基于表面简化络合模型的碳酸盐岩储层润湿性改进剂注入解析解

Ricardo A. Lara Orozco, R. Okuno, L. Lake
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引用次数: 0

摘要

调成分水驱提高碳酸盐岩油藏采收率的潜力已经在文献中得到了广泛的研究。一致认为,润湿性变化的发生是由于碳酸盐岩表面与电位决定离子Ca2+、Mg2+、CO32−和SO42−之间的静电相互作用。最近,甘氨酸作为最简单的氨基酸,也被研究作为碳酸盐的润湿性改性剂,其作用类似于盐水中的硫酸盐离子。通过表面络合模型(SCM)描述了甘氨酸和方解石等润湿性调节剂对岩石润湿性的影响,并将润湿性与表面电位的变化联系起来。然而,地球化学反应相关性的确定受到SCM复杂性的阻碍。此外,表面电位作为岩石润湿状态的替代品与文献中报道的甘氨酸实验结果不相关。本研究利用单片机对方解石的单相置换结果进行了分析,确定了重要的表面络合反应。然后,将润湿性变化建模为润湿性改性剂(如SO42 -和Gly -)与吸附的羧酸之间的一系列阴离子交换反应。最后,给出了具有阴离子交换反应的两相多组分反应输运耦合模型的解析解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analytical Solutions for the Injection of Wettability Modifiers in Carbonate Reservoirs Based on a Reduced Surface Complexation Model
The potential of tuned-composition waterflooding to enhance oil recovery from carbonate reservoirs has been widely investigated in the literature. The consensus is that wettability alteration occurs because of the electrostatic interactions between the carbonate rock surface and the potential determining ions, Ca2+, Mg2+, CO32−, and SO42−. Recently, glycine, the simplest amino acid, has also been investigated as a wettability modifier for carbonates that acts similarly as the sulfate ions in brine. The impact of wettability modifiers like glycine and calcite's potential determining ions has been described by surface complexation models (SCM) and the wetting-state of the rock has been related to change of the surface potential. However, determining the relevance of the geochemical reactions is obstructed by the complexity of the SCM. Moreover, the surface potential as a surrogate of the wetting-state of the rock does not correlate with the experimental results with glycine reported in the literature. The present research analyzed the results of single-phase displacement using a SCM for calcite to determine the important surface complexation reactions. Then, wettability alteration is modeled as a set of anion exchange reactions between wettability modifiers, like SO42− and Gly−, and adsorbed carboxylic acids. Finally, analytical solutions are presented for the coupled two-phase and multicomponent reactive-transport model with anion exchange reactions.
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