Dissolution Behavior of Carbonate Rocks from Brazilian Pre-Salt at Reservoir Conditions by LSWI

T. Borges, J. V. Vargas, E. Koroishi, Nilo Kim, O. V. Trevisan, G. S. Bassani
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Abstract

The low salinity water injection (LSWI) is one of the most studied techniques applied to enhanced oil recovery (EOR) from carbonates reservoirs. Wettability alteration and dissolution reaction are mechanisms that support the understanding of this technique. However, the dissolution behavior of Brazilian pre-salt carbonates rocks when treated by LSWI is not yet known. Therefore, the purpose of this work is to evaluate the dissolution effects provided by low salinity water injection in carbonate rocks from a Brazilian pre-salt reservoir using two different injection flow rates in core flooding tests at reservoir conditions. Porosity variation along the length was determined by Computerized Tomography scan analysis. Permeability was determined through pressure drop data. Ions identification and concentration were determined by ions chromatography. The experiments consisted in carrying out two core flooding tests assembled in series at 8100 psi of injection pressure and 65°C. It was performed two different injection flow rates (1 mL/min and 0.1 mL/min) of 16 times diluted synthetic seawater. It was possible to observe three different porosity behaviors along the sample length in both flow rates tested and for both core holder samples. However, the porosity behavior intensity is different from each case. There are regions of predictable behavior, regions of random behavior and inert regions. According to the porosity plots, the sample from the second core holder of the series presented more interaction with the injection fluid. Probably, the mineralogical heterogeneity has influenced in the dissolution phenomenon. The permeability profile remained almost constant for both samples. The ion chromatography analysis revealed a huge variation of magnesium and calcium ions concentration in the first injected porous volume and, subsequently, a constant trend towards the base-line values.
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巴西盐下碳酸盐岩储层溶蚀行为的LSWI研究
低矿化度注水技术(LSWI)是碳酸盐岩油藏提高采收率(EOR)研究最多的技术之一。润湿性改变和溶解反应是支持该技术理解的机制。然而,巴西盐下碳酸盐岩在LSWI作用下的溶解行为尚不清楚。因此,本研究的目的是在储层条件下的岩心驱油试验中,利用两种不同的注入流速,评估低矿化度注水对巴西盐下储层碳酸盐岩的溶解效果。通过计算机断层扫描分析确定孔隙度沿长度的变化。渗透率通过压降数据确定。离子色谱法测定离子的鉴别和浓度。实验包括在注入压力为8100 psi、温度为65°C的条件下进行两次岩心注水试验。在16倍稀释的合成海水中进行两种不同的注射流速(1 mL/min和0.1 mL/min)。在测试的两种流速和两种岩心支架样品中,沿样品长度可以观察到三种不同的孔隙度行为。然而,每种情况下孔隙度行为强度是不同的。有可预测行为的区域,随机行为的区域和惰性区域。从孔隙度图来看,该系列第2个岩心支架的样品与注入流体的相互作用更大。可能是矿物学的非均质性影响了溶蚀现象。两种样品的渗透率曲线几乎保持不变。离子色谱分析显示,在第一次注入的多孔体积中,镁离子和钙离子浓度发生了巨大的变化,随后,镁离子和钙离子浓度趋于基线值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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