首页> 外文期刊>International Journal of Greenhouse Gas Control >High-resolution characterization of a CO2 plume using crosswell seismic tomography: Cranfield, MS, USA. (Special Section: Midproject assessment of the SECARB early test at Cranfield, Mississippi.)
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High-resolution characterization of a CO2 plume using crosswell seismic tomography: Cranfield, MS, USA. (Special Section: Midproject assessment of the SECARB early test at Cranfield, Mississippi.)

机译:使用井间地震层析成像对CO 2 羽的高分辨率表征:美国MS,Cranfield。 (特别部分:密西西比州克兰菲尔德市SECARB早期测试的项目中期评估。)

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摘要

We present the results of a high-resolution time-lapse crosswell seismic survey carried out at a large-scale CO2 injection pilot located in Cranfield, MS, USA. This dataset, spanning an injector and two monitoring wells, provided a detailed view of the boundaries and internal structure of the injection unit, the Tuscaloosa D/E sand. Time-lapse tomographic processing of one well pair revealed the signature of the injected plume, two zones of decreased P-wave velocity which spatially correspond to higher permeability sections of the reservoir unit. We then used White's model for patchy saturation, combined with secondary information from core and well-log measurements, to convert the imaged changes in P-wave velocity into estimates of supercritical (sc) CO2 saturation in the interwell region. Our estimate is relatively consistent with existing lithologic and core data as well as independent measurements of scCO2 saturation derived from pulsed neutron logging. While effective in mapping the zone of CO2 invasion in the interwell region, several sources of uncertainty still exist in quantifying saturation using crosswell seismic methods, including (but not limited to) the degree of mesoscale mixing or "patchiness" at scales below a seismic wavelength.
机译:我们介绍了位于美国密西西比州克兰菲尔德的大规模CO 2 注入试点进行的高分辨率时移井间地震勘探的结果。该数据集涵盖一个注入器和两个监测井,提供了注入单元塔斯卡卢萨D / E砂的边界和内部结构的详细视图。一口井对的延时层析成像处理显示出注入的羽流的特征,即P波速度降低的两个区域,在空间上对应于储层单元的较高渗透率部分。然后,我们使用White的斑块饱和度模型,结合岩心和测井测得的次要信息,将成像的P波速度变化转换为超临界(sc)CO 2 饱和度的估计值。井间区域。我们的估计与现有的岩性和岩心数据以及脉冲中子测井得出的scCO 2 饱和度的独立测量值相对一致。尽管可以有效地绘制井间区域CO 2 侵入带的图,但在使用井间地震法定量饱和度时,仍然存在一些不确定性来源,包括(但不限于)中尺度混合程度或“低于地震波长的尺度”。

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