3D Visualization of Film Flow During Three-Phase Displacement in Water-Wet Rocks via Microtomography Method

W. N. A. W. Razak, N. I. Kechut, E. Andrews, S. Krevor
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Abstract

Spatial image resolution has limited previous attempts to characterize the thin film flow of oil sandwiched in-between gas and water in a three-phase fluid system This paper describes how a systematically designed displacement experiment can produce imagery to define the film flow process in a 3D pore space of water-wet sandstone rocks. We image multiphase flow at the pore scale through three displacement experiments conducted on water-wet outcrop rock with variable spreading tendencies. The experiment has been formulated to observe the relationship between fluid spreading, phase saturations, and pore-scale displacement mechanisms. We provide exhaustive evidence of the three-phase fluid configurations that serve as a proxy mechanism assisting the fluid displacement process in a three-phase system, which includes the oil sandwiches in-between water and gas, the flow of oil via clay fabrics, and the double-displacement process that generates oil and water film in 3D pore spaces. Further, we show evidence that the stable thin-oil film has enhanced the gas trapping mechanism in the water-wet rocks. We observed that the oil layer had covered the isolated and trapped gas blobs, enhancing their stability. As a result, the trapped gas in the positive and zero spreading systems is slightly higher than in the negative spreading system due to a stable oil film. We analyze the Euler characteristic of the individual fluid phases and the interface pair of the fluids during waterflooding, gas injection, and chase water flooding. The comparison of the Euler characteristic for the connected and disconnected fluid phases between three different spreading systems (i.e., positive, zero, and negative) shows that the oil layer's connectivity is highest in the positive spreading system and lowest in the negative spreading system. The oil layer in the positive spreading system is also thicker than in the negative spreading system.
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水湿岩石三相位移过程中膜流的微层析成像三维可视化
空间图像分辨率限制了之前表征三相流体系统中夹在气和水之间的油薄膜流动的尝试。本文描述了一个系统设计的位移实验如何产生图像来定义水湿砂岩三维孔隙空间中的膜流动过程。通过对不同扩展趋势的露头水湿岩进行三次驱替实验,在孔隙尺度上对多相流进行成像。该实验旨在观察流体扩散、相饱和度和孔隙尺度位移机制之间的关系。我们提供了详尽的证据,证明三相流体结构可以作为辅助三相系统流体驱替过程的代理机制,包括水和气之间的油夹层、油通过粘土结构的流动,以及在三维孔隙空间中产生油水膜的双重驱替过程。此外,我们还证明了稳定的薄油膜增强了水湿岩中的气体捕获机制。我们观察到,油层已经覆盖了孤立的和被困的气体团,增强了它们的稳定性。结果表明,由于油膜稳定,正扩散系统和零扩散系统的截留气略高于负扩散系统。分析了水驱、注气和驱水过程中各个流体相和流体界面对的欧拉特性。对比三种不同扩散体系(正、零、负)连通与不连通流体相的欧拉特性,发现正扩散体系中油层连通性最高,负扩散体系中油层连通性最低。正扩散系统中的油层也比负扩散系统中的油层厚。
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