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Characterization and Quantification of the CO2 Sequestration Potential of a Carbonate Aquifer in Falaha Syncline, Onshore Abu Dhabi

机译:Falaha Syncline中碳酸盐含水层CO2螯合电位的表征及定量,陆上阿布扎比

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The capacity for the storage of carbon dioxide in saline aquifers remains enormous. Of all geological storage media, it provides the best storage capacity. In this study, the potential of the Shuaiba Formation, in the Falaha syncline, for geologic sequestration is assessed. A regional geo-model was built using seismic and well data (logs, cores) from the Falaha Syncline and nearby fields. The model was built to honor the heterogeneity and sequence stratigraphy of the Shuaiba carbonate platform using a five-order hierarchical conceptual model of the Shuaiba formation that merged sequence architecture and reservoir architecture together. This was achieved by honoring lithofacies, facies association packages and rock types in their corresponding depositional settings in the sequence framework. Dynamic simulations were then conducted on an upscaled geological model using a compositional reservoir simulator to determine its storage and flow capacity, plume migration pathways and to understand the physics of the fluid flow in the aquifer. Simulations are made to be conservative thus accounting for structural/stratigraphic, solubility (dissolution in resident brine) and residual trapping without accounting for the slower mineral trapping process. Detailed sensitivity studies were conducted during the simulations to understand the effect of well parameters, rock and fluid properties amongst others on the storage capacity in the aquifer. Simulation results indicate that significant volumes could be stored in the aquifer and could take a significant amount of time before the injected gas reaches the surrounding hydrocarbon producing fields. This study provides the first full field approach to characterize and to quantify the suitability of the identified aquifer for long term storage of carbon dioxide in the subsurface of UAE.
机译:盐水含水层中二氧化碳储存的能力仍然是巨大的。在所有地质存储介质中,它提供了最佳的存储容量。在这项研究中,评估了佛拉哈拉蹄素的水洗形成的潜力,用于地质封存。使用来自Falaha Syncline和附近的领域的地震和井数据(日志,核心)建立了区域地理模型。该模型建立了讲述舒瓦碳酸盐平台的异质性和序列地层,采用舒瓦巴地层的五阶分层概念模型合并了序列架构和储层架构在一起。这是通过在序列框架中的相应沉积设置中的岩石缩放,相结合包和岩石类型来实现的。然后使用组合储层模拟器在升高的地质模型上进行动态模拟,以确定其储存和流量,羽流迁移途径,并了解含水层中的流体流动的物理。因此,仿真是保守的,从而占结构/地层,溶解性(静静脉溶解)和残留捕获,而无需占较慢的矿物捕获过程。在模拟期间进行了详细的敏感性研究,以了解井中参数,岩石和液体特性在含水层中的储存能力中的效果。仿真结果表明,显着的体积可以储存在含水层中,并且可以在注射的气体到达周围的碳氢化合物生产领域之前花费大量时间。本研究提供了第一种全场方法来表征,并量化鉴定的含水层在阿联酋地下储存二氧化碳的长期储存的适用性。

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