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首页> 外文期刊>SPE Reservoir Evaluation & Engineering >Monitoring Sagd Steam Injection Using Microseismicity And Tiltmeters
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Monitoring Sagd Steam Injection Using Microseismicity And Tiltmeters

机译:使用微地震仪和倾角仪监测凹陷蒸汽注入

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A combination of microseismic and surface-deformation monitoring with an array of tiltmeters was used to monitor the warm-up phase of a steam-assisted-gravity-drainage (SAGD) well pair. A sequence of microseismic events was recorded with signal characteristics that suggested deformation associated with thermal expansion of the wellbore, in addition to events apparently associated with induced fracturing in the reservoir. Integration of the microseismic data with volumetric strain, inverted from the measured surface deformation, indicates a discrete deforming region near the toe of the well. The volumetric strain also shows another region near the heel of the well, although the area is too far from the microseismic observation well for any associated microseismicity to be recorded. The central portion of the well pair did not have significant deformation, indicating poor steam conformance during this warm-up phase. A comparison of the temporal response of the microseismic deformation with the surface uplift suggests a lag between periods of accelerated seismic deformation followed by an associated period of accelerated uplift a few days later. This timing suggests the creation of a fracture network and related seismic deformation, which then fills with steam and starts to expand over a period of a few days. In a related paper (Du et al. 2007), stress changes associated with the volumetric strain are used to examine potential geomechanical failure zones that match the observed locations of microseisms. Together, the volumetric strain, computed stress changes, and failure zones could be used to calibrate a geomechanically linked reservoir simulator.
机译:微地震和表面变形监测与倾斜仪阵列的组合被用来监测蒸汽辅助重力排水(SAGD)井对的预热阶段。记录了一系列微地震事件,其信号特征表明与井眼热膨胀有关的变形,以及与储层中诱发压裂有关的事件。从测得的表面变形开始,将微地震数据与体积应变积分在一起,表明井底附近存在离散的变形区域。体积应变还显示了靠近井底的另一个区域,尽管该区域距离微震观测井太远,以至于无法记录任何相关的微震。井对的中心部分没有明显的变形,表明在此预热阶段中蒸汽的顺应性较差。将微地震变形的时间响应与地表隆起进行比较,表明加速地震变形的时间段之间存在滞后,几天后是相关的加速隆起时间。这个时机表明裂缝网络的产生和相关的地震变形,然后充满蒸汽,并在几天内开始膨胀。在一篇相关论文中(Du等人,2007年),与体积应变相关的应力变化被用于检查与观察到的微震位置相匹配的潜在地质力学破坏区域。总之,体积应变,计算出的应力变化和破坏区域可用于校准与地质力学相关的油藏模拟器。

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