对水力压裂的连续地震监测揭示了复杂的地下动态:利用分布式声学传感和地表轨道振动器进行观测

GEOPHYSICS Pub Date : 2024-07-03 DOI:10.1190/geo2023-0785.1
Julia Correa, S. Glubokovskikh, Avinash Nayak, Linqing Luo, T. Wood, Xiaoyu Zhu, Jonathan Ajo-Franklin, B. Freifeld
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引用次数: 0

摘要

了解水力压裂对改善非常规储层的激励和提高液体产量至关重要。本研究提出了一种新型地震监测技术,利用分布式声学传感(DAS)和表面轨道振动器(SOV),以高时间间隔捕捉压裂地震响应和机械特性。我们分析了在奥斯汀白垩纪/鹰滩页岩实验室处理非常规储层的前九天中每小时采集的连续延时垂直地震剖面(VSP)数据。VSP 数据包含从激活的裂缝中散射出的清晰地震信号。SOV/DAS 数据显示的裂缝反射率时空变化与低频 DAS 数据推断的裂缝位置观测结果非常吻合。这些结果捕捉到了裂缝的打开和闭合过程,并突出显示了由于与原有裂缝系统的水力连接而可能导致的裂缝前期激活。因此,对所提供的数据集进行分析,不仅为了解非常规资源,而且为了解增强地热系统中的断裂起始和后续演化提供了一个独特的机会。
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Continuous seismic monitoring of hydraulic fracturing reveals complex subsurface dynamics: observations using distributed acoustic sensing and surface orbital vibrators
Understanding hydraulic fracturing is crucial to improving the stimulation of unconventional reservoirs and increasing fluid production. This study proposes a novel seismic monitoring technology, using distributed acoustic sensing (DAS) and surface orbital vibrators (SOV), to capture fracture seismic response and mechanical properties at high temporal intervals. We analyze continuous time-lapse Vertical Seismic Profiling (VSP) data acquired every hour during the first nine days of treatment of an unconventional reservoir in the Austin Chalk/Eagle Ford Shale Laboratory. The VSP data contains clear seismic signals scattered from the activated fractures. The spatiotemporal changes of the fracture reflectivity revealed by the SOV/DAS data correlate well with the observations of fracture locations inferred from low-frequency DAS data. These results capture the fracture opening and closure processes, as well as highlighting potential pre-stage activations of the fractures due to hydraulic connectivity with pre-existing fracture systems. Therefore, analysis of the presented data set provides a unique opportunity to understand fracture initiation and subsequent evolution, not only in the context of unconventional resources, but also in enhanced geothermal systems.
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