Panav Hulsurkar, Abdelhalim I.A. Mohamed, Maziar Arshadi, Yanbin Gong, Mohammad Piri
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Steady-state (SS) drainage (non-wetting-phase displacing wetting-phase) and imbibition (wetting-phase displacing non-wetting-phase) tests were performed under a wide range of saturation histories (full-cycle and scanning-curves) to study relative permeability hysteresis of the propped fractures. Every SS drainage or imbibition test consisted of several discrete points at which fluid saturations and the corresponding relative permeability were measured by varying the fractional flow rates of fluids whilst maintaining a constant total flow rate. We analyzed residual non-wetting phase saturations and relative permeability trends to understand two-phase flow behavior in each proppant pack. High-resolution x-ray microtomography was used to understand the pore-scale topology, wettability, and to provide insights about the pore-scale displacement mechanisms involved in this study. 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引用次数: 0
摘要
在各种地下应用中,了解充满矿物和支撑剂的裂缝中的多相流至关重要。有限的实验数据导致人们依赖于缺乏物理基础的相关性。我们进行了实验,以确定未固结多孔介质填充的粗壁裂缝中的相对渗透率。我们测试了使用水湿 40/70 砂(硅石)和表面涂层陶瓷支撑剂填充的裂缝。盐水和矿物油分别用作润湿流体相和非润湿流体相。在多种饱和历史(全周期和扫描曲线)条件下进行了稳态(SS)排水(非润湿相置换润湿相)和浸润(润湿相置换非润湿相)试验,以研究支撑裂缝的相对渗透滞后性。每次 SS 排水或浸润试验都包括几个离散点,在这些点上,通过改变流体的部分流速,同时保持恒定的总流速,测量流体饱和度和相应的相对渗透率。我们分析了剩余非湿相饱和度和相对渗透率趋势,以了解每个支撑剂包中的两相流动行为。我们使用高分辨率 X 射线显微层析技术来了解孔隙尺度的拓扑结构和润湿性,并深入了解本研究涉及的孔隙尺度位移机制。结果表明,常用于估算裂缝相对渗透率的模型大大高估了本研究中测得的 SS 盐水和石油相对渗透率(用 krw 和 kro 表示)。进一步的分析表明,两种支撑剂在浸润过程中的 kro 值都超过了排水过程中的 kro 值,陶瓷支撑剂的初始水饱和度较低,排水位移结束时的终点 kro 渗透率较高,在所有浸润过程中的 krw 值也较高。研究还介绍了 Brooks-Corey 型相对渗透率相关性的最新拟合参数。本研究提出了更深入的见解、大量实验生成的相对渗透率数据以及更新的相对渗透率相关性,这些都可以用来减少与断裂地下地层多相流行为连续尺度预测相关的不确定性。
Steady-state two-phase relative permeability measurements in proppant-packed rough-walled fractures
Understanding multiphase flow in fractures filled with minerals and proppants is vital in various subsurface applications. Limited experimental data have led to reliance on correlations lacking physical basis. We conducted experiments to characterize relative permeability in rough-walled fractures packed with unconsolidated porous media. We tested fractures packed with water-wet 40/70 sand (silica) and surface-coated ceramic proppants. Brine and mineral oil were used as the wetting and non-wetting fluid phases, respectively. Steady-state (SS) drainage (non-wetting-phase displacing wetting-phase) and imbibition (wetting-phase displacing non-wetting-phase) tests were performed under a wide range of saturation histories (full-cycle and scanning-curves) to study relative permeability hysteresis of the propped fractures. Every SS drainage or imbibition test consisted of several discrete points at which fluid saturations and the corresponding relative permeability were measured by varying the fractional flow rates of fluids whilst maintaining a constant total flow rate. We analyzed residual non-wetting phase saturations and relative permeability trends to understand two-phase flow behavior in each proppant pack. High-resolution x-ray microtomography was used to understand the pore-scale topology, wettability, and to provide insights about the pore-scale displacement mechanisms involved in this study. The results showed that commonly used models to estimate relative permeabilities of fractures significantly overestimated the SS brine and oil relative permeabilities (denoted as krw and kro) measured in this study. Further analysis unveiled that the kro values during imbibition exceeded their drainage counterparts in both proppants, the ceramic proppant exhibited a lower initial water saturation and a higher end-point kro permeability at the end of the drainage displacement, as well as higher krw across all flooding processes. Updated fitting parameters for a Brooks-Corey-type relative permeability correlation are introduced. This study presents improved insights, extensive experimentally generated relative permeability data, and an updated relative permeability correlation, which can be collectively utilized to reduce uncertainties associated with continuum-scale forecasts of multiphase flow behavior in fractured subsurface formations.
期刊介绍:
Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources.
Examples of appropriate topical areas that will be considered include the following:
• Surface and subsurface hydrology
• Hydrometeorology
• Environmental fluid dynamics
• Ecohydrology and ecohydrodynamics
• Multiphase transport phenomena in porous media
• Fluid flow and species transport and reaction processes