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The EGS Collab Hydrofracture Experiment at the Sanford Underground Research Facility - Campaign Cross-Borehole Seismic Characterization

机译:Sanford地下研究设施的EGS Collab压裂实验-运动跨井眼地震表征

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The enhanced geothermal system (EGS) multi-laboratory and multi-university collaborative (Collab) project brings together skilled and experienced scientists and engineers in the areas of subsurface process modeling, monitoring, and a series of experiments to focus on intermediate-scale EGS reservoir generation processes and related model validation at crystalline rock sites. Cooperative research under the EGS Collab project will provide a foundation of knowledge and modeling capability that form a bridge to meeting the challenges of EGS development and proliferation. The EGS Collab project is being performed within the re-purposed mine workings (drifts) of Sanford Underground Research Facility (SURF), located in Lead, South Dakota, USA. For the first experiment, a suite of sub-horizontal boreholes was drilled from within one of the SURF mine drifts directly into the surrounding crystalline rock formation. The suite is comprised of one stimulation well, one production well, and six monitoring wells. The goal of this experiment is to generate fractures radiating from the stimulation well that intersect the production well, and then perform flow testing of this inter-well/hydrofracture system. Stimulation and flow is monitored with micro-earthquake (MEQ) and acoustic emission (AE) instrumentation that is grouted into the monitoring wells. A fundamental component of MEQ/AE monitoring requires campaign-style cross-borehole seismic characterization. Cross-borehole techniques include compressional (P-) and Shear (S-) wave tomography. The results provide baseline P- and S-wave velocity models that are critical in calibrating hypocenter locations from MEQ/AE monitoring, and also yield elastic moduli data/constraints that will be utilized for stimulation modeling. A supplemental goal is to perform velocity change detection analysis by collecting cross-borehole P- and S-wave data between the stimulation and production wells prior and subsequent to fracture stimulation.
机译:增强的地热系统(EGS)多实验室和多大学协作(COLLAB)项目在地下过程建模,监测和一系列实验中携带熟练和经验丰富的科学家和工程师,以专注于中间级EGS水库晶体岩位点的生成过程及相关模型验证。 EGS Collab项目下的合作研究将为知识和建模能力提供,形成桥梁,以满足EGS开发和扩散的挑战。 EGS Collab项目正在桑福德地下研究设施(海浪)的重新铺设矿山工作(漂移)内进行,位于美国南达科他州的领先地位。对于第一次实验,从一个冲浪矿床内直接进入周围的晶体岩层的一个水平钻孔套装。该套件由一个刺激孔组成,一个生产良好,六个监测井。该实验的目标是产生从与生产井相交的刺激孔的骨折,然后对该井间/水力折衷系统进行流动测试。用微地震(MEQ)和声发射(AE)仪器监测刺激和流动,该仪器灌注到监测孔中。 MEQ / AE监控的基本组成部分需要竞选式交叉钻孔地震表征。交叉钻孔技术包括压缩(P-)和剪切(S-)波断层扫描。结果提供了基线P-和S波速度模型,这在校准MEQ / AE监测中校准低缩进位置,并且还产生将用于刺激建模的弹性模数/约束。补充目标是通过在裂缝刺激之前和之后收集刺激和生产井之间的交叉钻孔P-和S波数据进行速度变化检测分析。

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