TY - JOUR
T1 - Time-lapse monitoring of shallow subsurface in the Aquistore CO2 storage site from surfacewave analysis using a continuous and controlled seismic source
AU - Ikeda, T.
AU - Tsuji, T.
AU - Takanashi, M.
AU - Kurosawa, I.
AU - Nakatsukasa, M.
AU - Worth, K.
AU - White, D.
AU - Roberts, B.
N1 - Publisher Copyright:
© 2016 SEG.
PY - 2016
Y1 - 2016
N2 - We performed time-lapse surface-wave analysis to monitor the shallow subsurface at the Aquistore CO2 storage site, managed by the Petroleum Technology Research Centre, Canada. A continuous and controlled seismic source system called the Accurately Controlled Routinely Operated Signal System (ACROSS) is used to enhance the temporal resolution and source repeatability in the monitoring. We extracted hourly-variation of surface-wave phase velocities from continuous seismic data with 4 hour stacking. As a result, we could monitor phase velocities within 1 % accuracy during 1-9 days in the frequency range of 4.5-6 Hz. We identified 2-5 % seasonal variation of phase velocities. The high phase velocities observed in winter can be explained by the degree of freezing of partially saturated rock. Our time-lapse results contributed to improving the accuracy of monitoring deep reflections from the CO2 injection reservoir by correcting seasonal variations of nearsurface velocity. The high temporal resolution and accuracy of our monitoring results have the potential to identify sudden changes such as CO2 leakage from CO2 storage sites.
AB - We performed time-lapse surface-wave analysis to monitor the shallow subsurface at the Aquistore CO2 storage site, managed by the Petroleum Technology Research Centre, Canada. A continuous and controlled seismic source system called the Accurately Controlled Routinely Operated Signal System (ACROSS) is used to enhance the temporal resolution and source repeatability in the monitoring. We extracted hourly-variation of surface-wave phase velocities from continuous seismic data with 4 hour stacking. As a result, we could monitor phase velocities within 1 % accuracy during 1-9 days in the frequency range of 4.5-6 Hz. We identified 2-5 % seasonal variation of phase velocities. The high phase velocities observed in winter can be explained by the degree of freezing of partially saturated rock. Our time-lapse results contributed to improving the accuracy of monitoring deep reflections from the CO2 injection reservoir by correcting seasonal variations of nearsurface velocity. The high temporal resolution and accuracy of our monitoring results have the potential to identify sudden changes such as CO2 leakage from CO2 storage sites.
UR - http://www.scopus.com/inward/record.url?scp=85019124420&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85019124420&partnerID=8YFLogxK
U2 - 10.1190/segam2016-13822593.1
DO - 10.1190/segam2016-13822593.1
M3 - Conference article
AN - SCOPUS:85019124420
SN - 1052-3812
VL - 35
SP - 5479
EP - 5484
JO - SEG Technical Program Expanded Abstracts
JF - SEG Technical Program Expanded Abstracts
T2 - SEG International Exposition and 86th Annual Meeting, SEG 2016
Y2 - 16 October 2011 through 21 October 2011
ER -