论文标题
低磁性地震性,带有下孔分布的声感应阵列 - 伪造地热实验的示例
Low-magnitude Seismicity with a Downhole Distributed Acoustic Sensing Array -- examples from the FORGE Geothermal Experiment
论文作者
论文摘要
我们显示了下孔分布的声感应(DAS)阵列在检测,定位和表征在犹他州地热能量(Forge)位点研究中发生的低稳定地震的检测,定位和表征。在2019年4月至5月的最初刺激地热系统的初步刺激期间,在锻造地热部位的监测井中获得了10.5天的连续数据。犹他州矿物山下方的地震活动也发生在欧洲矿山山下的地震活动,也发生在Forge监测井的10公里内。在实验过程中,犹他大学地震仪站将来自这些地区的四个事件分类。我们对DAS数据的处理,包括模板匹配,在此期间发现了82次地震,其中16个在区域网络上可见。通过DAS处理获得的完整性的大小至少比Forge位点周围的致密表面阵列更好。虽然单个垂直DAS阵列由于其方位角歧义而在事件位置方面受到限制,但多个DAS井或井下阵列与表面站或近地面水平DAS的组合可以共同解决位置。所有检测到的事件都可能源自两个主动源区域,并且可以聚集在几个不同的家庭中。
We show the capabilities of a downhole Distributed Acoustic Sensing (DAS) array in detecting, locating and characterizing low-magnitude earthquakes occurring in the vicinity of the Frontier Observatory for Research in Geothermal Energy (FORGE) site in Utah. 10.5 days of continuous data were acquired in a monitoring well at the FORGE geothermal site during the initial stimulation of an Enhanced Geothermal System in April-May 2019. Earthquake activity beneath Mineral Mountains, Utah also occurred within 10 km of the FORGE monitoring well. During the experiment, four events from those areas were cataloged by the University of Utah Seismograph Stations. Our processing of DAS data, including template matching, finds 82 earthquakes during that period, of which 16 are visible on the regional network. The magnitude of completeness obtained by DAS processing is better by at least M=0.5 than the dense surface array around the FORGE site. While a single vertical DAS array is limited in terms of event location due to its azimuthal ambiguity, multiple DAS wells or a combination of a downhole array with surface stations or near-surface horizontal DAS could jointly resolve locations. All detected events probably originated from the two active source areas and can be clustered into several distinct families.