Temperature dependence of water wettability on reservoir rock surfaces: In Situ characterization and mechanistic analysis based on subcritical water properties

IF 5.4 2区 化学 Q2 CHEMISTRY, PHYSICAL Colloids and Surfaces A: Physicochemical and Engineering Aspects Pub Date : 2025-03-28 DOI:10.1016/j.colsurfa.2025.136753
Kai Shan , Zhengsong Qiu , Xiaojun Wang , Shouzhi Wang , Yu Jiang , Xiaoxia Ren , Hanyi Zhong , Xin Zhao
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Abstract

The exploration of deep, high-temperature oil and gas reservoirs is increasingly critical for future energy solutions. Understanding the in-situ wettability of reservoir rocks at high temperatures is essential to prevent water phase trapping and optimize enhanced oil recovery methods. This study employs a high-temperature, high-pressure contact angle measurement system to assess water contact angles on various rock surfaces, within a temperature range of 20°C to 200°C, under an 8 MPa nitrogen atmosphere. The mechanism of temperature-dependent wettability changes was conducted using molecular simulation, atomic force microscopy, scanning electron microscopy, and energy-dispersive X-ray spectroscopy. Findings reveal that the contact angle on quartz surfaces reduces with temperature, exhibiting distinct segmented behavior. The rate of change in contact angle was approximately −0.07°/°C from 20°C to 100°C and −0.17°/°C from 100°C to 200°C. Under subcritical conditions, an increase in hydrogen bonds between water molecules and the silica surface, along with a reduction in hydrogen bonds between water molecules, markedly influences the wettability on quartz surfaces. Water contact angles on crude oil-adsorbed rock samples progressively declined with increasing temperature, from 108.3° to 52.3°, transitioning the surface from oleophilic to hydrophilic. The adhesion work of water on these oil-adsorbed rock surfaces remained nearly constant up to 100°C; beyond this, under subcritical conditions, the adhesion work surged, with a change rate of 49.14 % at 200°C. Microscopic analysis of rock surface morphology and elemental composition, combined with the physicochemical properties of subcritical water, indicated that the desorption or thermal degradation of hydrocarbons adsorbed on the rock surfaces under the action of the subcritical water significantly alters their wettability characteristics. This research offers novel insights into the mechanisms driving wettability changes on high-temperature reservoir rock surfaces and supports the development of effective strategies for preventing water phase trapping and enhancing oil recovery.
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储层岩石表面水润湿性的温度依赖性:基于亚临界水特性的原位表征和机理分析
对于未来的能源解决方案来说,勘探深层、高温油气储层变得越来越重要。了解储层岩石在高温下的原位润湿性对于防止水相圈闭和优化提高采收率的方法至关重要。本研究采用高温高压接触角测量系统,在温度为20℃~ 200℃,氮气压力为8 MPa的条件下,对不同岩石表面的水接触角进行了测量。利用分子模拟、原子力显微镜、扫描电镜和能量色散x射线能谱分析了温度依赖性润湿性变化的机理。结果表明,石英表面的接触角随温度的升高而减小,呈现出明显的分节行为。从20°C到100°C,接触角的变化率约为- 0.07°/°C,从100°C到200°C,其变化率约为- 0.17°/°C。在亚临界条件下,水分子与二氧化硅表面之间氢键的增加,以及水分子之间氢键的减少,显著影响石英表面的润湿性。随着温度的升高,原油吸附岩石表面的水接触角逐渐减小,从108.3°降至52.3°,由亲油向亲水转变。在100°C以下,水在这些油吸附岩石表面的粘附作用几乎保持不变;在亚临界条件下,黏附功急剧增加,在200℃时的变化率为49.14 %。岩石表面形貌和元素组成的微观分析,结合亚临界水的物理化学性质,表明在亚临界水的作用下,烃类吸附在岩石表面的解吸或热降解显著改变了岩石表面的润湿性特征。该研究为高温储层岩石表面润湿性变化的驱动机制提供了新的见解,并为防止水相圈闭和提高采收率的有效策略的开发提供了支持。
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来源期刊
CiteScore
8.70
自引率
9.60%
发文量
2421
审稿时长
56 days
期刊介绍: Colloids and Surfaces A: Physicochemical and Engineering Aspects is an international journal devoted to the science underlying applications of colloids and interfacial phenomena. The journal aims at publishing high quality research papers featuring new materials or new insights into the role of colloid and interface science in (for example) food, energy, minerals processing, pharmaceuticals or the environment.
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