
TY  - JOUR
A1  - Saito, H. 
A1  - Nobuoka, D. 
A1  - Azuma, H. 
A1  - Xue, Z. 
A1  - Tanase, D. 
T1  - Time-lapse crosswell seismic tomography for monitoring injected CO2 in an onshore aquifer, Nagaoka, Japan
JF  - Exploration Geophysics
JO  - Explor. Geophys.
Y1  - 2006
VL  - 37
IS  - 1
SP  - 30
EP  - 36
KW  - 
UR  - https://doi.org/10.1071/EG06030 
N2  - Japan?s first pilot-scale CO2 sequestration experiment has been conducted in Nagaoka, where 10 400 t of CO2 have been injected in an onshore aquifer at a depth of about 1100 m. Among various measurements conducted at the site for monitoring the injected CO2, we conducted time-lapse crosswell seismic tomography between two observation wells to determine the distribution of CO2 in the aquifer by the change of P-wave velocities. This paper reports the results of the crosswell seismic tomography conducted at the site. The crosswell seismic tomography measurements were carried out three times; once before the injection as a baseline survey, and twice during the injection as monitoring surveys. The velocity tomograms resulting from the monitoring surveys were compared to the baseline survey tomogram, and velocity difference tomograms were generated. The velocity difference tomograms showed that velocity had decreased in a part of the aquifer around the injection well, where the injected CO2 was supposed to be distributed. We also found that the area in which velocity had decreased was expanding in the formation up-dip direction, as increasing amounts of CO2 were injected. The maximum velocity reductions observed were 3.0% after 3200 t of CO2 had been injected, and 3.5% after injection of 6200 t of CO2. Although seismic tomography could map the area of velocity decrease due to CO2 injection, we observed some contradictions with the results of time-lapse sonic logging, and with the geological condition of the cap rock. To investigate these contradictions, we conducted numerical experiments simulating the test site. As a result, we found that part of the velocity distribution displayed in the tomograms was affected by artefacts or ghosts caused by the source-receiver geometry for the crosswell tomography in this particular site. The maximum velocity decrease obtained by tomography (3.5%) was much smaller than that observed by sonic logging (more than 20%). The numerical experiment results showed that only 5.5% velocity reduction might be observed, although the model was given a 20% velocity reduction zone. Judging from this result, the actual velocity reduction can be more than 3.5%, the value we obtained from the field data reconstruction. Further studies are needed to obtain more accurate velocity values that are comparable to those obtained by sonic logging. 
ER  -

