
Enhanced seismicity monitoring in central Alberta, Canada: 2020–2022
Geothermal energy has emerged in recent years as a potential alternative green technology to address an ever-increasing demand by the world for energy. This study focuses on a geothermal prototype system in Alberta, Canada whereby fluid circulating in the system never enters the surrounding rock, and instead acts in a similar manner to a radiator, using conduction to heat the fluid returning to the surface. We installed a local monitoring array within 10 km of the geothermal operations to monitor for any potential microseismicity over a 2-year period. Using a machine learning data analysis approach, we identified 94 seismic events within a350 km radius of the geothermal operations, with magnitudes ranging from ML 0.94 to ML 4.09. Events detected included natural and induced events (e.g. from quarry blasting). However, no seismicity was detected within 30 km of the operations. The fact that small magnitude events were detected by the monitoring equipment, but not in the vicinity of the operations, gives us confidence that no events ML > 1 were likely induced by the geothermal activities during the 2-year monitoring period.