首页> 外文OA文献 >Exploring the Potential Linkages Between Oil-Field Brine Reinjection, Crystalline Basement Permeability, and Triggered Seismicity for the Dagger Draw Oil Field, Southeastern New Mexico, USA, Using Hydrologic Modeling
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Exploring the Potential Linkages Between Oil-Field Brine Reinjection, Crystalline Basement Permeability, and Triggered Seismicity for the Dagger Draw Oil Field, Southeastern New Mexico, USA, Using Hydrologic Modeling

机译:使用水文模型探索美国新墨西哥州东南部Dagger Draw油田的油田卤水注入,结晶基底渗透率和触发地震之间的潜在联系

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摘要

We used hydrologic models to explore the potential linkages between oil-field brine reinjection and increases in earthquake frequency (up to Md 3.26) in southeastern New Mexico and to assess different injection management scenarios aimed at reducing the risk of triggered seismicity. Our analysis focuses on saline water reinjection into the basal Ellenburger Group beneath the Dagger Draw Oil field, Permian Basin. Increased seismic frequency (\u3eMd 2) began in 2001, 5 years after peak injection, at an average depth of 11 km within the basement 15 km to the west of the reinjection wells. We considered several scenarios including assigning an effective or bulk permeability value to the crystalline basement, including a conductive fault zone surrounded by tighter crystalline basement rocks, and allowing permeability to decay with depth. We initially adopted a 7 m (0.07 MPa) head increase as the threshold for triggered seismicity. Only two scenarios produced excess heads of 7m five years after peak injection. In the first, a hydraulic diffusivity of 0.1 m2s-1 was assigned to the crystalline basement. In the second, a hydraulic diffusivity of 0.3 m2s-1 was assigned to a conductive fault zone. If we had considered a wider range of threshold excess heads to be between 1 and 60m, then the range of acceptable hydraulic diffusivities would have increased (between 0.1-0.01 m2s-1 and 1-0.1 m2s-1 for the bulk and fault zone scenarios, respectively). A permeability–depth decay model would have also satisfied the 5-year time lag criterion. We also tested several injection management scenarios including redistributing injection volumes between various wells and lowering the total volume of injected fluids. Scenarios that reduced computed excess heads by over 50% within the crystalline basement resulted from reducing the total volume of reinjected fluids by a factor of 2 or more.
机译:我们使用水文模型探讨了在新墨西哥州东南部油田注入盐水和地震频率增加(高达Md 3.26)之间的潜在联系,并评估了旨在降低触发地震风险的不同注入管理方案。我们的分析集中在二叠纪盆地Dagger Draw油田下方的基础Ellenburger组中注入盐水。地震频率(增加)在2001年开始,即注入高峰后的5年,在回注井以西15 km的地下室平均深度为11 km。我们考虑了几种方案,包括为晶体基底分配有效渗透率或整体渗透率值,包括由更紧密的晶体基底岩石围绕的导电断层带,以及使渗透率随深度衰减。我们最初采用增加7 m(0.07 MPa)的水头作为触发地震的阈值。注入高峰后的五年,只有两种情况产生了超过700万的压头。首先,将0.1 m2s-1的水力扩散系数分配给该晶体基底。在第二步中,将水力扩散率为0.3 m2s-1分配给导电断层带。如果我们认为更大的阈值超额压差范围在1至60m之间,那么可接受的水力扩散率范围将会增加(对于大体积和断层带方案,介于0.1-0.01 m2s-1和1-0.1 m2s-1之间, 分别)。渗透率-深度衰减模型也将满足5年时滞标准。我们还测试了几种注入管理方案,包括在各个井之间重新分配注入量并降低注入流体的总量。在结晶基底内将计算的多余水头降低了50%以上的方案是由于将回注流体的总体积减少了2倍或更多。

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