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首页> 外文期刊>International Journal of Greenhouse Gas Control >Detection and characterization of CO2 leakage by multi-well pulse testing and diffusivity tomography maps
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Detection and characterization of CO2 leakage by multi-well pulse testing and diffusivity tomography maps

机译:通过多井脉冲测试和扩散层析成像图检测和表征CO2泄漏

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Pressure pulse testing, a type of interference well testing, has shown promising applications in subsurface carbon dioxide (CO2) leakage detection and monitoring. In pressure pulse testing, a pressure signal generated by periods of injection and shut-in (from a pulsing well) propagates deep into the formation, and the corresponding response is recorded at the observation well(s). The shape of the signal alters as it travels between the pulsing well and the observation well. Analysis of this characteristic change is the basis for measurement of formation properties such as the total hydraulic diffusivity coefficient. If the test is repeated over time, one can detect and monitor temporal changes in the hydraulic diffusivity coefficient. In this paper, we used a modified analytical solution in the frequency domain to analyze the pressure pulse test data and to characterize the location and geometry of the CO2 leak. Using this technique, we first transferred the periodic pressure response to the frequency domain using the Fast Fourier Transform. Then we used a modified analytical solution to calculate the diffusivity coefficient excluding the injection rate data. The derived diffusivity coefficient for each pulse test was assigned to the midpoint between the pulsing well and the observation well. Finally, a stochastic simulation approach was used to generate a large-scale diffusivity tomography map for the target formation. When this concept was applied to a network of monitoring wells, the derived diffusivity tomography map successfully located and visualized the extent of CO2 leakage. The contour lines of the diffusivity tomography map reasonably revealed the geometry of CO2 leakage (point-source vs. line-source leakage) and when superposed on the CO2 saturation profile, showed very good agreement. Analysis of the results indicated that even a small amount of CO2 leakage in the investigation zone can have a measurable effect on the calculated diffusivity coefficient. This finding can be of great importance when early leak detection is of interest. Such information can be applied to monitor plume evolution and design a remediation process. Our study shows that the pressure pulse test analysis has the capability to monitor large areas inside the formation and to detect and characterize possible CO2 leaks with reasonable accuracy. (C) 2016 Elsevier Ltd. All rights reserved.
机译:压力脉冲测试是一种干扰井测试,已显示出在地下二氧化碳(CO2)泄漏检测和监测中的有希望的应用。在压力脉冲测试中,由注入和关闭阶段(来自脉冲井)产生的压力信号会深入地层,并在观测井处记录相应的响应。当信号在脉冲井和观测井之间传播时,信号的形状会发生变化。分析此特性变化是测量地层特性(例如总水力扩散系数)的基础。如果随时间重复测试,则可以检测并监视水力扩散系数的时间变化。在本文中,我们在频域中使用了改进的分析解决方案来分析压力脉冲测试数据,并表征CO2泄漏的位置和几何形状。使用这种技术,我们首先使用快速傅立叶变换将周期性压力响应传递到频域。然后,我们使用改进的解析解来计算不包括注入速率数据的扩散系数。将每个脉冲测试得出的扩散系数分配给脉冲井和观察井之间的中点。最后,使用随机模拟方法来生成用于目标形成的大规模扩散层析成像图。当将此概念应用于监控井网络时,得出的扩散层析成像图成功定位并可视化了CO2泄漏的程度。扩散层析成像图的轮廓线合理地揭示了CO2泄漏的几何形状(点源泄漏与线源泄漏),并且当叠加在CO2饱和剖面上时,显示出很好的一致性。对结果的分析表明,即使在研究区中发生少量的CO2泄漏,也可以对计算出的扩散系数产生可测量的影响。当对早期泄漏检测感兴趣时,此发现可能非常重要。此类信息可用于监视羽流演变并设计补救过程。我们的研究表明,压力脉冲测试分析能够监视地层内部的大面积区域,并能够以合理的精度检测和表征可能的CO2泄漏。 (C)2016 Elsevier Ltd.保留所有权利。

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