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Uncertainty Quantification of CO2 Plume Migration Using Static Connectivity of Geologic Features

机译:使用地质特征静态连接的CO2羽流迁移的不确定性量化

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During the operation of a geological carbon storage project, a critical question is whether injected CO2 remains within the permitted zone. However, because a large suite of subsurface models are possible given very sparse static data, simulating flow in the entire suite to quantify the uncertainty in CO2 plume migration is impractical. We propose a fast alternative that scans the suite of geologic models and groups them on the basis of static connectivity. Grouping is achieved simply by measuring the shape dissimilarity of permeable zones in the prior models using path skeletons. By selecting a specific group of models that reflect the performance observed in the field, it is possible to quantify the uncertainty in CO2 plume migration. Our approach is compared against results obtained by flow simulation and subsequent model classification using principal component analysis (PCA) in characteristics of connectivity.
机译:在地质碳储存项目的运行期间,一个关键问题是注射二氧化碳是否仍然在允许区内。但是,由于提供了大量的地下模型,因为提供了非常稀疏的静态数据,因此在整个套件中模拟流量以量化CO2羽流中的不确定性是不切实际的。我们提出了一种快速替代方案,扫描了地质模型的套件并根据静态连接群体组。仅通过使用路径骨架测量先前模型中渗透区的形状不相似来实现分组。通过选择反映在该字段中观察到的性能的特定模型组,可以量化CO2羽流迁移中的不确定性。将我们的方法与通过在连通性特性中使用主成分分析(PCA)的流动模拟和随后的模型分类而获得的方法。

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