Carbon Storage Leak Detection via Seismic FWI and RTM: Different Surveys Analysis

S. Amani
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Abstract

Marine seismic data processing is investigated to monitor possible leakages from the geological Carbon storage. Due to the high importance of storage permanence, a precise leakage monitoring strategy is crucial. Advanced seismic monitoring solutions should be used for this goal. The proficiency of these solutions for monitoring a Carbon storage leakage can be affected by shallower layers due to their structures, seismic wave attenuation, and leak size. Knowing the difficulty of this problem, we investigate the two popular seismic monitoring methods on Seismic data for monitoring Carbon leaks in different scenarios: Full Waveform Inversion (FWI) and Reverse-Time Migration (RTM). Finding the best survey strategy for monitoring carbon leaks is also significant. So, the results of different survey strategies, including vertical seismic profiling (VSP), cross-well, and surface, are compared to demonstrate the pros and cons of each strategy. The synthetic marine seismic data is calculated for different models, including Carbon storage and its leak. We used a set of realistic physical values for sedimentary rocks that are common for such a media. An elastic finite-difference time-domain scheme is used for the simulations. We applied FWI and RTM methods for monitoring Carbon Leaks using the seismic data. The FWI results demonstrate a good detection of the leakage areas that were clearer in the VSP survey than the others. Also, the performance of the FWI method was checked for different sizes of Carbon leaks. The results show the high capability of FWI as a solution to this problem. Besides, the RTM results show the high potential of the z-component of seismic data outperformed in showing the borders of the CO2 leakage. This point is more visible in the VSP results than in others. On the other side, the x-component of seismic data in the RTM results shows that it can demonstrate lateral reflectors better.
基于地震FWI和RTM的储碳泄漏检测:不同测量方法的分析
研究了海洋地震资料处理,以监测地质碳储存可能发生的泄漏。由于存储持久性的高度重要性,精确的泄漏监测策略是至关重要的。先进的地震监测解决方案应该用于实现这一目标。由于其结构、地震波衰减和泄漏大小,这些解决方案监测碳储存泄漏的熟练程度可能受到较浅层的影响。认识到这一问题的难度,我们研究了两种流行的地震监测方法,用于监测不同场景下的碳泄漏:全波形反演(FWI)和逆时偏移(RTM)。找到监测碳泄漏的最佳调查策略也很重要。因此,不同的勘探策略(包括垂直地震剖面(VSP)、井间地震剖面和地面地震剖面)的结果进行了比较,以展示每种策略的优缺点。对不同模型下的海洋合成地震数据进行了碳储量和碳泄漏计算。我们使用了一组沉积岩的真实物理值,这是这种介质中常见的。模拟采用弹性时域有限差分格式。利用地震资料,采用FWI和RTM方法监测碳泄漏。FWI检测结果表明,VSP测量能够很好地检测泄漏区域,比其他方法更清晰。同时,测试了FWI方法在不同尺寸碳泄漏情况下的性能。结果表明,FWI的高性能解决了这一问题。此外,RTM结果表明,地震数据的z分量在显示CO2泄漏边界方面具有较高的潜力。这一点在VSP结果中比在其他结果中更明显。另一方面,RTM结果中地震资料的x分量可以更好地显示侧向反射。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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