South-Central Section - 49th Annual Meeting (19–20 March 2015)

Paper No. 2
Presentation Time: 9:00 AM-4:00 PM

SHALLOW GROUNDWATER MONITORING BEFORE AND AFTER CO2 SEQUESTRATION IN SOUTH CENTRAL KANSAS


KREHEL, Austin W., Department of Geology, Kansas State University, 108 Thompson hall, Manhattan, KS 66506, DATTA, Saugata, Department of Geology, Kansas State University, 104 Thompson Hall, Manhattan, KS 66506, WATNEY, W. Lynn, Kansas Geological Survey, Univ of Kansas, 1930 Constant Avenue, Lawrence, KS 66047 and BIRDIE, Tiraz, TBirdie Consulting, Inc, lawrence, KS 66047, awkrehel@gmail.com

A CO2 injection pilot project is currently being conducted at Wellington Field, Sumner County, south-central Kansas. Injection will be performed in two phases to demonstrate CO2-Enhanced Oil Recovery (EOR) and permanent carbon storage potential. CO2-EOR is expected to commence in 2015, within the Mississippian carbonate reservoir. Pending the containment and integrity of CO2 injected for EOR, injection for permanent storage is expected to commence in 2015, within the deep saline Arbuckle aquifer. Each phase will include approximately 26,000 metric tons of supercritical CO2 (sCO2) injected within a period of 8 months.

A pre-injection baseline of chemical and physical parameters has been established to define the hydrogeochemistry of shallow depths on two monitoring wells (100’ and 200’ depths) within the Upper Wellington Formation – a possible Underground Source of Drinking Water (USDW), and will be established for two additional shallow wells. Some important parameters used to establish the baseline for the (100’, 200’) wells are ORP (133.7, 120.5 mV), pH (6.93, 6.65), conductivity (83.9, 68.4 mS/cm, dissolved oxygen (3, 1.5 mg/L), alkalinity (100, 60 mg/L), and chloride (40,000, 100,000 mg/L). These parameters will be measured on the nest of four shallow monitoring wells regularly following injection of both phases to assess if leakage and migration of CO2 to shallower water sources is occurring, and what effects it has on the possible USDW. A pre-injection baseline will also be conducted on two monitoring wells to assess the Mississippian hydrogeochemistry, and has been conducted on the Arbuckle. Following injections from both phases, water from these wells will be monitored to address the activity of CO2. An U-tube sampler will be employed to collect in-situ samples from these wells following injection. The samples will be analyzed for tracers, and physical and chemical parameters.