S010-0002
Short‐Term Probabilistic Hazard Assessment in Regions of Induced Seismicity

Tuesday, 8 December 2020
Poster
Ganyu Teng, Stanford University, Civil and Environmental Engineering, Stanford, CA, United States and Jack W Baker, Stanford Univ, Stanford, CA, United States
Abstract:
This project introduces short‐term hazard assessment frameworks for regions with induced seismicity. For hydraulic‐fracturing‐induced earthquakes, the short‐term hazard is defined as the hazard induced during the injection. For wastewater‐disposal‐induced earthquakes, it is the hazard within a few days after an observed earthquake. In West Texas, hydraulic‐fracturing‐induced earthquakes cluster around the injection activities, and the earthquake occurrence varies greatly in time and space. We develop a method to estimate the hazard level at the production site during the injection, based on past injection and earthquake records. The results suggest that the injection volume has a negligible effect on the short‐term earthquake occurrence in this region, because injection volumes per well fall within a relatively narrow range, whereas the regional variations in seismic productivity of wells and b‐values are important. The framework could be easily modified for implementation in other regions with hydraulic‐fracturing‐induced earthquakes. We then compare the framework with wastewater‐disposal‐induced earthquakes in Oklahoma–Kansas and natural earthquakes in California. We found that drivers of short‐term seismic hazard differ for the three cases. In West Texas, clustered earthquakes dominate seismic hazards near production sites. However, for Oklahoma–Kansas and California, the short‐term earthquake occurrence after an observed mainshock could be well described by the mainshock–aftershock sequence. For Stillwater in Oklahoma, aftershocks contribute less to the hazard than San Francisco in California, due to the high Poissonian mainshock rate. For example, for the rate of exceeding a Modified Mercalli Intensity of 3 within 7 days after an M4 earthquake, the aftershock sequence from natural earthquakes contributed 85% of the hazard level in San Francisco, whereas the aftershock contribution was only 60% for induced earthquakes in Stillwater. Although different models were implemented for hazard calculations in regions with hydraulic fracturing versus wastewater injection, injection activities could be drivers of short‐term hazards in both cases.