G33A-1132
First results of geodetic deformation monitoring after commencement of CO2 injection at the Aquistore underground CO2 storage site

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Michael Craymer1, Don White2, Mieczyslaw Piraszewski1, Yanlai Zhao1, Joseph Henton3, Jason Silliker1 and Sergey Samsonov4, (1)Natural Resources Canada, Canadian Geodetic Survey, Ottawa, ON, Canada, (2)Natural Resources Canada, Geological Survey of Canada, Ottawa, ON, Canada, (3)Natural Resources Canada, Canadian Geodetic Survey, Sidney, BC, Canada, (4)Natural Resources Canada, Canada Centre for Remote Sensing, Ottawa, ON, Canada
Abstract:
Aquistore is a demonstration project for the underground storage of CO2 at a depth of ~3350 m near Estevan, Saskatchewan, Canada. An objective of the project is to design, adapt, and test non-seismic monitoring methods that have not been systematically utilized to date for monitoring CO2 storage projects, and to integrate the data from these various monitoring tools to obtain quantitative estimates of the change in subsurface fluid distributions, pressure changes and associated surface deformation. Monitoring methods being applied include satellite-, surface- and wellbore-based monitoring systems and comprise natural- and controlled-source electromagnetic methods, gravity monitoring, continuous GPS, synthetic aperture radar interferometry (InSAR), tiltmeter array analysis, and chemical tracer studies. Here we focus on the GPS, InSAR and gravity monitoring. Five monitoring sites were installed in 2012 and another six in 2013, each including GPS and InSAR corner reflector monuments (some collocated on the same monument). The continuous GPS data from these stations have been processed on a daily basis in both baseline processing mode using the Bernese GPS Software and precise point positioning mode using CSRS-PPP. Gravity measurements at each site have also been performed in fall 2013, spring 2014 and fall 2015, and at two sites in fall 2014. InSAR measurements of deformation have been obtained for a 5 m footprint at each site as well as at the corner reflector point sources. Here we present the first results of this geodetic deformation monitoring after commencement of CO2 injection on April 14, 2015. The time series of these sites are examined, compared and analyzed with respect to monument stability, seasonal signals, longer term trends, and any changes in motion and mass since CO2 injection.