Seismicity Characterization and Monitoring at WESTCARB's Proposed Montezuma Hills Geologic Sequestration Site

Daley, T.M. ; Haught, R. ; Peterson, J.E. ; Boyle, K. ; Beyer, J.H. ; Hutchings, L.R.

关键词: 54;    58;    CALIFORNIA;    CARBON DIOXIDE;    CARBON SEQUESTRATION;    COMMUNITIES;    FRACTURES;    GROUND MOTION;    MONITORING;    SEISMIC EVENTS;    SEISMICITY;    SITE CHARACTERIZATION;    STORAGE;    TECTONICS;   

DOI  :  10.2172/992490
RP-ID  :  LBNL-4006E
PID  :  OSTI ID: 992490
Others  :  TRN: US201023%%146

美国|英语

来源: SciTech Connect

【 摘 要 】

The West Coast Regional Carbon Sequestration Partnership (WESTCARB), in collaboration with Shell Oil Co. performed site characterization for a potential small-scale pilot test of geologic sequestration of carbon dioxide (CO2). The site area, know as Montezuma Hills, is near the town of Rio Vista in northern California. During the process of injection at a CO2 storage site, there is a potential for seismic events due to slippage upon pre-existing discontinuities or due to creation of new fractures. Observations from many injection projects have shown that the energy from these events can be used for monitoring of processes in the reservoir. Typically, the events are of relatively high frequency and very low amplitude. However, there are also well documented (non-CO2-related) cases in which subsurface injection operations have resulted in ground motion felt by near-by communities. Because of the active tectonics in California (in particular the San Andreas Fault system), and the potential for public concern, WESTCARB developed and followed an induced seismicity protocol (Myer and Daley, 2010). This protocol called for assessing the natural seismicity in the area and deploying a monitoring array if necessary. In this report, we present the results of the natural seismicity assessment and the results of an initial temporary deployment of two seismometers at the Montezuma Hills site. Following the temporary array deployment, the project was suspended and the array removed in August of 2010.