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In-situ characterization of wettability and pore-scale displacements during two- and three-phase flow in natural porous media

机译:天然多孔介质中两相和三相流动过程中的润湿性和孔尺度位移的原位表征

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摘要

We establish a unique approach to measure in-situ contact angle from micro-CT images acquired during two-and three-phase miniature core-flooding experiments in order to overcome the uncertainties associated with conventional contact angle measurement techniques. The measurements are used to quantify the wettability behavior of the rock and explain pore-level displacement events occurring in three-phase flow. Six two-phase experiments are performed on individual core samples with three pairs of fluids, i.e., oil-brine, gas-oil, and gas-brine, and under two thermodynamic conditions: (a) binary-equilibrated, when only the two respective phases are at equilibrium and (b) ternary-equilibrated, when all three phases are equilibrated and only the two desired fluids are injected into the core. A three-phase experiment set is also performed under ternary-equilibrated conditions, which includes gas injection, a waterflood, and an oilflood process. All experiments are performed on Berea miniature core samples using a nonspreading brine-oil-gas fluid system.
机译:我们建立了一种独特的方法来测量在两相和三相微型堆芯注水实验中获得的微型CT图像中的原位接触角,以克服与常规接触角测量技术相关的不确定性。这些测量用于量化岩石的润湿性,并解释在三相流中发生的孔隙水平位移事件。在两个热力学条件下,用三对流体,即油-盐水,瓦斯油和瓦斯-盐水,对单个岩心样品进行六个两阶段实验:(a)二元平衡,当只有两个分别当所有三相均已平衡且仅将两种所需流体注入岩心时,相处于平衡状态且(b)三元平衡。在三元平衡的条件下也执行了一个三相实验装置,包括注气,注水和注油过程。所有实验均使用非扩散盐水-油气流体系统对Berea微型岩心样本进行。

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