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Impact of a CO2 leakage on groundwater quality. Influence of regional flow using reactive transport models.

机译:二氧化碳泄漏对地下水质量的影响。使用反应性运输模型的区域流量的影响。

摘要

Carbon Capture and Storage in deep and saline aquifers is one of the most hopeful technologies to reduce CO2 emissions into the atmosphere. However, CO2 leakages into shallow freshwater aquifers are a potential risk and potential impacts on groundwater have to be studied. A better understanding on how it could affect groundwater quality, aquifer minerals and trace elements is necessary to characterize a future storage site. Moreover, monitoring and remediation solutions have to be evaluated before storage operations. As part of the ANR project CIPRES, we present here reactive transport works. In a 3D model using ToughReact2, we perform different CO2 leakage scenarios in a confined aquifer, considering both brines and carbon dioxide gas. Our modeling works are based on the Albian aquifer, a strategic water resource for the Paris basin. This layer is the main aquifer overlying the Dogger deep saline aquifer. We consider one groundwater and rocks chemistry of the Albian aquifer composed by the Albian green sand (Quartz, Calcite, Glauconite , Kaolinite) at 700 m deep. The geochemical model was elaborated from experimental data performed in previous study (Humez, 2012). The aquifer consists in a mesh, divided roughly in 20000 cells making a 60 m thick and a 500 m large layer. Furthermore, cells are subdivided near the leakage point to consider local phenomena (secondary precipitation, kinetics, sorption/desorption...). We highlight the importance of surface complexation on trace element transport (As, Zn and Ni). Moreover, we distinguish different geochemical behavior (CO2 plume shape, secondary precipitation of siderite or chalcedony, desorption...) according to different horizontal flow rate influenced directly by the hydrodynamics (regional gradient). Understanding how geochemical reactions and regional flows influence water chemistry, allows to ascertain measurement monitoring and verification plan and remediation works in case of leak considering a given location.
机译:在深层和盐水层中进行碳捕集与封存是减少二氧化碳向大气中排放的最有希望的技术之一。但是,CO2泄漏到浅层淡水含水层中是潜在的风险,必须研究对地下水的潜在影响。必须对它如何影响地下水质量,含水层矿物质和微量元素有一个更好的了解,以表征未来的存储地点。此外,在存储操作之前必须评估监视和补救解决方案。作为ANR项目CIPRES的一部分,我们在此介绍反应性运输工程。在使用ToughReact2的3D模型中,考虑到盐水和二氧化碳气体,我们在密闭含水层中执行了不同的CO2泄漏情景。我们的建模工作基于巴黎盆地的战略水资源Albian含水层。该层是覆盖在Dogger深层盐水层上的主要含水层。我们考虑了深度为700 m的由Albian绿沙(石英,方解石,Glauconite,Kaolinite)组成的Albian含水层的一种地下水和岩石化学。地球化学模型是根据先前研究(Humez,2012年)中进行的实验数据精心制定的。含水层由一个网眼组成,大致分为20000个单元,形成60 m厚和500 m大层。此外,在泄漏点附近将细胞细分,以考虑局部现象(二次沉淀,动力学,吸附/解吸...)。我们强调了表面络合对痕量元素转运(砷,锌和镍)的重要性。此外,根据受流体动力学直接影响的不同水平流速(区域梯度),我们区分了不同的地球化学行为(二氧化碳羽状,菱铁矿或玉髓的二次沉淀,解吸等)。了解地球化学反应和区域流量如何影响水化学,可以确定测量监控和验证计划,并在考虑给定位置的泄漏情况下进行补救工作。

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