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3-D Time-lapse Electrical Resistivity Monitoring of Injected CO2 in a Shallow Aquifer

机译:浅含水层中注射二氧化碳的三维延时电阻率监测

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Contamination of potable groundwater by leaking CO2 is a potential risk of carbon sequestration. With the help of a field experiment, we investigate if surface electrical resistivity tomography (ERT) can detect dissolved CO2 in a shallow aquifer. For this purpose, we injected CO2 at a depth of 5 and 10 m and monitored its migration using 320 surface electrodes on a 126 m × 20 m grid. A fully automated acquisition system continuously collected data and uploaded it into an online database. The large amount of data allows for time-series analysis for data quality and noise estimation. A baseline inversion reveals the geology at the site consisting of aeolian sands near the surface and glacial sands below 5 m depth. Time-lapse inversions clearly image the dissolved CO2 plume with decreased electrical resistivity values. We can follow the CO2 plume as it spreads and moves with the groundwater, and the spatial distribution of the plume agrees well with direct measurements of the groundwater resistivity. Future work will include improved time-series analyses and quantitative comparison with the groundwater resistivity measurements.
机译:通过泄漏CO 2污染饮用地下水是碳封存的潜在风险。借助现场实验,我们研究了表面电阻率断层摄影(ERT)是否可以检测浅含水层中的溶解二氧化碳。为此目的,我们在深度为5和10μm的深度中注入CO 2,并在126m×20m网格上使用320个表面电极监测其迁移。完全自动采集系统持续收集数据并将其上传到在线数据库中。大量数据允许数据质量和噪声估计的时间序列分析。基线反转揭示了由在5米以下的表面和冰川砂附近的天体砂的地质构成。延时反转显然将溶解的CO2羽流与电阻率值降低。我们可以随着地下水铺设和移动时,我们可以遵循二氧化碳羽流,羽流的空间分布良好地对地下水电阻率的直接测量很好。未来的工作将包括改进的时间序列分析和与地下水电阻率测量的定量比较。

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