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MICROFLUIDIC STUDY OF DRAINAGE AND IMBIBITION IN POROUS MEDIA: DEFINITION OF AMOTT INDICES

机译:多孔介质中排水和吸水的微流控研究:阿莫特指数的定义

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The wettability of reservoir rocks plays a critical role in oil recovery operations. This property is traditionally defined in terms of the contact angle between the fluid-fluid interface and the solid surface. In natural porous media, it has been preferred to characterize the wettability and its effects on fluid flow behavior in terms of Amott indices, through the capillary pressure-fluid saturation relationship. This "bulk" definition is based on the steady states reached by the two phases, the wetting one and the non-wetting one, upon drainage (removal of the wetting fluid) and imbibition (removal of the non-wetting fluid). These indices provide some indirect indication of the rock surface chemistry and porosity structure. Previous studies on Amott indices have mostly focused on numerical modeling of rocks. In this paper, we present an experimental study on two phase flow in regular lattices of glass microchannels. A wet etching technique is used to fabricate 2D networks composed of hundreds of repeat units. The repeat units are square, hexagonal, or triangular, with a lattice parameter of about 100 micrometers. Controlling and varying the microchannel wettability, network geometry, and fluid properties allow correlating the physical chemistry of the system and the characteristics of the multiphase flow. We perform drainage-imbibition cycles by controlling the pressure difference across the device. For each pressure difference, we record and characterize the distribution of the two phases at equilibrium. Our results capture the dependance of the Amott index on both fluid and network properties. The values obtained are consistent with previous studies on wetting phenomena at the pore level. The drainage-imbibition cycles also provide information on the patterns of invasion. We show that the study of the cycles can further predictability of Amott indices.
机译:储层岩石的润湿性在采油作业中起着至关重要的作用。传统上,根据流体-流体界面与固体表面之间的接触角定义此属性。在天然多孔介质中,最好通过毛细压力-流体饱和度关系用Amott指数表征润湿性及其对流体流动行为的影响。这种“大体积”的定义是基于排水(除去润湿液)和吸取(除去非润湿液)两个阶段达到的稳态,即润湿阶段和非润湿阶段。这些指数间接指示了岩石表面化学性质和孔隙结构。以前有关Amott指数的研究主要集中在岩石的数值模拟上。在本文中,我们对玻璃微通道规则晶格中的两相流进行了实验研究。湿法蚀刻技术用于制造由数百个重复单元组成的2D网络。重复单元是正方形,六边形或三角形,其晶格参数约为100微米。控制和改变微通道的可湿性,网络几何形状和流体特性,可以使系统的物理化学性质与多相流的特性相关联。我们通过控制设备上的压差来执行排水吸水循环。对于每个压力差,我们记录并描述两相在平衡状态下的分布。我们的结果捕获了Amott指数对流体和网络特性的依赖性。获得的值与先前关于孔水平的润湿现象的研究一致。排水-吸水循环还提供了有关入侵方式的信息。我们表明,对周期的研究可以进一步预测Amott指数的可预测性。

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