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基于事件的多孔介质内接触角测量:使用时间分辨微计算机断层扫描技术。

Event-based contact angle measurements inside porous media using time-resolved micro-computed tomography.

机构信息

PProGRess/UGCT, Dept. of Geology, Ghent University, Krijgslaan 281/ S8, 9000 Ghent, Belgium.

PProGRess/UGCT, Dept. of Geology, Ghent University, Krijgslaan 281/ S8, 9000 Ghent, Belgium; Environmental Hydrogeology, Dept. of Earth Sciences, Utrecht University, Princetonlaan 8a, 3584 Utrecht, the Netherlands.

出版信息

J Colloid Interface Sci. 2020 Jul 15;572:354-363. doi: 10.1016/j.jcis.2020.03.099. Epub 2020 Mar 27.

Abstract

HYPOTHESIS

Capillary-dominated multiphase flow in porous materials is strongly affected by the pore walls' wettability. Recent micro-computed tomography (mCT) studies found unexpectedly wide contact angle distributions measured on static fluid distributions inside the pores. We hypothesize that analysis on time-resolved mCT data of fluid invasion events may be more directly relevant to the fluid dynamics.

EXPERIMENT

We approximated receding contact angles locally in time and space on time-resolved mCT datasets of drainage in a glass bead pack and a limestone. Whenever a meniscus suddenly entered one or more pores, geometric and thermodynamically consistent contact angles in the surrounding pores were measured in the time step just prior to the displacement event. We introduced a new force-based contact angle, defined to recover the measured capillary pressure in the invaded pore throat prior to interface movement.

FINDINGS

Unlike the classical method, the new geometric and force-based contact angles followed plausible, narrower distributions and were mutually consistent. We were unable to obtain credible results with the thermodynamically consistent method, likely because of sensitivity to common imaging artifacts and neglecting dissipation. Time-resolved mCT analysis can yield a more appropriate wettability characterization for pore scale models, despite the need to further reduce image analysis uncertainties.

摘要

假设

多孔材料中以毛细管为主导的多相流受孔隙壁润湿性的强烈影响。最近的微计算机断层扫描(mCT)研究发现,在孔隙内静态流体分布上测量的接触角分布出人意料地宽。我们假设对流体侵入事件的时变 mCT 数据分析可能与流体动力学更直接相关。

实验

我们在玻璃珠填充和石灰岩排水的时变 mCT 数据集上局部近似了时变接触角,只要弯月面突然进入一个或多个孔隙,就在位移事件之前的时间步中测量周围孔隙中的几何和热力学一致的接触角。我们引入了一种新的基于力的接触角,该接触角定义为在界面移动之前恢复侵入的孔隙喉道中的测量毛细管压力。

发现

与经典方法不同,新的几何和基于力的接触角遵循合理的、更窄的分布且相互一致。我们无法使用热力学一致的方法获得可靠的结果,可能是因为对常见成像伪影敏感且忽略了耗散。尽管需要进一步降低图像分析的不确定性,但时变 mCT 分析可以为孔隙尺度模型提供更合适的润湿性描述。

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