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Coupled Large Scale Hydromechanical Modelling for Caprock Failure Risk Assessment of CO2 Storage in Deep Saline Aquifers

机译:深盐水层二氧化碳封存盖层破坏风险评估的大型水力耦合模型

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Coupled Large Scale Hydromechanical Modelling for Caprock Failure Risk Assessment of CO2 Storage in Deep Saline Aquifers - This work presents a numerical strategy of large scale hydromechanical simulations to assess the risk of damage in caprock formations during a CO2 injection process. The proposed methodology is based on the development of a sequential coupling between a multiphase fluid flow (TOUGH2) and a hydromechanical calculation code (Code_Aster) that enables us to perform coupled hydromechanical simulation at a regional scale. The likelihood of different caprock damage mechanisms can then be evaluated based on the results of the coupled simulations. A scenario based approach is proposed to take into account the effect of the uncertainty of model parameters on damage likelihood. The developed methodology is applied for the caprock failure analysis of deep aquifer of the Dogger formation in the context of the Paris basin multilayered geological system as a demonstration example. The simulation is carried out at a regional scale (100 km) considering an industrial mass injection rate of CO2 of 10 Mt/y. The assessment of the stress state after 10 years of injection is conducted through the developed sequential coupling. Two failure mechanisms have been taken into account, namely the tensile fracturing and the shear slip reactivation of pre-existing fractures. To deal with the large uncertainties due to sparse data on the layer formations, a scenario-based strategy is undertaken. It consists in defining a first reference modelling scenario considering the mean values of the hydromechanical properties for each layer. A sensitivity analysis is then carried out and shows the importance of both the initial stress state and the reservoir hydraulic properties on the caprock failure tendency. On this basis, a second scenario denoted "critical" is defined so that the most influential model parameters are taken in their worst configuration. None of these failure criteria is activated for the considered conditions. At a phenomenological level, this study points out three key aspects for risk management. The maximum overpressure is reached rapidly after a couple of years, the lateral extension of the "overpressurized" zone induced by the injection is very large (>50 km) and the most critical zone is the injection near zone (distance <100 m) at the interface between the caprock and the reservoir layer.
机译:耦合深部盐水力学模型用于深层盐水层中CO2封存的盖层破坏风险评估-这项工作提出了一种大型水力学模拟的数值策略,用于评估在注CO2过程中盖层形成中受损的风险。所提出的方法基于多相流体流(TOUGH2)与流体力学计算代码(Code_Aster)之间的顺序耦合的开发,该序列耦合使我们能够在区域范围内执行耦合流体力学模拟。然后可以基于耦合模拟的结果来评估不同盖层破坏机制的可能性。提出了一种基于场景的方法,以考虑模型参数的不确定性对损坏可能性的影响。以巴黎盆地多层地质系统为背景,将开发的方法应用于道格格地层深层含水层的盖层破坏分析。考虑到10 Mt / y的CO2工业注入量,该模拟是在区域规模(100 km)上进行的。通过开发的顺序耦合对注射10年后的应力状态进行评估。已经考虑了两种破坏机制,即拉伸裂缝和原有裂缝的剪切滑移再活化。为了应对由于层地层数据稀疏而造成的巨大不确定性,我们采取了一种基于场景的策略。它包括定义第一个参考建模方案,其中考虑了每一层的流体力学特性的平均值。然后进行了敏感性分析,并显示了初始应力状态和储层水力特性对盖层破坏趋势的重要性。在此基础上,定义了表示为“关键”的第二种情况,以使最有影响力的模型参数采用最差的配置。对于所考虑的条件,这些失败标准均未激活。在现象学层面,本研究指出了风险管理的三个关键方面。几年后迅速达到最大超压,注入引起的“超压”区域的横向扩展非常大(> 50 km),最关键的区域是注入附近的区域(距离<100 m)盖层和储层之间的界面。

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