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Surface wettability alteration of shales exposed to CO2: Implication for long-term integrity of geological storage sites
International Journal of Greenhouse Gas Control ( IF 3.9 ) Pub Date : 2021-08-09 , DOI: 10.1016/j.ijggc.2021.103426
Ahmed Fatah 1 , Ziad Bennour 1 , Hisham Ben Mahmud 1 , Raoof Gholami 2 , Mofazzal Hossain 3
Affiliation  

Surface wettability is a key factor controlling the CO2 seal capacity and defines the CO2 storage potential. Limited studies have addressed the shale/water wettability behavior during CO2 injection, thus considerable attention is needed to understand this concept. In this paper, an ample number of supercritical CO2 exposure experiments were conducted to evaluate the alteration of shale/water contact angles. Different types of shales with various mineralogy from Eagle Ford, Wolfcamp, and Mancos fields, were exposed to SCCO2 at different durations, pressures, and temperatures. Shale mineralogy and surface were analyzed using X-ray diffraction and scanning electron microscope. The results indicated a strong relationship between mineral composition and the alteration in shale/water wettability. Clay-rich shales displayed a possible turn in wetting behavior to CO2-wet with extending the SCCO2 treatment time and increasing the treatment pressure, caused by SCCO2 dissolution of clay and carbonate minerals. While the wettability of high-quartz contents shales remained strongly hydrophilic after various SCCO2 treatment conditions. Increasing the temperature accelerated the CO2/shale interactions, and a minor effect was observed on the shale hydrophilicity. Increasing the cohesive energy density of CO2 promotes a favorable CO2 wetting environment, which reduced the hydrophilicity of the surface and reduces the surface energy. In conclusion, shales with high quartz contents exhibit strong water wetting behavior after SCCO2 treatment, which leads to better sealing capacity, more efficient integrity of geological storage sites, and higher potential for CO2 containment.



中文翻译:

暴露于 CO2 的页岩的表面润湿性改变:对地质封存场长期完整性的影响

表面润湿性是控制 CO 2密封能力的关键因素,并定义了 CO 2储存潜力。有限的研究已经解决了 CO 2注入过程中的页岩/水润湿性行为,因此需要相当多的注意力来理解这个概念。在本文中,进行了大量超临界 CO 2暴露实验以评估页岩/水接触角的变化。来自 Eagle Ford、Wolfcamp 和 Mancos 油田的不同矿物类型的页岩在不同的持续时间、压力和温度下暴露于 SCCO 2。使用X分析页岩矿物学和表面射线衍射和扫描电子显微镜。结果表明矿物组成与页岩/水润湿性的改变之间存在很强的关系。随着SCCO 2处理时间的延长和处理压力的增加,由于粘土和碳酸盐矿物的SCCO 2溶解,富含粘土的页岩的润湿行为可能转变为CO 2湿的。而高石英含量页岩的润湿性在各种 SCCO 2处理条件后仍保持强亲水性。升高温度加速了CO 2 /页岩的相互作用,并且观察到对页岩亲水性的影响较小。提高 CO 2的内聚能密度促进了有利的 CO 2润湿环境,从而降低了表面的亲水性并降低了表面能。总之,石英含量高的页岩在 SCCO 2处理后表现出较强的水润湿行为,这导致更好的密封能力、更有效的地质封存场完整性和更高的 CO 2围堵潜力。

更新日期:2021-08-09
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