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首页> 外文期刊>Geophysical Research Letters >Potential Link Between 2020 Mentone, West Texas M5 Earthquake and Nearby Wastewater Injection: Implications for Aquifer Mechanical Properties
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Potential Link Between 2020 Mentone, West Texas M5 Earthquake and Nearby Wastewater Injection: Implications for Aquifer Mechanical Properties

机译:2020 Mentone,West Texas M5地震和附近废水注射液之间的潜在环节:对含水层机械性能的影响

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摘要

The M5 Mentone earthquake that occurred on March 26, 2020, was the largest event recorded over the last 2 decades in West Texas within the Delaware Basin, a U.S. major petroleum-producing area. Also, numerous hydrofracturing and wastewater disposal wells are spread across this region. Within a 30 km distance to mainshock, eight class-II injection wells for industrial wastewater disposal target the deep porous Ellenburger aquifer at an average rate of 1.36 x 10(6) barrel (BBL) per month during 2012-2020. Poroelastic models of fluid diffusion show these nearby injectors collectively imparted up to 80.5 kPa of Coulomb stress at the mainshock location, capable of triggering this M5 event. Assuming the Mentone event occurs when pore-pressure increase is maximum, the time delay between peak injection and the M5 occurrence corresponds with an optimal permeability of 6.76 x 10(-14) m(2) for the Ellenburger aquifer layer, in agreement with independent estimates.
机译:2020年3月26日发生的M5 Mentone地震是过去20年中德克萨斯州西部特拉华盆地内记录的最大地震,特拉华盆地是美国主要石油产区。此外,许多水力压裂和废水处理井遍布该地区。2012-2020年间,在距离mainshock 30公里的范围内,八口用于工业废水处理的二级注入井以平均每月1.36 x 10(6)桶(BBL)的速度将深层多孔埃伦堡含水层作为目标。流体扩散的多孔弹性模型显示,这些附近的喷射器在主震位置集体施加高达80.5 kPa的库仑应力,能够触发M5事件。假设孔隙压力增加最大时发生Mentone事件,峰值注入和M5事件之间的时间延迟对应于埃伦堡含水层的最佳渗透率为6.76 x 10(-14)m(2),与独立估计一致。

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