HR: 1340h
AN: H13F-1641    [Abstracts]
TI: Resistivity Variation due to CO2 Migration in Different Temperature and Pressure Conditions
AU: * Nakatsuka, Y
EM: nakatsuka@earth.kumst.kyoto-u.ac.jp
AF: Kyoto University Faculty of Engineering, C1-1-118,Kyoto Daigaku Katsura,Nishikyo-ku, Kyoto, 6158540, Japan
AU: Onishi, K
AF: Kyoto University Faculty of Engineering, C1-1-111,Kyoto Daigaku Katsura,Nishikyo-ku, Kyoto, 6158540, Japan
AU: Yamada, Y
AF: Kyoto University Faculty of Engineering, C1-1-108,Kyoto Daigaku Katsura,Nishikyo-ku, Kyoto, 6158540, Japan
AU: Matsuoka, T
AF: Kyoto University Faculty of Engineering, C1-1-109,Kyoto Daigaku Katsura,Nishikyo-ku, Kyoto, 6158540, Japan
AU: Xue, Z
AF: Research Institute of Innovative Technology for the Earth, 9-2 Kizugawadai,Kizu- cho,Soraku-gun, Kyoto, 6190292, Japan
AB: CO2 geological sequestration is one of the effective approaches solving the global warming problem. Captured CO2 is injected to the deep aquifers or depleted oil and gas fields. Injected CO2 migrates thorough the reservoir rock, however, the details behavior of injected CO2 under the ground at super critical phase is not yet fully understood. Migration of injected CO2 will change by the condition of the injected reservoir such as the temperature and pressure. Also density and permeability of the rock may be changed due to temperature or pressure variations. These changes control the migration behavior of injected CO2. In this study, experiments of resistivity measurements were conducted to detect the migration difference of CO2 in different temperature and pressure conditions by using sandstone core samples. Core sample was taken from Berea sandstone and processed to 5cm diameter and 12cm length. For the resistivity measurement, impression electrode was set on the both end and the measurement electrode of ring condition was set on the side of the rock sample. We stetted the core sample in the pressure vessel and recreated the condition of underground reservoir which is high pressure and high temperature. We injected supercritical CO2 in different pressure and temperature for each experiment. Pressure was changed in range of 8 to 11MPa and temperature was changed in range of 35° to 45°. This means that all the experiments were conducted in supercritical phase. From the measured resistivity variation, we verified the migration of CO2 and compared the migration behavior of CO2 in different conditions.
DE: 1895 Instruments and techniques: monitoring
DE: 4930 Greenhouse gases
DE: 5109 Magnetic and electrical properties (0925)
DE: 5114 Permeability and porosity
SC: Hydrology [H]
MN: 2007 Fall Meeting