Zankoor Ahmed, Khishvand Mahdi, Mohamed Abdelhalim, Wang Rui, Piri Mohammad
Center of Innovation for Flow through Porous Media, Department of Petroleum Engineering, University of Wyoming, Laramie, WY 82071, USA.
Center of Innovation for Flow through Porous Media, Department of Petroleum Engineering, University of Wyoming, Laramie, WY 82071, USA.
J Colloid Interface Sci. 2021 Dec;603:356-369. doi: 10.1016/j.jcis.2021.06.052. Epub 2021 Jun 15.
Geometrical analyses of pore-scale fluid-fluid-rock interfaces have recently been used for in-situ characterization of capillary pressure and wettability in natural porous media. Nevertheless, more robust techniques and multi-scale, well-characterized experimental data are needed to rigorously validate these techniques and enhance their efficacy when applied to saturated porous media.
We present two new techniques for automated measurements of in-situ capillary pressure and contact angle, which offer several advancements over previous methodologies. These approaches are methodically validated using synthetic data and X-ray images of capillary rise experiments, and subsequently, applied on pore-scale fluid occupancy maps of a miniature Berea sandstone sample obtained during steady-state drainage and imbibition flow experiments.
The results show encouraging agreement between the image-based capillary pressure-saturation function and its macroscopic counterpart obtained from a porous membrane experiment. However, unlike the macroscopic behavior, the micro-scale measurements demonstrate a nonmonotonic increase with saturation due to the intermittency of the pore-scale displacement events controlling the overall flow behavior. This is further explained using the pertinent micro-scale mechanisms such as Haines jumps. The new methods also enable one to generate in-situ contact angle distributions and distinguish between the advancing and receding values while automatically excluding invalid measurements.
孔隙尺度流体-流体-岩石界面的几何分析最近已用于天然多孔介质中毛细管压力和润湿性的原位表征。然而,需要更强大的技术和多尺度、特征明确的实验数据来严格验证这些技术,并提高其应用于饱和多孔介质时的功效。
我们提出了两种用于自动测量原位毛细管压力和接触角的新技术,与以前的方法相比有几个进步。这些方法通过合成数据和毛细管上升实验的X射线图像进行了系统验证,随后应用于在稳态排水和吸水流动实验中获得的微型 Berea 砂岩样品的孔隙尺度流体占有率图。
结果表明,基于图像的毛细管压力-饱和度函数与其从多孔膜实验获得的宏观对应物之间的一致性令人鼓舞。然而,与宏观行为不同,微观尺度测量显示随着饱和度的增加呈非单调增加,这是由于控制整体流动行为的孔隙尺度位移事件的间歇性。使用诸如海恩斯跳跃等相关微观尺度机制对此进行了进一步解释。新方法还使人们能够生成原位接触角分布,并区分前进和后退值,同时自动排除无效测量。