The Effect of Wettability on Waterflood Remaining Oil Saturation and Endpoint Relative Permeabilities in Carbonate and Sandstone Rocks

IF 2.7 3区 工程技术 Q3 ENGINEERING, CHEMICAL
Ramzi Ali, Yanbin Gong, Amir H. Alizadeh, Mohammad Piri
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引用次数: 0

Abstract

We systematically examine how wettability governs waterflood remaining oil saturation and endpoint relative permeabilities in carbonate and sandstone rocks using capillary-dominated coreflooding experiments. Water-wet and mixed-wet conditions (intermediate- and strongly oil-wet) are imposed by chemical aging of core plugs and validated by contact-angle measurements. Each experiment comprises primary oil drainage to establish the initial water saturation, an optional aging step, and subsequent waterflooding with 20–25 pore volumes (PV) of brine. In carbonate plugs, endpoint oil relative permeability is highest under water-wet conditions and decreases as oil-wetness increases. Across all wettability conditions, samples with larger average pore sizes exhibit higher endpoint oil relative permeability. Water-wet carbonates reach a recovery plateau after 1–2 PV, whereas intermediate- and oil-wet systems continue to recover oil over substantially larger injected volumes. Consistent with trends widely reported for sandstones, the carbonate cores achieve maximum recovery at near-intermediate wettability over the 20–25 PV window studied. We further infer that strongly oil-wet plugs may ultimately attain the lowest remaining oil saturations at much larger injected volumes due to persistent, hydraulically conductive oil layers, although this lies beyond the PV range tested. Endpoint water relative permeability increases as wettability shifts away from water-wet conditions; under water-wet states, it increases slightly as average pore size decreases. Sandstone experiments corroborate prior observations that near-neutral wettability yields the highest recovery after 20–25 PV of brine injection.

润湿性对碳酸盐岩和砂岩水驱剩余油饱和度和端点相对渗透率的影响
我们系统地研究了润湿性如何影响碳酸盐岩和砂岩的水驱剩余油饱和度和端点相对渗透率。水湿和混合湿条件(中度和强烈油湿)是由岩心桥塞的化学老化造成的,并通过接触角测量进行验证。每个实验包括一次排油以确定初始含水饱和度,一个可选的老化步骤,随后用20-25孔隙体积(PV)的盐水进行水驱。在碳酸盐岩桥塞中,终端油相对渗透率在水湿条件下最高,随着油湿程度的增加而降低。在所有润湿性条件下,平均孔径较大的样品表现出较高的端点油相对渗透率。水湿型碳酸盐岩在1-2 PV后达到采收率平台,而中间和油湿型体系在更大的注入量下继续采油。与广泛报道的砂岩趋势一致,在研究的20-25 PV窗口内,碳酸盐岩心在接近中等润湿性时实现了最大采收率。我们进一步推断,由于持续存在的水力导电性油层,强油湿桥塞最终可能在更大的注入量下获得最低的剩余油饱和度,尽管这超出了PV测试范围。随着润湿性从水-湿状态转移,端点水相对渗透率增加;在水-湿状态下,随着平均孔径的减小,平均孔径略有增大。砂岩实验证实了先前的观察结果,即在注水20-25 PV后,接近中性润湿性的采收率最高。
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来源期刊
Transport in Porous Media
Transport in Porous Media 工程技术-工程:化工
CiteScore
5.30
自引率
7.40%
发文量
155
审稿时长
4.2 months
期刊介绍: -Publishes original research on physical, chemical, and biological aspects of transport in porous media- Papers on porous media research may originate in various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering)- Emphasizes theory, (numerical) modelling, laboratory work, and non-routine applications- Publishes work of a fundamental nature, of interest to a wide readership, that provides novel insight into porous media processes- Expanded in 2007 from 12 to 15 issues per year. Transport in Porous Media publishes original research on physical and chemical aspects of transport phenomena in rigid and deformable porous media. These phenomena, occurring in single and multiphase flow in porous domains, can be governed by extensive quantities such as mass of a fluid phase, mass of component of a phase, momentum, or energy. Moreover, porous medium deformations can be induced by the transport phenomena, by chemical and electro-chemical activities such as swelling, or by external loading through forces and displacements. These porous media phenomena may be studied by researchers from various areas of physics, chemistry, biology, natural or materials science, and engineering (chemical, civil, agricultural, petroleum, environmental, electrical, and mechanical engineering).
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