Quantifying CO2 Saturation from Time-Lapse Well Logging in an Onshore Saline Aquifer, Nagaoka, Japan

Ziqiu Xue, CO2 Sequestration Research Group, Research Institute of Innovative technology for the Earth, 9-2 Kizugawadai, Kizu-cho, soraku-gun, Kyoto, 619 0292, Japan, phone: 81 774 75 2312, fax: 81 774 75 2313, xue@rite.or.jp, Jiro Watanabe, Geophysical Surveying Co. Ltd, and Daiji Tanase, Engineering Advancement Association of Japan.

Injection of carbon dioxide (CO2) into saline aquifers has been proposed as a means to reduce greenhouse gas emissions. In geological carbon sequestration, monitoring is necessary to confirm the containment of CO2, assess leakage paths, and gain understanding into interactions between CO2, the rock-forming minerals and formation fluids. Monitoring is also necessary to quantify the net quantity of CO2 that has been sequestrated within the reservoirs. The major challenge is how to correlate wave velocity or electrical conductivity with fluid (CO2 or formation water) saturations in partially saturated porous rocks. A series of time-lapse geophysical loggings consisted of dual induction, neutron, sonic and gamma-ray has been performed frequently at the Nagaoka pilot-scale sequestration site. The pilot-scale CO2 injection site is located at Minami-Nagaoka oil and gas fields, and one injection well (IW-1) and three observation wells (OB-2,-3,-4) were drilled at the pilot site. The goal of this paper is to interpret and analyze time-lapse sonic log data quantitatively obtained from observation wells OB-2 and OB-4, to better understand fluid saturations around the two wells. The CO2 breakthrough was clearly confirmed from the sonic velocity reduction up to 20%. This significant velocity reduction agreed fairly well with the laboratory experiment result on drilled cores. Based on the rock-properties model and Gassmann's equation, we successfully matched the sonic velocity change due to presence of injected CO2 at observation wells. The CO2 saturation around the observation wells ranged from 10 to 40%. From the history matching result we also found that there is no CO2 leakage from the reservoir, even a huge earthquake hit the Nagaoka area. Our results strongly suggested the capability for quantifying CO2 concentration from seismic wave data with Gassmann's equation.