporation during CO2 injection. While salt precipitation alters reservoir porosity and permeability, the level of CO2 injectivity remains higher compared to brine displacement using water-saturated CO2. This study examines the effects of water-saturated (wet) and undersaturated (dry) supercritical CO2 (scCO2) injection on the properties of brine-saturated Stenlille sandstone reservoir cores from the Gassum Formation. Three high-volume core flooding experiments under reservoir conditions were conducted, analyzing dynamic differential pressure, in situ saturation changes (measured with a high-pressure acoustic separator), and pre- and postexperiment core properties. The results showed distinct differences between dry and wet CO2 injection, particularly regarding the vaporization and salt precipitation effects on permeability. Dry CO2 injection reduced water saturation to as low as 4% PV, simulating dry-out near injection wells, and caused absolute permeability changes of 21% on average due to salt precipitation. In contrast, wet CO2 injection, representative of bulk reservoir flow, preserved high water saturations without salt precipitation. Additionally, the final relative permeability to supercritical CO2 (KrscCO2) was higher for the dried core (0.62) compared to that of the wet injection experiment (0.40). This suggests that water vaporization during dry CO2 injection enhances CO2 effective permeability despite salt precipitation. Comparing wet CO2 injections in samples with different permeabilities using dimensionless numbers revealed that unstable flow in high-permeability channels leads to higher overall relative permeability and residual water saturation. The comprehensive experimental data from this study provide valuable insights for simulating two-phase scCO2–brine displacement and dissolution processes under reservoir conditions.
AB - Saline aquifers are prime candidates for carbon dioxide (CO2) storage. However, some projects encounter challenges such as salt precipitation due to water evaporation during CO2 injection. While salt precipitation alters reservoir porosity and permeability, the level of CO2 injectivity remains higher compared to brine displacement using water-saturated CO2. This study examines the effects of water-saturated (wet) and undersaturated (dry) supercritical CO2 (scCO2) injection on the properties of brine-saturated Stenlille sandstone reservoir cores from the Gassum Formation. Three high-volume core flooding experiments under reservoir conditions were conducted, analyzing dynamic differential pressure, in situ saturation changes (measured with a high-pressure acoustic separator), and pre- and postexperiment core properties. The results showed distinct differences between dry and wet CO2 injection, particularly regarding the vaporization and salt precipitation effects on permeability. Dry CO2 injection reduced water saturation to as low as 4% PV, simulating dry-out near injection wells, and caused absolute permeability changes of 21% on average due to salt precipitation. In contrast, wet CO2 injection, representative of bulk reservoir flow, preserved high water saturations without salt precipitation. Additionally, the final relative permeability to supercritical CO2 (KrscCO2) was higher for the dried core (0.62) compared to that of the wet injection experiment (0.40). This suggests that water vaporization during dry CO2 injection enhances CO2 effective permeability despite salt precipitation. Comparing wet CO2 injections in samples with different permeabilities using dimensionless numbers revealed that unstable flow in high-permeability channels leads to higher overall relative permeability and residual water saturation. The comprehensive experimental data from this study provide valuable insights for simulating two-phase scCO2–brine displacement and dissolution processes under reservoir conditions.
UR - http://www.scopus.com/inward/record.url?scp=85218864187&partnerID=8YFLogxK
U2 - 10.1021/acs.energyfuels.4c06131
DO - 10.1021/acs.energyfuels.4c06131
M3 - Article
SN - 0887-0624
VL - 39
SP - 4395
EP - 4411
JO - Energy & Fuels
JF - Energy & Fuels
IS - 9
ER -