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Inferring migration of CO_2 plume using injection data and a probabilistic history matching approach

机译:使用注射数据和概率历史匹配方法推断CO_2羽流的迁移

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Large-scale implementation of geologic carbon storage (GCS) will require reliable techniques for monitoring the movement of the CO_2 plume in the subsurface. The movement of CO_2 plumes beyond the region permitted for storage will be of particular interest both to regulators and to operators. However, the cost of many monitoring technologies, such as time-lapse seismic, limits their application. Given that injection data (pressures, rates) from wells are readily available and inexpensive, we examine whether they can be used as a viable alternative for monitoring and predicting plume migration. In this paper, we have implemented a probabilistic history matching approach to creating models of the aquifer for predicting the movement of the CO_2 plume. The geologic property of interest for example hydraulic conductivity is updated conditioned to geological information and injection pressures. The resultant aquifer model which is geologically consistent can be used to reliably predict the movement of the CO_2 plume in the subsurface. We tailor the method to CO_2 sequestration by considering only injection data in the matching process. We also introduce a two-step approach to stochastically simulate high-permeability features such as oriented sets of natural fractures that occupy only a small fraction of the storage formation. We illustrate the approach by applying it to data from the In Salah Gas project. The final history-matched models contain high permeability features consistent with the field observation of rapid arrival of injected CO_2 at a suspended well and with surface deformation data obtained by remote sensing. We conclude that the approach can provide a probabilistic assessment of plume migration at the field scale.
机译:地质碳储存(GCS)的大规模实施将需要可靠的技术来监测地下CO_2羽流的运动。 CO_2羽毛超出允许储存的区域的运动将特别感兴趣的是监管机构和运营商。然而,许多监测技术的成本,例如延时地震,限制了它们的应用。鉴于来自井的注射数据(压力,速率)易于获得和廉价,我们检查它们是否可以用作监控和预测羽流迁移的可行替代方案。在本文中,我们已经实现了一种概率历史匹配方法,用于创建含水层的模型,以预测CO_2羽流的运动。利用例如液压导电性的地质特性被更新为地质信息和注射压力。在地质上一致的所得含水层模型可用于可靠地预测地下CO_2羽流的运动。我们通过考虑匹配过程中的注射数据来定制对CO_2 SeateStation的方法。我们还介绍了一项两步的方法来随机模拟高渗透功能,例如取向的自然骨折组,占据储存形成的一小部分。我们通过将其应用于Salah天然气项目中的数据来说明方法。最终历史匹配的模型包含高磁导率特征,该功能一致,与悬浮井的注射的CO_2快速到达的现场观察,以及通过遥感获得的表面变形数据。我们得出结论,该方法可以在现场规模处提供对羽流迁移的概率评估。

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