巴西东北部碎屑岩油藏低矿化度注水实验研究

A. Almeida, Rajan G. Patel, Carolina Arambula, J. Soares, G. Costa, M. Embiruçu
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引用次数: 4

摘要

一些研究人员已经在实验室实验和现场应用中证明,降低注入水中盐的浓度和多价阳离子的含量可能会提高石油采收率。采用巴西东北部砂岩油藏的原油和合成地层水,对低矿化度注水(LSWI)采油效果进行了评价。采用2个长度为6 in、直径为2 in的Botucatu砂岩岩心样品进行驱心实验。使用的流体包括轻质原油样品,以及由原始地层水的四种主要盐(NaCl、KCl、CaCl2和MgCl2)生成的合成地层水(SFW)。在岩心1中,在平均储层温度为60°C的条件下进行了两次注入,一次使用20000mg /l的SFW作为二次开采模式,一次使用稀释40倍(40xd_SFW)的SFW获得5000 mg/l的低矿化度水作为三次开采模式。在Core 2中,在相同温度下注入40xd_SFW,比较二次模式下的高、低矿化度水效应。此外,在6种稀释的SFW和去离子水中,对Botucatu砂岩粉末进行了zeta (ζ)电位测量。实验结果表明,在二次和三次注入40xd_SFW时,原油采收率和pH值均有所提高。岩芯1的流出离子浓度表明,在高温水浸过程中,Ca2+被还原,表明其在岩石表面被吸附。最显著的是,在第一次注入LSWI孔体积时,流出样品中Ca2+浓度升高,Na+浓度降低,表明岩石表面钙离子交换为钠离子。此外,出水中还观察到Fe2+/Fe3+和微量Al3+,表明SFW和40xd_SFW中发生了细迁移。boucatu砂岩上负ζ电位的大小随着盐水溶液盐度的降低而增大。在此基础上,我们注意到在Botucatu砂岩和Recôncavo盆地的油盐样品中同时存在一套LSWI机制,这表明LSWI在巴西类似油藏中具有应用潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Low Salinity Water Injection in a Clastic Reservoir in Northeast Brazil: An Experimental Case Study
Several researchers have demonstrated in laboratory experiments and field applications that reducing the concentration of salts and the content of multivalent cations in the injection water may increase oil recovery. This study evaluates the performance of low salinity water injection (LSWI) in oil recovery using a crude oil and synthetic formation water of a sandstone reservoir in northeast Brazil. Two Botucatu sandstone core samples of 6 in of length and 2 in of diameter were used for the coreflooding experiments. The fluids used included a light crude oil sample, and synthetic formation water (SFW) produced from the four main salts of the original formation water (NaCl, KCl, CaCl2, and MgCl2). In Core 1, two injections were carried out at an average reservoir temperature of 60 °C, one using SFW with 200,000 mg/l as secondary recovery mode, and one using SFW diluted 40 times (40xd_SFW) resulting in a low salinity water of 5,000 mg/l as tertiary recovery mode. In Core 2, 40xd_SFW was injected at the same temperature to compare the high and low salinity water effects in the secondary mode. Moreover, zeta (ζ) potential measurements on Botucatu sandstone powder were performed in 6 dilutions of the SFW and deionized water. The experimental results demonstrated an increase in oil recovery and pH when 40xd_SFW was injected in secondary and tertiary modes. The effluent ionic concentration from Core 1 showed the reduction of Ca2+ during HSWI, indicating its adsorption on the rock surface. Most remarkably, Ca2+ concentration increases and the Na+ concentration decreases in the effluent samples in the first LSWI pore volume injected, which suggested ionic exchange of calcium for sodium on the rock surface. Furthermore, Fe2+/Fe3+ and traces of Al3+ were observed in the effluent demonstrating the occurrence of fine migration in SFW and 40xd_SFW. The magnitude of negative ζ potential on Botucatu sandstone increases as the salinity of the brine solutions decreases. Based on that experimental study, it is noticed that a set of LSWI mechanisms occurr simultaneously in Botucatu sandstone, and oil and brine samples from Recôncavo Basin, indicating a potential of application for LSWI in similar Brazilian oil reservoirs.
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