Wettability Alteration of Carbonates with Seawater and Higher Salinity Brines Explored Using a 3D Micromodel

Grecia Ro
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Abstract

We provide experimental evidence of wettability alteration using seawater salinity brine of an oil-wet system composed of a three-dimensional carbonate micromodel, crude oil, and connate-water brine salinity. We designed this procedure as a first step for evaluation of using seawater as an Improved Oil Recovery (IOR) agent. Our innovative design combines two main experimental best practices: micromodels, for repeatable experiments and X-ray computed tomography (CT) as a non-invasive technique for monitoring in situ fluid distribution. Both practices merge into a new three-dimensional micromodel set-up that uses only reservoir species (no high x-ray contrast chemicals). Wettability alteration plays a key role to improve oil recovery from matrix blocks surrounded by water-invaded fractures in carbonate reservoir rocks. We designed a simple and replicable experimental apparatus and procedure to quantify contact angle distributions inside of porous media with a controlled level of heterogeneity in roughness and mineralogy. This experiment consists of visualizing the in-situ contact angle distribution of the aqueous phase inside a three-dimensional carbonate micromodel. Using Micro Computerized Tomography (MicroCT), we obtained three-dimensional images of fluid distribution with a voxel size of 3.8 microns. We successfully studied the wettability state after connate water displacement and we also altered wettability of the carbonate porous medium from more oil wet to less water wet conditions. The water contact angle of the ganglia showed a 70% reduction in contact angle from an oil-wet to a water-wet system using an approximate seawater salinity and a 63% reduction in contact angle in the case of a full synthetic seawater. The initial average contact angles were 140° and 142° for the two solutions, respectively. After EOR seawater flooding, the average contact angle declined to 44° and 51°, respectively.
三维微模型研究碳酸盐岩在海水和高盐度盐水中的润湿性变化
我们利用三维碳酸盐微模型、原油和原生水盐水盐度组成的油湿体系的海水盐度盐水,提供了润湿性变化的实验证据。我们设计了这个程序,作为评估使用海水作为提高采收率(IOR)剂的第一步。我们的创新设计结合了两种主要的实验最佳实践:用于可重复实验的微模型和用于监测原位流体分布的无创x射线计算机断层扫描(CT)技术。这两种方法合并成一种新的三维微观模型,只使用储层物种(不使用高x射线对比化学物质)。在碳酸盐岩储集层中,润湿性蚀变是提高被水侵裂缝包围的基质块采收率的关键。我们设计了一个简单且可复制的实验装置和程序来量化多孔介质内部的接触角分布,并控制粗糙度和矿物学的非均质性水平。本实验包括可视化三维碳酸盐微模型中水相的原位接触角分布。利用微计算机断层扫描(MicroCT),我们获得了3.8微米体素尺寸的流体分布的三维图像。我们成功地研究了原生水驱替后的润湿性状态,并将碳酸盐多孔介质的润湿性从多油湿润状态改变为少水湿润状态。在近似的海水盐度下,从油湿系统到水湿系统,神经节的水接触角减少了70%,在全合成海水的情况下,接触角减少了63%。两种溶液的初始平均接触角分别为140°和142°。EOR海水驱后,平均接触角分别降至44°和51°。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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