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

J. Rohmer, D. Seyedi
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引用次数: 77

Abstract

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 scenariobased 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.
深盐层CO2封存盖层破坏风险评价的耦合大尺度流体力学模型
这项工作提出了一种大规模流体力学模拟的数值策略,以评估二氧化碳注入过程中盖层地层的损害风险。所提出的方法是基于多相流体流动(TOUGH2)和流体力学计算代码(Code_Aster)之间的顺序耦合的发展,使我们能够在区域尺度上进行耦合的流体力学模拟。然后,可以根据耦合模拟的结果评估不同盖层破坏机制的可能性。为了考虑模型参数的不确定性对损伤可能性的影响,提出了一种基于情景的方法。以巴黎盆地多层地质体系为例,应用该方法对多格尔组深层含水层盖层破坏进行了分析。模拟是在区域尺度(100公里)上进行的,考虑到工业质量二氧化碳注入速率为10万吨/年。通过发达的序贯耦合对注入10年后的应力状态进行了评估。考虑了两种破坏机制,即拉伸破裂和原有裂缝的剪切滑移再激活。为了解决地层数据稀疏导致的较大不确定性,采用了一种基于场景的策略。它包括定义第一个参考建模场景,考虑每层流体力学特性的平均值。然后进行敏感性分析,表明初始应力状态和储层水力性质对盖层破坏趋势的重要性。在此基础上,定义了第二个表示为“关键”的场景,以便在最坏的配置中采用最具影响力的模型参数。对于所考虑的条件,这些故障标准都没有被激活。在现象学层面上,本研究指出风险管理的三个关键方面。最大超压在几年后迅速达到,注入引起的“超压”带横向延伸非常大(> 50 km),最关键的区域是盖层与储层界面的近区域(距离< 100 m)注入。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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