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Experimental study on CO2 monitoring and quantification of stored CO2 in saline formations using resistivity measurements
Authors:Yoshihiro Nakatsuka  Ziqiu Xue  Henry Garcia  Toshifumi Matsuoka
Affiliation:1. Department of Civil and Earth Engineering, Kyoto University, Kyoto 615-8540, Japan;2. Japan Oil Gas and Metals National Corporation, Chiba 261-0025, Japan;3. Research Institute of Innovative Technology for the Earth, Kyoto 619-0292, Japan;1. Earth Sciences Division, Lawrence Berkeley National Laboratory, One Cyclotron Road, Berkeley, CA 94720, United States;2. Department of Geoscience, Aarhus University, C.F. Møllers Allé 4, DK-8000 Aarhus, Denmark;3. Atmospheric, Earth, and Energy Division, Lawrence Livermore National Laboratory, 7000 East Avenue, Livermore, CA 94550, United States;4. Bureau of Economic Geology, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78713, United States;1. Department of Geoscience, 2500 University Drive NW, University of Calgary, Calgary, Alberta, Canada T2N 1N4;2. Carbon Management Canada Inc., 3535 Research Road NW, Calgary, Alberta, Canada T2L 2K8;3. Shell Canada Limited, 400, 4th Avenue SW, Calgary, Alberta, Canada T2P 2H5;4. GeoZentrum Nordbayern, Department of Geography and Geosciences, Friedrich-Alexander Universität Erlangen-Nürnberg, Schlossgarten 5, 91056 Erlangen, Germany;1. Institut de Recerca, Centre Mixt d’Investigació GEOMODELS, Group of Geodynamics and Basin Analysis, Dept. Geodinàmica i Geofísica, Universitat de Barcelona (UB), Spain;2. Fundación Ciudad de la Energía (CIUDEN), Ponferrada, Spain;1. Earth & Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USA;2. SCCER-SoE, Department of Earth Sciences, ETH Zürich, Zürich, Switzerland
Abstract:This paper reports CO2 saturation estimations based on resistivity data obtained from laboratory measurements and induction logging results at the Nagaoka pilot CO2 injection site. The laboratory experiments put in evidence that the presence of clay content tends to reduce the increase of resistivity caused by the displacement of brine by less conductive CO2. As a result, CO2 saturations estimated from resistivity measurements without any correction for the clay effect are considerably lower than the actual saturations. The resistivity index (RI) provides better estimates of CO2 saturations than the Archie's equation because it requires the determination or assumption of only one rock parameter: the saturation exponent. CO2 saturations estimated from the induction logging data acquired at Nagaoka are considerably lower than the neutron porosity changes due to displacement between brine and CO2 in the reservoir. Even in the case of considering the De Witte's equation and the Poupon's to account for the clay effect, it was still difficult to get a good agreement with the neutron logging results. New relations based on the resistivity index with correction factors for the clay effect are developed and implemented in this study. One of these relations has proved to be effective to estimate CO2 saturations in saline formations with high clay content.
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