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Optimal designs of time-lapse seismic surveys for monitoring CO2 leakage through fault zones

机译:延时地震勘探的最佳设计,用于监测通过断裂带的CO2泄漏

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摘要

Cost-effective time-lapse seismic surveys are crucial for long-term monitoring of geologic carbon sequestration. In this paper, we numerically model time-lapse seismic surveys for monitoring CO2 leakage through fault zones, and design optimal surveys for time-lapse seismic data acquisition using elastic-wave sensitivity analysis. Two stages of CO2 leakage through fault zones are simulated. In the early stage of leakage, when CO2 is confined in a relatively deep region, and our results show that the most desired location for receivers at the surface is at the hanging-wall side of the fault zone, of normal faults (with large dip angles) or reverse faults. The most sensitive places at the surface to the change of different elastic parameters (e.g. P- and S-wave velocity and density) are similar to one another, and are often not sensitive to the source location. In a late stage of leakage, in which CO2 migrates close to the surface, our modeling demonstrates that the best region at the surface for time-lapse seismic surveys is very sensitive to the source location and the elastic parameter to be monitored. For time-lapse vertical seismic profiling (VSP) surveys, our modeling suggests that it is important to account for the effect of free-surface reflections, especially for large offset VSP surveys.
机译:具有成本效益的延时地震勘测对于长期监测碳固存至关重要。在本文中,我们对延时地震勘测进行了数值建模,以监测通过断层带的CO2泄漏,并使用弹性波敏感性分析设计了用于延时地震数据采集的最佳勘测。模拟了通过断层带泄漏二氧化碳的两个阶段。在泄漏的早期阶段,当二氧化碳被限制在一个相对较深的区域时,我们的结果表明,接收器最期望的位置是在正常断层(倾角较大)的断层的悬挂壁侧。角度)或反向故障。表面上对不同弹性参数(例如P波和S波的速度和密度)的变化最敏感的位置彼此相似,并且通常对源位置不敏感。在泄漏的后期,CO2迁移到地表附近,我们的模型表明,用于时移地震勘探的地表最佳区域对震源位置和要监测的弹性参数非常敏感。对于延时垂直地震剖面(VSP)勘测,我们的模型表明,考虑自由表面反射的影响非常重要,尤其是对于大偏移量VSP勘测而言。

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