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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Feasibility of CO2 plume detection using 4D seismic: CO2CRC Otway Project case study - Part 2: Detectability analysis
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Feasibility of CO2 plume detection using 4D seismic: CO2CRC Otway Project case study - Part 2: Detectability analysis

机译:使用4D地震检测CO2羽流的可行性:CO2CRC Otway项目案例研究-第2部分:可检测性分析

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A key objective of stage 2 of the Cooperative Research Centre for Greenhouse Gas Technologies (CO2CRC) Otway Project is to explore the ability of the seismic reflection method to detect and monitor injection of a small amount of greenhouse gas into a saline formation. Development of a seismic monitoring program requires an understanding of expected time-lapse (TL) seismic signals. Hence, before such an injection experiment is undertaken, we assessed the feasibility of seismic monitoring in a modeling study. Considering realistic gas distributions inferred from reservoir simulations, we analyzed the influence of various factors (injection volume, time after injection, and realizations of the reservoir flow model) on the TL seismic signal. However, the applicability of seismic monitoring depends not only on the strength of the TL seismic signal but also on the noise level of the seismic data. Hence, to estimate the detectability of gas in the subsurface, we have developed a workflow that integrated actual data repeatability observed at the Otway test site into the seismic feasibility study. Although we observed differences between the considered scenarios, all of the scenarios indicated a high likelihood of successful plume detection with the observed noise level and surface 4D seismic acquisition geometry used in stage 1 of the CO2CRC Otway Project at the same site. However, a thin layer of gas spreading out from the edges of the main plume below the seal in all scenarios would be a challenge for surface seismic monitoring.
机译:温室气体技术合作研究中心(CO2CRC)奥特韦项目第二阶段的主要目标是探索地震反射法检测和监测向盐层中注入少量温室气体的能力。地震监测程序的开发需要了解预期的时差(TL)地震信号。因此,在进行这样的注入实验之前,我们在模型研究中评估了地震监测的可行性。考虑到从油藏模拟中得出的实际天然气分布,我们分析了各种因素(注入量,注入后的时间以及油藏流动模型的实现)对TL地震信号的影响。但是,地震监测的适用性不仅取决于TL地震信号的强度,还取决于地震数据的噪声水平。因此,为了估计地下气体的可探测性,我们开发了一个工作流程,将在奥特韦测试现场观察到的实际数据可重复性整合到地震可行性研究中。尽管我们观察到了所考虑的场景之间的差异,但所有场景都表明在同一地点的CO2CRC Otway项目第一阶段中使用的观测到的噪声水平和地面4D地震采集几何形状具有成功完成羽流检测的可能性。然而,在所有情况下,薄薄的气体层都从密封下方的主羽边缘扩散出来,这对于地表地震监测将是一个挑战。

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