立陶宛盆地深部含盐含水层存在断层和裂缝时CO2注入的机理模拟方法评估CO2泄漏

Shankar Lal Dangi, Shruti Malik, Pijus Makauskas, Vilte Karliute, Ravi Sharma, Mayur Pal
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引用次数: 0

摘要

向深层盐水含水层注入二氧化碳是碳捕获与封存(CCS)减少温室气体排放的重要策略。然而,确保二氧化碳储存的长期完整性对于防止泄漏和潜在的环境危害至关重要。本文研究了Syderiai深层咸水层注入二氧化碳用于碳捕集与封存(CCS)的情况下,裂缝渗透率对co2泄漏体积的影响。研究了裂缝渗透率与CO 2泄漏可能性之间的关系,以及盖层上下水中溶解的CO 2体积。此外,该研究还研究了Syderiai深盐水含水层的泄漏量如何随时间演变。基于平均渗透率、孔隙度、NTG和厚度,建立了立陶宛盆地Syderiai深盐水含水层的机理模型(图1),并用于本次分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of CO2 leakage using mechanistic modelling approach for CO2 injection in deep saline aquifer of Lithuanian basin in presence of fault and fractures
Injecting CO 2 into deep saline aquifers is a prominent strategy for carbon capture and storage (CCS) to mitigate greenhouse gas emissions. However, ensuring the long-term integrity of CO 2 storage is crucial to prevent leakage and potential environmental hazards. This paper investigates the impact of fracture permeability on CO 2 leakage volumes in the context of CO 2 injection into Syderiai deep saline aquifer for carbon capture and storage (CCS) applications. It explores the relationship between fracture permeability and the potential for CO 2 leakage, as well as the volume of CO 2 dissolved in water above and below the cap rock. Furthermore, the study examines how the leakage volume may evolve over time in Syderiai deep saline aquifer. A mechanistic model of Syderiai deep saline aquifer, of Lithuanian basin, was developed based on average permeability, porosity, NTG and thickness (Fig. 1) and is used in this analysis.
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