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Integrity analysis of CO2 storage sites concerning geochemical-geomechanical interactions in saline aquifers

机译:与盐水层中地球化学-地球力学相互作用有关的CO2封存位置的完整性分析

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A systematic and careful analysis of changes in the magnitude of geomechanical parameters is essential to mitigate the risk of leakage from CO2 storage sites. However, depending on rocks and storage sites, these changes might be different due to chemical reactions taking place, especially when it comes to saline aquifers. There have only been few studies carried out in the past to evaluate the maximum sustained pressure of rocks being exposed to these chemical interactions. However, more studies are still required to evaluate the strength of the storage medium or seals when different kinds of rocks and fluids (fresh water or brine) are included in the hostile environment of a storage site. In this paper, attempts were made to evaluate changes in the variation of geomechanical parameters of the Berea sandstone during and after the injection of supercritical CO2 in a short period of time. The results obtained indicated that the presence of brine in the pore space during injection enhances the severity of geochemical reactions, causing reductions in the magnitudes of elastic parameters including shear modulus. Having a good look into the SEM images of the sample before and after exposure to scCO(2) indicated that these changes can be attributed to the dissolution/fracturing of calcite and clays in the matrix of the sample. Although findings were provided based on the pulse measurements tests, more studies are required to have a deeper understanding as to how geochemical reactions may cause difficulties during and after injection into a storage site. (C) 2016 Elsevier B.V. All rights reserved.
机译:对地质力学参数大小的变化进行系统而仔细的分析对于减轻二氧化碳封存地点泄漏的风险至关重要。但是,根据岩石和存储地点的不同,由于发生化学反应,这些变化可能会有所不同,尤其是在涉及盐水层的情况下。过去,很少有研究评估暴露于这些化学相互作用的岩石的最大持续压力。但是,当存储场所的恶劣环境中包含不同种类的岩石和流体(淡水或盐水)时,仍需要进行更多的研究来评估存储介质或密封件的强度。本文试图评估在短时间内注入超临界CO2期间和之后Berea砂岩的地质力学参数的变化。获得的结果表明,注入过程中孔隙空间中盐水的存在会加剧地球化学反应的严重性,从而导致包括剪切模量在内的弹性参数的大小降低。在暴露于scCO(2)之前和之后,对样品的SEM图像都有很好的了解,这些变化可能归因于方解石和粘土在样品基质中的溶解/破裂。尽管提供了基于脉冲测量测试的结果,但是需要进行更多的研究才能更深入地了解地球化学反应在注入存储地点期间和之后如何造成困难。 (C)2016 Elsevier B.V.保留所有权利。

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