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3D geomechanical modeling for CO2 geological storage in faulted formations. A case study in an offshore northern Adriatic reservoir, Italy

机译:断层构造中二氧化碳地质封存的3D地质力学建模。意大利北部亚得里亚海近海水库的案例研究

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摘要

One of the six CO2 carbon capture and storage (CCS) demonstration projects recently selected within the European Energy Programme for Recovery (EEPR) is located in Italy. In the framework of the feasibility study, the selection of a geological formation suitable to store the required 1 Mt/yr of CO2 over 10 years and the safety of the CO2 disposal are two major issues. In the present modeling study, we investigate the role played by geomechanics in assessing the maximum CO2 amount that can be sequestered into a 2000 m deep multi-compartment reservoir seated in the off-shore northern Adriatic sedimentary basin. We use a three-dimensional finite element-interface element geomechanical model to simulate the possible mechanical failure in both the injected formation and caprock, the fault reactivation, and the ground surface displacement. The faulted geological structure is reproduced based on detailed seismic surveys, with petrophysical/geomechanical properties based on the several well-logs available from several oil/gas explorations in the area. The pore pressure distribution due to two injection wells is provided by a fluid-dynamic simulator and a sensitivity analysis is carried out to investigate the role of the major uncertainties in the geomechanical setting. The modeling results suggest that a safe and permanent containment may be secured over a few years only. Afterwards, mechanical failure by shear stress is likely to be experienced by a significant portion of reservoir's injected compartments. Shear failure and fault reactivation can occur much before attaining the hydraulic fracturing pressure, hence represent two major issues in assessing the maximum allowable CO2 injection overpressure
机译:最近在欧洲能源回收计划(EEPR)中选定的六个CO2碳捕集与封存(CCS)示范项目之一位于意大利。在可行性研究的框架内,选择适合于在10年内存储所需的1 Mt / yr的CO2的地质构造以及CO2处置的安全性是两个主要问题。在目前的模型研究中,我们调查了地质力学在评估可封存到位于北部亚得里亚海北部沉积盆地的2000 m深多隔层储层中的最大CO2量中所发挥的作用。我们使用三维有限元-界面元地质力学模型来模拟注入地层和盖层中可能发生的机械破坏,断层再活化和地表位移。断层地质结构是根据详细的地震勘测结果复制的,其岩石物理/地质力学特性是根据该地区几处油气勘探获得的几口测井数据得出的。流体动力学模拟器提供了由于两个注入井而引起的孔隙压力分布,并进行了敏感性分析以研究主要不确定性在地质力学环境中的作用。建模结果表明,只能在几年内确保安全和永久的围堵。此后,储层注入隔间的很大一部分很可能会经历剪切应力引起的机械故障。在达到水力压裂压力之前,可能会发生剪切破坏和断层再活化,因此在评估最大允许CO2注入超压时代表了两个主要问题

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