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A New Organic Acid to Stimulate Deep Wells in Carbonate Reservoirs

机译:一种可刺激碳酸盐岩储层深井的新型有机酸

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摘要

Carbonate acidizing has been carried out using HCl-based stimulation fluids for decades. However, at high temperatures, HCl does not produce acceptable results because of its fast reaction, acid penetration, and hence surface dissolution, and its high corrosion rate. As a result, alternatives to HCl have been investigated including organic acids. In this work, the reaction of a new organic acid with calcite was investigated using the rotating disk apparatus and coreflood setup. The organic acid was obtained using both a phosphorous-based and iron-based catalyst.The rate of reaction of a 10 wt% solution of the new organic acid was measured using the rotating disk apparatus at temperatures up to 250?F. Low-permeability Indiana limestone (1-5 md) samples of 1.5 in. diameter and 0.75 in. length were used. The effect of disk rotational speed (100-1,500 rpm) was investigated. Samples of the reacted fluid were collected periodically and calcium and iron concentrations were measured using Inductively-Coupled Plasma, and used to determine the acid-rock reaction rate and to study the possibility of precipitation. Also, coreflood experiments at different injection rates and a temperature of 300?F were performed to study the effect of the acid onwormhole propagation in calcite. Low-permeability Indiana limestone (1-10 md) cores used in these experiments have a diameter of 1.5-in. and a length of 6 in.For the phosphorus-based acid, experimental results showed that the rate of calcite dissolution at 205?F was controlled only by the rate of mass transfer of the acid to the surface. However, at 250?F, the reaction was controlled by both mass transfer and by the kinetics of the surface reaction. At 205?F, the reaction rate varied from 7.79E-07 to 4.47E-06 gmol/cm^(2).s, while at 250?F, the range was between 5.82E-07 and 2.72E-06 gmol/cm^(2).s. In coreflood experiments, the phosphorus-based acid caused calcium phosphate precipitation at 300?F, while the iron-based acid achieved breakthrough. Also, the optimum injection rate of the iron-based acid was determined to be 2.0 cm^(3)/min. This study summarizes the results obtained and recommends the use of the new organic acid for field applications in calcite reservoirs.
机译:碳酸盐酸化已经使用基于HCl的增产液进行了数十年。但是,在高温下,HCl不能产生令人满意的结果,这是因为它的快速反应,酸渗透,表面溶解以及高腐蚀速率。结果,已经研究了HCl的替代物,包括有机酸。在这项工作中,使用转盘设备和岩心驱替装置研究了一种新的有机酸与方解石的反应。用磷基和铁基催化剂均可得到有机酸。用转盘装置在最高250?F的温度下测定10%(重量)新有机酸溶液的反应速率。使用了直径为1.5英寸,长度为0.75英寸的低渗透印第安纳州石灰石(1-5 md)样品。研究了磁盘转速(100-1,500 rpm)的影响。定期收集反应液的样品,并使用感应耦合等离子体测量钙和铁的浓度,并用于确定酸岩反应速率并研究沉淀的可能性。另外,在不同的注入速率和300?F的温度下进行了岩心驱替实验,以研究酸对方解石中虫孔扩散的影响。这些实验中使用的低渗透印第安纳州石灰石岩心(1-10 md)的直径为1.5英寸。长度为6英寸的磷基酸的实验结果表明,在205?F下方解石的溶解速率仅受酸向表面的质量转移速率控制。但是,在250?F时,反应既受传质又受表面反应动力学控制。在205?F下,反应速率从7.79E-07到4.47E-06 gmol / cm ^(2).s,而在250?F下,反应范围在5.82E-07和2.72E-06 gmol / cm ^ / s之间。厘米^(2).s。在岩心驱油实验中,磷基酸在300?F时引起磷酸钙沉淀,而铁基酸则取得了突破。而且,铁基酸的最佳注入速率被确定为2.0cm 2(3)/ min。这项研究总结了获得的结果,并建议在方解石储层的现场应用中使用新的有机酸。

著录项

  • 作者

    Al-Douri, Ahmad F;

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  • 年度 2015
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  • 原文格式 PDF
  • 正文语种 en
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