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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Surface-downhole electrical resistivity tomography applied to monitoring of CO2 storage at Ketzin, Germany
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Surface-downhole electrical resistivity tomography applied to monitoring of CO2 storage at Ketzin, Germany

机译:地表下电阻率层析成像技术在德国Ketzin的二氧化碳存储监测中的应用

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摘要

Surface-downhole electrical resistivity tomography (SD-ERT) surveys were repeatedly carried out to image CO2 injected at the pilot storage Ketzin, Germany. The experimental setup combines surface with downhole measurements by using a permanent electrode array that has been deployed in three wells. Two baseline experiments were performed during the site startup and three repeat experiments were performed during the first year of CO2 injection. By the time of the third repeat, approximately 13,500 tons of CO2 had been injected into the reservoir sandstones at about 650 m depth. Field data and inverted resistivity models showed a resistivity increase over time at the CO2 injector. The lateral extent of the related resistivity signature indicated a preferential CO2 migration toward the northwest. Using an experimental resistivity-saturation relationship, we mapped CO2 saturations by means of the resistivity index method. For the latest repeat, CO2 saturations show values of up to 70% near the injection well, which matches well with CO2 saturations determined from pulsed neutron-gamma logging. The presence of environmental noise, reservoir heterogeneities, and irregularities in the well completions are the main sources of uncertainty for the interpretations. The degradation of the permanently installed downhole components is monitored by means of frequently performed resistance checks. In consistency with the SD-ERT data, these resistance checks indicate a long-term resistivity increase near the CO2 injector. In conclusion, the investigations demonstrate the capability of surface-downhole electrical resistivity tomography to image geologically stored CO2 at the Ketzin site.
机译:重复进行了地下电阻率层析成像(SD-ERT)测量,以对在德国Ketzin的中试仓库注入的CO2进行成像。实验装置通过使用已部署在三个井中的永久性电极阵列,将地面测量与井下测量结合起来。在站点启动期间进行了两个基准实验,在二氧化碳注入的第一年进行了三个重复实验。到第三次重复时,已在大约650 m的深度将约13,500吨的CO2注入到储层砂岩中。现场数据和反演的电阻率模型显示,二氧化碳注入器的电阻率随时间增加。相关电阻率特征的横向范围表明CO2向西北方向优先迁移。使用实验电阻率-饱和度关系,我们通过电阻率指数法绘制了CO2饱和度图。对于最新的重复,在注入井附近,CO2饱和度显示高达70%的值,与脉冲中子伽马测井确定的CO2饱和度非常匹配。井眼完井中存在环境噪声,储层非均质性和不规则性是解释不确定性的主要来源。永久安装的井下组件的退化通过频繁执行的电阻检查进行监控。与SD-ERT数据一致,这些电阻检查表明在CO2注入器附近长期电阻率增加。总之,研究表明,井下电阻率层析成像技术能够对Ketzin站点上地质存储的CO2进行成像。

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