用高速离心机研究低盐度水对碳酸盐岩润湿性的影响

Sarah Bernardes de Almeida, A. Winter, L. Pires, O. V. Trevisan
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引用次数: 1

摘要

碳酸盐岩储层的特征是中性或油湿表面,作为二次采油方法注水可能导致采收率低。注入低盐度盐水是一种可以显著提高采收率的方法,因为它们可以促进表面润湿性的变化,使其更接近水湿状态。一些研究表明,注入盐水中存在的一些离子(Ca2+、Mg2+和SO42-)能够参与促进润湿性改变的离子交换。此外,在一些研究中,Na+和Cl-浓度的降低导致了额外的采油系数。实验室规模的采油研究通常在Amott细胞中或通过岩心驱油进行。本文提出了一种创新的方法,利用高速离心机(HSC)进行采油研究,目的是验证高速离心机作为研究润湿性变化的设备的可行性。为此,使用了6个志留纪白云岩露头岩心。对HSC进行一次排水处理,建立初始含水饱和度条件。巴西某盐下油田的地层水和油加入2%的环烷酸作为饱和流体。岩心在110°C下老化20天,以改变初始水湿状态。在HSC中进行了两组试验,研究了海水成分中Na+和Cl-离子的还原效果。使用去除Na+和Cl离子的盐水,可以观察到额外的采收率。此外,还观察了样品渗透率对采收率的影响。高浓度的Na+和Cl-离子阻碍了电位离子(Ca2+、Mg2+和SO42-)进入岩石表面,从而阻碍了润湿性改变机制。除去这些离子后,潜在离子可以更容易地到达表面,并将其润湿性改变为更亲水的状态,从而提高石油采收率。结果表明,HSC可以作为碳酸盐样品润湿性变化研究的初步仪器。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wettability Alteration in Carbonate Rocks by the Low Salinity Water using a High-Speed Centrifuge
Carbonate reservoirs are characterized by neutral or oil-wet surfaces and the injection of water as a secondary recovery method may result in low oil recovery factors. The injection of low salinity brines has shown to be a method that can lead to significant additional oil recoveries, since they promote alteration of the surface wettability towards a more water-wet condition. Several studies indicated that some ions present in the injected brine (Ca2+, Mg2+ and SO42-) are able to act in the ionic exchanges that promote the wettability alteration. Also, the decrease of the concentration of Na+ and Cl- resulted in an additional oil recovery factor in some studies. The studies of oil recovery at laboratory scale are usually performed in Amott's cells or by coreflooding. In this paper, the study of oil recovery using a high-speed centrifuge (HSC) is proposed in an innovative way with the aim to validate it as an apparatus for the study of wettability alteration. For this, six Silurian dolomite outcrop cores were used. Primary drainage process was performed on the HSC to establish the initial water saturation condition. Formation water and oil from a Brazilian pre-salt field with 2% weight of naphthenic acid were used as the saturation fluids. The cores were aged at 110 °C for 20 days to alter the initial water-wet condition. Two sets of tests were performed in the HSC to study the effects of the reduction of Na+ and Cl- ions in seawater composition. Additional oil recovery was observed using brine depleted of Na+ and Cl- ions. Besides, it was observed the influence of the sample permeability on oil recovery. The high concentration of Na+ and Cl- ions hinder the access of the potential ions (Ca2+, Mg2+ and SO42-) to the rock surface and, as consequence, hamper the wettability alteration mechanism. Removing these ions, the potential ions can reach easier to the surface and alters its wettability towards a more water-wet condition, promoting the additional oil recovery. Thus, the results showed that HSC could be used as preliminary apparatus for the wettability alteration studies in carbonate samples.
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