控制盐度水驱过程中岩石-水和油水界面相互作用的认识

A. Belhaj, N. Singh, H. Sarma
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引用次数: 3

摘要

多年来,实验室研究和有限数量的现场试验表明,采用控制盐度的水驱可以提高石油采收率。注入盐水成分是一种很有前途的技术,可以通过改变电位决定离子(pdi)的浓度来改变碳酸盐岩的润湿性,特别是Ca2+, Mg2+和SO42 -离子。本文对岩石-水和油水界面的岩石-流体和流体-流体相互作用进行了全面的实验研究。研究的第一步是使用旋滴式张力仪测量界面张力(IFT),并研究油水相互作用的动态行为。然后使用专门设计的zeta电位计测量碳酸盐岩样品的zeta电位,该zeta电位计能够利用整个岩心塞,而不是粉碎的样品。采用流动电位技术测量了zeta电位,并在不同改性盐水组成和岩石饱和度条件下进行了实验。随后,使用专门设计的高压高温(HP/HT)池进行润湿性改变实验。IFT测量结果显示,随着盐度的降低,岩石-水相互作用比油水相互作用更占优势。zeta电位实验结果表明,随着海水逐渐稀释至1%dSW,由于双电层的膨胀,zeta电位有明显的负值增加的趋势。另一方面,当卤水成分改变时,pdi (Ca2+和Mg2+)的增加对zeta电位的影响不如SO42−离子的影响大。在润湿性蚀变实验中,稀释盐水和成分改性盐水都产生了更高的吸胀率,与使用海水的实验相比,总产油量更高。此外,从接触角的测量结果可以推断,岩石表面的润湿性变化更倾向于水湿条件。润湿性蚀变试验前后的zeta电位测量表明,实验结束后,zeta电位的负值有所减小,表明岩石有排油作用。非饱和岩石和含盐含油饱和岩石的zeta电位测量进一步验证了这一点。本研究的结果将有助于更好地理解控制盐度水驱过程中岩石-流体和流体-流体相互作用,这将有利于该领域的未来研究。
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Understanding the Interactions at Rock-Water and Oil-Water Interfaces during Controlled-Salinity Water Flooding
Over the years, laboratory studies and a limited number of field trials have demonstrated the potential of enhancing oil recovery using controlled-salinity water flooding. The injected brine composition is one of the promising techniques that could alter the wettability of carbonate rocks by changing the concentration of the potential determining ions (PDIs), specifically Ca2+, Mg2+, and SO42− ions. In this study, a comprehensive experimental study was conducted to investigate the rock-fluid and fluid-fluid interactions at rock-water and oil-water interfaces. The first step of the study was to measure the interfacial tension (IFT) using the spinning-drop tensiometer and study the dynamic behavior of the oil-water interactions. The zeta potential of carbonate rock samples was then measured using a specially-designed zeta potentiometer capable of utilizing the whole core plug, rather than the pulverized samples. The streaming potential technique was used for the zeta potential measurements and the experiments were conducted under different modified brine composition and rock saturation conditions. Subsequently, wettability alteration experiments were conducted using a specially designed high-pressure high-temperature (HP/HT) cell. The IFT measurements showed an increasing trend as salinity decreases, clarifying that rock-water interactions are more dominant over oil-water interactions. Results of the zeta potential experiments showed a clear trend of yielding more negative values as the seawater gradually diluted down to 1%dSW, due to the expansion of the electrical double layer. On the other hand, when the brine composition was modified, the increase of the PDIs (Ca2+ and Mg2+) did not have as much impact on zeta potential as the SO42− ions. In the wettability alteration experiments, both diluted and composition-modified brine generated a higher imbibition rate, resulting in a higher total oil production when compared with the experiments using the seawater. Furthermore, the wettability alteration of the rock surface trended more towards water-wetness conditions, as inferred from the contact angle measurements. The measurement of zeta potential before and after wettability alteration tests showed that the zeta potential value became less negative after the experiment, which suggested the expulsion of oil from the rock. This was further verified by the measurements of zeta potential for the unsaturated rock and saturated rock with brine and oil. The findings from this study would provide a better understanding of the rock-fluid and fluid-fluid interactions during controlled-salinity water flooding, which will benefit future studies in this area.
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