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首页> 外文期刊>Geophysical Prospecting >The first post-injection seismic monitor survey at the Ketzin pilot CO2 storage site: results from time-lapse analysis
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The first post-injection seismic monitor survey at the Ketzin pilot CO2 storage site: results from time-lapse analysis

机译:Ketzin中试二氧化碳封存地点的首次注入后地震监测器调查:时移分析的结果

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摘要

The injection of CO2 at the Ketzin pilot CO2 storage site started in June 2008 and ended in August 2013. During the 62 months of injection, a total amount of about 67 kt of CO2 was injected into a saline aquifer. A third repeat three-dimensional seismic survey, serving as the first post-injection survey, was acquired in 2015, aiming to investigate the recent movement of the injected CO2. Consistent with the previous two time-lapse surveys, a predominantly west-northwest migration of the gaseous CO2 plume in the up-dip direction within the reservoir is inferred in this first post-injection survey. No systematic anomalies are detected through the reservoir overburden. The extent of the CO2 plume west of the injection site is almost identical to that found in the 2012 second repeat survey (after injection of 61 kt); however, there is a significant decrease in its size east of the injection site. Assessment of the CO2 plume distribution suggests that the decrease in the size of the anomaly may be due to multiple factors, such as limited vertical resolution, CO2 dissolution, and CO2 migration into thin layers, in addition to the effects of ambient noise. Four-dimensional seismic modelling based on dynamic flow simulations indicates that a dynamic balance between the newly injected CO2 after the second repeat survey and the CO2 migrating into thin layers and being dissolved was reached by the time of the first post-injection survey. In view of the significant uncertainties in CO2 mass estimation, both patchy and non-patchy saturation models for the Ketzin site were taken into consideration.
机译:在Ketzin中试二氧化碳存储地点开始注入二氧化碳,始于2008年6月,至2013年8月结束。在注入的62个月中,总共向盐水层注入了约67 kt的二氧化碳。 2015年进行了第三次重复三维地震勘测,作为第一次注入后调查,目的是调查注入的CO2的最新运动。与之前的两次延时调查一致,在第一次注入后调查中推断出气态CO 2羽流在储层内向上倾斜方向上的西北向主要迁移。通过储层覆盖层未检测到系统异常。注入点以西的二氧化碳羽流范围几乎与2012年第二次重复调查(注入61 kt后)中发现的程度相同;但是,在注射部位以东的尺寸明显减小。对CO2羽状流分布的评估表明,异常的大小减小可能是由于多种因素引起的,例如,垂直分辨率受限,CO2溶解和CO2迁移到薄层中,此外还受到环境噪声的影响。基于动态流模拟的四维地震模型表明,在第二次重复测量之后,新注入的CO2与迁移到薄层中并溶解的CO2之间达到了动态平衡。鉴于CO2质量估算的重大不确定性,考虑了Ketzin站点的斑块饱和度模型和非斑块饱和度模型。

著录项

  • 来源
    《Geophysical Prospecting》 |2018年第1期|62-84|共23页
  • 作者单位

    Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden;

    GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany|Sintef Petr Res, SP Andersens Vei 15 B, NO-7031 Trondheim, Norway;

    Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden;

    Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden;

    GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

    GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

    GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

    GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

    Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden;

    Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden|Jilin Univ, Xi Min Zhu St 938, Changchun, Jilin, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Seismic processing; Reservoir monitoring; 4D; Time lapse; Uncertainties;

    机译:地震处理;储层监测;4D;时间流逝;不确定性;

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