首页> 外文会议>SPE International Symposium and Exhibition on Formation Damage Control >Matrix Acid Systems for Formations With High Clay Content
【24h】

Matrix Acid Systems for Formations With High Clay Content

机译:具有高粘土含量的形成基质酸系统

获取原文

摘要

There are a number of sandstone reservoirs in which more than 50% of the matrix is composed of clay and feldspar minerals. Typically, these reservoirs are subject to fines migration and respond poorly to conventional matrix acid stimulation treatments. There are numerous challenges when treating these formations: the removal and/or stabilization of the mobile fines in the pore spaces without destabilizing the clays in the matrix or the matrix itself; the need to stimulate the formation some distance away from the wellbore, and, equally importantly, to minimize reaction products precipitating in the matrix; and the very low critical velocities that can lead to plugging while injecting the treatment. In many conventional acid treatments, after an initially good response to the treatment, the production falls to levels similar to or lower than before the treatment. A common compromise is to empirically adjust the strength of a HF/HCl acid system used to treat a particular formation, so as to delay the onset of renewed fines migration after the treatment for as long as possible, at the expense of optimizing productivity. In many cases this results in making the treatments uneconomic. To meet theses challenges a new fluoroboric acid system has been developed. The basic chemistry used is similar to that of a retarded HF acid previously described in the literature as clay acid (Thomas and Crowe 1978).. However, unlike the retarded HF acid, the new fluid uses organic acid as a chelant and is effectively a blend of organic/fluoroboric acid and hence an organic clay acid. The fluoroboric acid is generated by the addition of hydrofluoric and boric acid. By adjusting the initial concentration and ratio of hydrofluoric and boric acid, it is possible to optimize the stimulation effect of the treatment in a particular formation and prevent future fines migration. A key is the initial concentration of free hydrofluoric acid and the available hydrofluoric acid from hydrolysis of the fluoroboric acid with respect to the clay mineralogy and temperature. The concentration of the organic acid, the chelant, is also adjusted based on an analysis of the effluent during core flow testing, to minimize precipitation. Prior to customizing the organic clay acid system, treatments were performed in low temperature (< 140°F) reservoirs, with 30% kaolinite along with zeolite and chlorite present in the formation matrix. While there was a noted stimulation effect and fines stabilization, the initial post-treatment productivity fell short of that seen using an organic mud acid. In the case of organic mud acid, however, the production declined rapidly, indicating renewed fines migration. This led to a reformulation of the organic clay acid for use as the main treating fluid, eliminating the need for HF preflushes. The initial productivity of wells treated using the reformulated organic clay acid were higher than that obtained using an organic mud acid and remained stable, indicating effective fines migration control. In contrast to what might be expected it has been observed during the testing that it is not always the "weakest" treating fluids that are the least damaging, especially in formations with low critical velocities. There is an apparent balance between the tendency for a fluid to move fines in the matrix and to dissolve them, with very low dissolution rates increasing the probability of plugging the formation. Since 2003, more than 120 successful treatments have been performed using a customized organic clay acid as the main treating fluid to stimulate a variety of reservoirs previously considered untreatable or difficult to treat. The temperature of these reservoirs ranges from as low as 105°F to as high as 250°F, and the clay/feldspar content in the matrix often exceeded 40%. The treatments were greatly helped by the use of a geochemical simulator with which to optimize the acid formulations, with respect to both clay content and temperature.
机译:有许多在该基体的50%以上是由粘土和长石矿物的砂岩储层。典型地,这些容器是受到罚款迁移和响应很差到常规基质酸增产处理。有治疗这些地层当许多挑战:在孔隙空间,而不在基质或基质本身不稳定粘土移动细粒的去除和/或稳定化;需要从井眼刺激形成一定距离,而且,同样重要的是,为了最小化反应产物在基质中沉淀;和极低的临界速度,可导致堵塞,同时注入的治疗。在许多传统的酸处理,给治疗初始良好响应后,产量下降到相似或比处理前降低的水平。一个常见的折衷方法是凭经验调整用于治疗的特定形成HF /盐酸酸系统的强度,以便延迟重新细粒运移发作处理后,只要有可能,在最优化生产率为代价。在许多情况下,这会导致使治疗不经济的。为了满足论文挑战新的氟硼酸系统已经研制成功。所使用的基础化学是类似于先前在文献中粘土酸(托马斯和Crowe 1978)中描述的延迟的HF酸的。然而,不同于延迟HF酸,新流体用途有机酸作为螯合剂和是一个有效混合有机/氟硼酸,因此有机粘土酸。的氟硼酸通过加入氢氟酸和硼酸的生成。通过调整初始浓度和氢氟酸和硼酸的比例,所以能够优化治疗的刺激作用在特定的形成和预防未来的细粒运移。一个关键是游离氢氟酸的初始浓度,并从氟硼酸的水解可用氢氟酸相对于所述粘土矿物学和温度。有机酸,螯合剂的浓度,基于核心流动测试期间的流出物的分析也被调整,以最小化沉淀。之前定制有机粘土酸体系,治疗是在低温与沸石和绿泥石存在于地层基质一起执行(<140°F)贮存器,用30%的高岭石。虽然有一个指出刺激效应和细粒稳定,初始治疗后生产率短的,使用的有机土酸看出下跌。在有机土酸的情况下,然而,产量迅速下降,说明更新细粒运移。这导致了有机粘土酸中的用途为主要处理流体进行改写,消除了对HF preflushes的需要。使用重新有机粘土酸处理的孔的初始生产率明显低于使用有机土酸和保持稳定获得更高,这表明有效的细粒迁移控制。相比之下什么可以预料它的测试,它并不总是“最弱”的处理液是最少的破坏,特别是在低临界速度地层中被观察到。有倾向之间的表观平衡用于流体移动细粒在基质中,并溶解它们,具有非常低的溶解速率增加堵塞形成的概率。自2003年以来,已经使用一个自定义的有机粘土的酸为主要处理流体,以刺激各种以前认为无法治疗的或难以治疗储层进行超过120次成功的治疗。这些水库范围从低至105°F到温度高达250°F,并在基质中的粘土/长石含量往往超过40%。所述治疗是大大通过使用地球化学模拟器与优化酸制剂,相对于二者的粘土含量和温度的帮助。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号