S24A-05
Geophysical Methods for CO2 Leak Detection and Plume Monitoring at the Southeast Regional Carbon Sequestration (SECARB) Anthropogenic Test Site near Citronelle, Alabama

Tuesday, 15 December 2015: 17:00
305 (Moscone South)
Robert C Trautz1, George J Koperna2, David E Riestenberg2, Thomas M Daley3 and Richard G Rhudy1, (1)Electric Power Research Institute Paolo Alto, Palo Alto, CA, United States, (2)Advanced Resources International, Arlington, VA, United States, (3)Lawrence Berkeley National Laboratory, Berkeley, CA, United States
Abstract:
The SECARB project is the largest demonstration of CO2 capture, transportation, injection and storage from a coal-fired power station in the US. In August 2012, SECARB began capturing CO2 emitted by Unit 5 at Plant Barry north of Mobile, Alabama and injecting it into the Paluxy Formation at a depth of 9,400 ft above the Citronelle oilfield.

Vertical seismic profile (VSP), cross-well and distributed acoustic sensing using fiber optics are being used to check for CO2 leakage out of the storage reservoir and track the CO2 plume. The acquisition plan includes one pre- and post-CO2 injection survey using an 80-level VSP array with a vibroseis source and cross-well using a piezoelectric source. “Snapshot” VSP surveys are performed every 6-12 months using a shorter 18-level geophone array installed on production tubing in the observation well.

Good quality results were produced for both the 80-level VSP and cross-well baseline surveys. Mixed results were obtained using the 18-level VSP array due to the smaller aperture, large depth to the target and thin sand layers receiving injected CO2. Time-lapse differencing shows weak illumination at the CO2 injection depth for only one far-offset source point. The lack of bright spots prompted SECARB to move the second cross-well survey up in the schedule. A second cross-well survey was conducted in June 2014. This time the hydrophones were deployed in the production tubing to avoid removing the 18-level array. The acquired data exhibited signal degradation compared to the baseline survey and tube waves interfered with the reflections. First arrivals were used to build a post-injection velocity tomogram. Differencing of the pre- and post-injection tomograms was performed, producing a time-lapse image of good quality. The resulting image (Figure) shows a significant velocity difference, indicating the CO2 plume has moved roughly 400 ft in zone. More importantly, no velocity anomaly or leakage is evident above the storage reservoir.