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Geomechanical aspects of CO2 sequestration in a deep saline reservoir in the Ohio River Valley region

机译:俄亥俄河谷地区深盐储层中固存二氧化碳的地质力学方面

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摘要

The Ohio River Valley CO2 Storage Project is an ongoing characterization of deep saline formations being considered as potential sites for geological CO2 sequestration. We completed a geomechanical analysis of the Rose Run Sandstone, a potential injection zone, and its adjacent formations at the American Electric Power's 1.3-GW Mountaineer Power Plant in New Haven, West Virginia. The results of this analysis were then applied to three investigations used to evaluate the feasibility of anthropogenic CO2 sequestration in the potential injection zone. First, we incorporated the results of the geomechanical analysis with a geostatistical aquifer model in CO2 injection-flow simulations to test the effects of introducing a hydraulic fracture to increase injectivity. We observed a nearly fourfold increase of injection rate caused by the introduction of a hydraulic fracture in the injection zone. The flow simulations predict that a single vertical well with a hydraulic fracture could inject a maximum of 300–400 kt of CO2/yr. In the second investigation, we determined that horizontal injection wells at the Mountaineer site are feasible because the high rock strength ensures that such wells would be stable in the local stress state. The third investigation used the geomechanical analysis results to evaluate the potential for injection-induced seismicity. If preexisting, but undetected, nearly vertical faults striking north-northeast or east-northeast are present, the increased pore pressure from CO2 injection would raise their reactivation potential. Geomechanical analysis of potential CO2 sequestration sites provides critical information required to evaluate its sequestration potential and associated risks.
机译:俄亥俄河谷CO 2 储藏项目正在进行中,对深盐岩层的描述 被认为是地质CO 2 < / sub>隔离。我们完成了对Rose Run砂岩,潜在注入区 及其在美国电力公司 1.3 GW登山家附近的地层的地质力学分析。西弗吉尼亚州纽黑文的发电厂。 然后将这一分析结果应用于三个调查中,用于评估人为CO 2 的可行性潜在注入区域中的sequestration 。首先,我们将地质力学分析的 结果与地层统计 含水层模型结合到CO 2 注入流模拟中,以测试 < / sup>引入水力压裂以增加注入量的效果。 我们观察到由于在注入中引入水力压裂而导致的 注入速率几乎增加了四倍。 区域。流动模拟预测,具有水力压裂的单个垂直井 每年最多可注入300–400 kt CO 2 / sub。在第二项调查中,我们确定Mountaineer站点的 水平注入井是可行的 ,因为高岩石强度确保了这些井 是稳定的在局部压力状态。第三次调查 使用了地质力学分析结果来评估注入诱发地震活动的潜力。如果存在 但早已发现但撞击东北或东北的近垂直断层,则CO 2 注入会增加孔隙压力sup> 将提高其重新激活的潜力。潜在的CO 2 螯合位点的地质力学分析 提供了评估其螯合潜力和相关的 风险所需的关键信息 。 sup>

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  • 来源
    《Environmental Geosciences》 |2006年第2期|85-103|共19页
  • 作者单位

    Department of Geophysics, Stanford University, Stanford, California 94305 luciera@pangea.stanford.edu;

    Department of Geophysics, Stanford University, Stanford, California 94305;

    Battelle Memorial Institute, 505 King Ave., Columbus, Ohio 432201-2693;

    Schlumberger-Doll Research, 36 Old Quarry Rd., Ridgefield, Connecticut 06877;

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