一种改善非均质碳酸盐岩储层酸分流的新型阳离子聚合物体系

A. Sarmah, Ahmed Farid Ibrahim, H. Nasr-El-Din, J. Jackson
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引用次数: 3

摘要

原位胶凝酸用于非均质碳酸盐岩储层的酸分流已有20多年的历史。大多数胶凝体系都是基于阴离子聚合物,在酸处理后存在清洗问题,导致地层受损。本研究评估了一种具有自破能力的新型阳离子-聚合物酸体系,该体系可作为碳酸盐岩储层中的酸性分散剂。实验研究了聚合物基酸体系的流变性能。在剪切速率(0 ~ 1000s -1)下,测定了活性酸和部分中和酸在pH 0 ~ 5范围内的表观粘度。还研究了盐度和温度(80 ~ 250°F)对酸体系流变性能的影响。用振荡流变仪对胶凝酸体系的粘弹性进行了评价。采用动态扫描试验来确定系统的弹性模量(G′)和粘性模量(G′)。为了研究聚合物-酸体系引起的导流性质,对印第安纳石灰岩岩心进行了单岩心驱油实验。通过对渗透率对比为1.5 ~ 20的印第安纳石灰岩岩心进行双岩心驱替实验,研究了渗透率对比对导流过程的影响。CT扫描研究了单次和双次岩心驱注酸后虫孔的扩展情况。活性酸体系表现出非牛顿剪切减薄行为,黏度随温度下降。当HCl含量为5 wt%,聚合物含量为20 gpt,温度为10 s-1时,粘度从230 cp下降到40 cp,温度从88°F上升到250°F。酸消耗测试表明,当pH值达到2时,酸生成的凝胶粘度显著提高到260 cp(250°F, 10 s-1)。高粘性凝胶堵塞了虫孔,迫使随后的酸进入下一个渗透率更高的层。凝胶的粘度持续增加,直到在pH为4.8的条件下分解到69 cp(在250°F和10 s-1下),这提供了一个自破碎系统和更好的清洁。岩心驱替研究表明,虫孔和导流过程取决于温度和流量。没有迹象表明该系统造成了任何损害。当温度从150°F升高到250°F时,注入到井眼的酸体积(PVBT)从2.2降低到1.4。由部分中和的酸体系形成的凝胶(G′= 3.976 Pa, 1 Hz)具有很强的弹性,证明了其作为转流剂的适用性。这种新型的酸-聚合物体系在酸分流中具有重要的应用前景,可以提高碳酸盐岩储层的增产效果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Novel Cationic Polymer System That Improves Acid Diversion in Heterogeneous Carbonate Reservoirs
In-situ gelled acids have been used for acid diversion in heterogeneous carbonate reservoirs for more than two decades. Most of the gelled systems are based on an anionic polymer that has a cleaning problem after the acid treatments that leads to formation damage. This work evaluates a new cationic-polymer acid system with the self-breaking ability for the application as an acid divergent in carbonate reservoirs. Experimental studies have been conducted to examine the rheological properties of the polymer-based acid systems. The apparent viscosities of the live and the partially neutralized acids at pH from 0 to 5 were measured against the shear rate (0 to 1,000 s-1). The impact of salinity and temperature (80 to 250°F) on the rheological properties of the acid system was also studied. The viscoelastic properties of the gelled acid system were evaluated using an oscillatory rheometer. Dynamic sweep tests were used to determine the elastic (G’) and viscous modulus (G") of the system. Single coreflood experiments were conducted on Indiana limestone cores to study the nature of diversion caused by the polymer-acid system. The impact of permeability contrast on the process of diversion was investigated by conducting dual coreflood experiments on Indiana limestone cores which had a permeability contrast of 1.5-20. CT scans were conducted to study the propagation of wormhole post acid injection for both single and dual corefloods. The live acid system displayed a non-Newtonian shear-thinning behavior with the viscosity declining with temperature. For 5 wt% HCl and 20 gpt polymer content at 10 s-1, the viscosity decreased from 230 to 40 cp with temperature increasing from 88 to 250°F. Acid spending tests demonstrated that the acid generated a gel with a significant improvement in viscosity to 260 cp (at 250°F and 10 s-1) after it reached a pH of 2. The highly viscous gel plugged the wormhole and forced the acid that followed to the next higher permeability zone. The viscosity of gel continued to increase until it broke down to 69 cp (at 250°F and 10 s-1) at a pH of 4.8, which provides a self-breaking system and better cleaning. Coreflood studies indicated that the wormhole and the diversion process is dependent on the temperature and the flow rate. There was no indication of any damage caused by the system. The injected acid volume to breakthrough (PVBT) decreased from 2.2 to 1.4 when the temperature increased from 150 to 250°F. The strong elastic nature of the gel (G’= 3.976 Pa at 1 Hz) formed by the partially neutralized acid system proves its suitability as a candidate for use as a diverting agent. This novel acid-polymer system has significant promise for usage in acid diversion to improve stimulation of carbonate reservoirs.
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