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复杂多孔材料中的润湿性、混合润湿状态及其与表面粗糙度的关系。

Wettability in complex porous materials, the mixed-wet state, and its relationship to surface roughness.

机构信息

Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, United Kingdom

Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, United Kingdom.

出版信息

Proc Natl Acad Sci U S A. 2018 Sep 4;115(36):8901-8906. doi: 10.1073/pnas.1803734115. Epub 2018 Aug 17.

Abstract

A quantitative in situ characterization of the impact of surface roughness on wettability in porous media is currently lacking. We use reservoir condition micrometer-resolution X-ray tomography combined with automated methods for the measurement of contact angle, interfacial curvature, and surface roughness to examine fluid/fluid and fluid/solid interfaces inside a porous material. We study oil and water in the pore space of limestone from a giant producing oilfield, acquiring millions of measurements of curvature and contact angle on three millimeter-sized samples. We identify a distinct wetting state with a broad distribution of contact angle at the submillimeter scale with a mix of water-wet and water-repellent regions. Importantly, this state allows both fluid phases to flow simultaneously over a wide range of saturation. We establish that, in media that are largely water wet, the interfacial curvature does not depend on solid surface roughness, quantified as the local deviation from a plane. However, where there has been a significant wettability alteration, rougher surfaces are associated with lower contact angles and higher interfacial curvature. The variation of both contact angle and interfacial curvature increases with the local degree of roughness. We hypothesize that this mixed wettability may also be seen in biological systems to facilitate the simultaneous flow of water and gases; furthermore, wettability-altering agents could be used in both geological systems and material science to design a mixed-wetting state with optimal process performance.

摘要

目前缺乏对表面粗糙度对多孔介质润湿性影响的定量原位表征。我们使用储层条件下的微米分辨率 X 射线断层扫描技术,并结合自动测量接触角、界面曲率和表面粗糙度的方法,来研究多孔材料内部的流体/流体和流体/固体界面。我们研究了来自巨型产油区石灰岩孔隙空间中的油和水,在三个毫米大小的样本上获取了数百万次曲率和接触角的测量值。我们在亚毫米尺度上识别出一种具有广泛接触角分布的明显润湿状态,其中存在水湿和疏水区域的混合。重要的是,这种状态允许两种流体相在广泛的饱和度范围内同时流动。我们发现,在大部分为水湿的介质中,界面曲率不依赖于固体表面粗糙度,即局部偏离平面的程度。然而,在润湿性发生显著变化的地方,较粗糙的表面与较低的接触角和较高的界面曲率相关。接触角和界面曲率的变化都随局部粗糙度的增加而增加。我们假设这种混合润湿性也可能在生物系统中看到,以促进水和气体的同时流动;此外,润湿性改变剂可以在地质系统和材料科学中使用,以设计具有最佳工艺性能的混合润湿状态。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8696/6130345/5976a584a652/pnas.1803734115fig01.jpg

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