Effects of CO2 pressure on the dynamic wettability of the kerogen surface: Insights from a molecular perspective

IF 6.3 2区 材料科学 Q2 CHEMISTRY, PHYSICAL Applied Surface Science Pub Date : 2025-02-26 DOI:10.1016/j.apsusc.2025.162822
Zhiming Yan , Fengjiao Wang , Yikun Liu , Jun Zhang , Lu Liu , Mingyu Gao
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Abstract

Wettability is crucial in controlling fluid flow in shale reservoirs, significantly impacting both enhanced oil and gas recovery and CO2 geological storage. In this work, a high-pressure dynamic wettability mathematical model was established considering the roles of viscosity and adhesion to investigate the dynamic wettability of kerogen substrate at various CO2 pressures. The wettability of kerogen substrate gradually transitioned from intermediate-wet to strongly CO2-wet as CO2 pressure increased. From a molecular viewpoint, the water-wetness of kerogen substrate was mainly affected by van der Waals and hydrogen bonds between O atoms in the kerogen substrate and the OH group in water molecules. As CO2 pressure increased, a carbon dioxide film formed on the substrate due to competitive adsorption. The shielding effect of this film reduced both non-bond interactions and hydrogen bonds, resulting in lower water-wetness. From the viewpoint of activation free energy, CO2 pressure primarily affected the water-wetness of kerogen substrate by modifying solid–liquid interactions, with little effect on viscosity. As CO2 pressure increased, the activation free energy associated with adhesion increased, leading to a lower friction coefficient and a higher wettability activation energy. The link between the dynamic contact angle and the speed of contact line was first quantitatively characterized, and the dynamic wettability mechanism in the high-pressure CO2-H2O-kerogen system was clarified. The research provides new theoretical insights into fluid flow in nanopores and provides more reliable references for calculating the efficiency of enhanced oil and gas recovery and CO2 geological storage.

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润湿性是控制页岩储层流体流动的关键,对提高油气采收率和二氧化碳地质封存都有重大影响。在这项工作中,考虑到粘度和粘附力的作用,建立了一个高压动态润湿性数学模型,以研究不同二氧化碳压力下角质原基质的动态润湿性。随着 CO2 压力的增加,角质层基底的润湿性从中度润湿逐渐过渡到强 CO2 润湿。从分子角度看,角质基质的水湿性主要受角质基质中 O 原子与水分子中 OH 基团之间的范德华键和氢键的影响。随着二氧化碳压力的增加,基质上会形成一层二氧化碳竞争吸附膜。这层膜的屏蔽作用减少了非键相互作用和氢键,从而降低了水的湿润性。从活化自由能的角度来看,二氧化碳压力主要通过改变固液相互作用来影响角质基质的水湿性,对粘度的影响很小。随着二氧化碳压力的增加,与粘附相关的活化自由能也随之增加,从而导致摩擦系数降低,润湿性活化能升高。该研究首次定量描述了动态接触角与接触线速度之间的联系,并阐明了高压 CO2-H2O-kerogen 体系中的动态润湿机制。该研究为纳米孔隙中的流体流动提供了新的理论见解,为计算提高油气采收率和二氧化碳地质封存效率提供了更可靠的参考。
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来源期刊
Applied Surface Science
Applied Surface Science 工程技术-材料科学:膜
CiteScore
12.50
自引率
7.50%
发文量
3393
审稿时长
67 days
期刊介绍: Applied Surface Science covers topics contributing to a better understanding of surfaces, interfaces, nanostructures and their applications. The journal is concerned with scientific research on the atomic and molecular level of material properties determined with specific surface analytical techniques and/or computational methods, as well as the processing of such structures.
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