Barnes Caitlin, Halihan Todd
Oklahoma State University, 105 Noble Research Center, Stillwater, OK 74078.
Ground Water. 2019 Jan;57(1):86-96. doi: 10.1111/gwat.12657. Epub 2018 Mar 30.
A systematic review across U.S. Geological Survey (USGS) identified potentially induced seismic locations was conducted to discover seismic distance patterns and trends over time away from injection disposal wells. Previous research indicates a 10 km (6 miles) average where the majority of induced seismicity is expected to occur within individual locations, with some areas reporting a larger radius of 35 km (22 miles) to over 70 km (43 miles). This research analyzed earthquake occurrences within nine USGS locations where specified wells were identified as contributors to induced seismicity to determine distance patterns from disposal wells or outward seismic migration over time using established principles of hydrogeology. Results indicate a radius of 31.6 km (20 miles) where 90% of felt earthquakes occur among locations, with the closest proximal felt seismic events, on average, occurring 3 km (1.9 miles) away from injection disposal wells. The results of this research found distance trends across multiple locations of potentially induced seismicity.
美国地质调查局(USGS)对已确定的潜在诱发地震地点进行了一项系统综述,以发现随着时间推移远离注入处置井的地震距离模式和趋势。先前的研究表明,大多数诱发地震预计发生在各个地点的平均距离为10公里(6英里),一些地区报告的半径更大,为35公里(22英里)至70多公里(43英里)。本研究分析了美国地质调查局九个地点内的地震发生情况,在这些地点特定的井被确定为诱发地震的成因,以利用既定的水文地质原理确定与处置井的距离模式或随时间向外的地震迁移。结果表明,90%的有感地震发生在各地点之间的半径为31.6公里(20英里)的范围内,平均而言,最近的近端有感地震事件发生在距注入处置井3公里(1.9英里)处。本研究结果发现了多个潜在诱发地震地点的距离趋势。