4.5 Article

Directional Hydraulic Characteristics of Reservoir Rocks for CO2 Geological Storage in the Pohang Basin, Southeast Korea

Journal

ENERGIES
Volume 14, Issue 8, Pages -

Publisher

MDPI
DOI: 10.3390/en14082211

Keywords

carbon capture and storage (CCS); CO2 geological storage; permeability; directional permeability

Categories

Funding

  1. Basic Research Program of the Korea Institute of Geoscience and Mineral Resources [GP2020-006]
  2. Energy Efficiency and Resources Program of the Korea Institute of Energy Technology Evaluation and Planning (KETEP) - Korean Government-Ministry of Knowledge Economy [20162010201980]

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This study conducted core sampling of a potential CO2 storage site in southeast Korea and identified two promising geological formations as prospective CO2 storage reservoirs. Injection efficiency, CO2 migration, and directional transport properties were evaluated using core plugs measurements and flow modeling. The analysis showed a higher injection efficiency at a depth of 739 m compared to 779 m, with correlations among directional permeabilities useful for assessing CO2 storage capacity, injectivity, and leakage risk.
This study conducted core sampling of an offshore borehole for geological reservoir characterization of a potential CO2 storage site in southeast Korea. From this, two promising geological formations at similar to 739 and similar to 779 m were identified as prospective CO2 storage reservoirs. Injection efficiency and CO2 migration were evaluated based on directional measurements of permeabilities from core plugs. The directional transport properties were determined using both a portable probe permeameter and a pressure cell capable of applying different in situ confining pressures. Both steady state and unsteady state measurements were used to determine permeability-the method selected according to the expected permeability range of the specific sample. This expected range was based on rapid screening measurements acquired using a portable probe permeameter (PPP). Anticipated performance of the prototypical CO2 injection site was evaluated based on flow modeling of the CO2 plume migration pathway including CO2 transport through the overlying formations based on the measured directional hydraulic properties. These analyses revealed that the injection efficiency at a depth of 739 m was double that at 779 m. These correlations among and distributions of the directional permeabilities of the potential CO2 geological storage site can be utilized for the assessment of CO2 storage capacity, injectivity, and leakage risk.

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