Complementary Subsurface Characterization Methods to Develop a Geologic Model for the EGS Collab Experiment, Sanford Underground Research Facility

The EGS (Enhanced Geothermal Systems) Collab project was performed within the Sanford Underground Research Facility (SURF) with a goal of understanding processes and evaluation of models related to hydraulic stimulation of rock at depth. The present work deals with the development of Testbed 2 where experiments were conducted at a depth of 1.25 km and were located within a well-characterized testbed in a metamorphic, amphibolite host rock. A total of eleven boreholes varying in length between 10.6 m and 81.2 m were continuously cored to develop the testbed. In addition to the continuous coring of the amphibolite host rock, geophysical instrumentation supporting electrical resistivity tomography (ERT), microearthquake (MEQ) detection, and optical fiber providing distributed temperature sensing (DTS) and distributed acoustic sensing (DAS) were installed in the monitoring boreholes, all of which produced a comprehensive complementary suite of characterization and monitoring technologies. Pre-stimulation characterization of the groundwater conditions identified only two hydraulically significant fractures, neither of which transects the central portion of the testbed. Flow and pressure monitoring indicated low preexisting pore pressure conditions likely affected by the mine openings.. Authors: Roggenthen, W. [South Dakota School of Mines and Technology, Rapid City, SD (United States)]; Kneafsey, Timothy [Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)]; Burghardt, J. [Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)]; Doe, T. [US Department of Energy (USDOE), Redmond, WA (United States). Geothermal Technologies Office]; Hopp, C. [Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)]. DOE Contract: AC02-05CH11231. Subjects: 15 GEOTHERMAL ENERGY; 58 GEOSCIENCES; electrical resistivity tomography; fractures; geothermal; microearthquakes