Reza Khoramian, Ibraheem Salaudeen, Peyman Pourafshary, Masoud Riazi, Riyaz Kharrat
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Abstract
The urgent challenge of climate change, driven by rising carbon emissions, necessitates innovative strategies for carbon capture and storage (CCS). This study examines the impact of hysteresis in relative permeability on CO2 entrapment efficiency within saline aquifers, known for their significant storage capabilities. An aquifer model was analyzed through numerical simulation by varying hysteresis values from 0.2 to 0.5 to evaluate their impact on CO2 plume behavior, retention during water-alternating-gas (WAG) injection, and plume morphology. The CO2 plume exhibits a funnel-shaped configuration at low hysteresis with a narrow, pointed base, indicating a concentrated upward migration trajectory. In contrast, a hysteresis value of 0.5 results in diminished gas movement toward the upper aquifer, transforming the plume into a more oval shape. Results from the land trapping model further support our findings, revealing an inverse relationship where increased hysteresis enhances residual CO2 entrapment, reflected in trapping coefficient values ranging from 0.5 to 4. This underscores the model's efficacy in verifying gas trapping efficiency and safety during sequestration. Moreover, increased water flow generates stronger forces, pushing CO2 into narrower pore spaces, where it becomes trapped. Our findings indicate that increased hysteresis enhances CO2 retention by limiting vertical migration and significantly influences plume geometry, promoting stable and predictable distribution patterns. At higher hysteresis values, CO2 migration is significantly restricted, resulting in near-complete immobilization of the injected gas. This research highlights hysteresis's critical role in refining injection methodologies and enhancing plume stability for long-term CO2 storage. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.
相对渗透率滞后效应对含盐含水层CO2储存量的影响
由碳排放上升所驱动的气候变化的紧迫挑战,需要创新的碳捕获与封存(CCS)战略。本研究考察了相对渗透率的滞后对含盐含水层中二氧化碳捕获效率的影响,含盐含水层以其显著的储存能力而闻名。通过对含水层模型进行数值模拟,分析了迟滞值在0.2 ~ 0.5范围内的变化,以评估其对CO2羽流行为、水-气交替(WAG)注入过程中的滞留以及羽流形态的影响。CO2羽流在低迟滞时呈漏斗状结构,底部窄而尖,呈集中向上运移轨迹。相反,滞后值为0.5时,气体向上层含水层的运动减少,使羽流变成更椭圆形的形状。陆地捕获模型的结果进一步支持了我们的发现,揭示了一个反比关系,即滞后增加会增加剩余二氧化碳的捕获,这反映在捕获系数的0.5到4之间。这强调了该模型在验证封存期间的气体捕获效率和安全性方面的有效性。此外,增加的水流产生更强的力,将二氧化碳推入更窄的孔隙空间,在那里被困住。研究结果表明,迟滞的增加通过限制垂直迁移来增强CO2的滞留,并显著影响羽流的几何形状,促进稳定和可预测的分布模式。在较高的迟滞值下,二氧化碳的运移受到明显限制,导致注入气体几乎完全不动。这项研究强调了迟滞在改进注入方法和提高长期二氧化碳储存羽流稳定性方面的关键作用。©2024化学工业协会和John Wiley &;儿子,有限公司
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