在裂缝性碳酸盐岩中探索低ift泡沫EOR:低于10 md石灰岩的成功和特殊挑战

Pengfei Dong, M. Puerto, Guoqing Jian, Kun Ma, K. Mateen, G. Ren, G. Bourdarot, D. Morel, S. Biswal, G. Hirasaki
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引用次数: 14

摘要

天然裂缝性石灰岩储层的地层非均质性高,需要流动性控制剂来提高波及效率和提高采收率。然而,典型的流动性控制剂,如聚合物和凝胶,由于潜在的堵塞问题,在低于10- md的致密地层中是不切实际的。本研究的目的是证明裂缝性低渗透石灰岩储层低界面张力(low-IFT)泡沫过程的可行性,并研究相关的地球化学相互作用。通过岩心驱油实验,研究了基质渗透率低于10- md的均质和裂缝性油湿岩心的低ift泡沫过程。比较了低ift泡沫配方和著名的标准泡沫(AOS C14-16)在采油效率方面的性能。测量了流出物的离子浓度,以了解石灰石的地球化学性质如何影响低ift泡沫过程。为了解释岩心驱替实验中观察到的结果,对破碎的岩心材料和含有不同二价离子浓度的盐水进行了水稳定性和相行为测试。在基质渗透率低于10- md的裂缝性油湿石灰岩油藏中,低ift泡沫工艺可以实现显著的原油采收率增量。与水驱相比,在渗透率为5 md的裂缝性油湿石灰岩岩心中进行低ift泡沫驱,采收率提高了64%。在这一过程中,由于表面活性剂溶液的毛细管进入压力明显低于气体,泡沫主要将表面活性剂溶液从裂缝转移到基质中。这种选择性导流效应导致表面活性剂或弱泡沫在致密基质中产生,从而改善了侵入流体在基质中的流动。同时,泡沫配方的低ift特性调动了基质中的剩余油。与缺乏低ift特性的配方相比,低ift配方的油动员效果在波及区获得了更低的剩余油饱和度。与白云岩储层相比,灰岩地球化学的不稳定性给灰岩储层的低ift泡沫过程带来了额外的挑战。方解石与注入流体的反应,如矿物溶解和钙、镁的交换,被发现增加了产出流体中的Ca2+浓度。由于低ift泡沫过程对盐水盐度敏感,额外的Ca2+可能导致潜在的表面活性剂沉淀和不利的过优条件。因此,它可能导致注入性和相圈闭问题,特别是在均质石灰岩中。研究结果表明,尽管存在石灰石溶解带来的挑战,但在基质渗透率低至5md的裂缝性油湿性致密储层中,低ift泡沫工艺可以显著提高化学提高采收率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Exploring Low-IFT Foam EOR in Fractured Carbonates: Success and Particular Challenges of Sub-10-mD Limestone
The high formation heterogeneity in naturally fractured limestone reservoirs requires mobility control agents to improve sweep efficiency and boost oil recovery. However, typical mobility control agents, such as polymers and gels, are impractical in tight sub-10-mD formations due to potential plugging issues. The objective of this study is to demonstrate the feasibility of a low-interfacial-tension (low-IFT) foam process in fractured low-permeability limestone reservoirs and to investigate relevant geochemical interactions. The low-IFT foam process was investigated through core flooding experiments in homogenous and fractured oil-wet cores with sub-10-mD matrix permeability. The performance of a low-IFT foaming formulation and a well-known standard foamer (AOS C14-16) were compared in terms of the efficiency of oil recovery. The effluent ionic concentrations were measured to understand how the geochemical properties of limestone influenced the low-IFT foam process. Aqueous stability and phase behavior tests with crushed core materials and brines containing various divalent ion concentrations were conducted to interpret the observations in the core flooding experiments. Low-IFT foam process can achieve significant incremental oil recovery in fractured oil-wet limestone reservoirs with sub-10-mD matrix permeability. Low-IFT foam flooding in a fractured oil-wet limestone core with 5-mD matrix permeability achieved 64% incremental oil recovery compared to water flooding. In this process, because of the significantly lower capillary entry pressure for surfactant solution compared to gas, foam primarily diverted surfactant solution from the fracture into the matrix. This selective diversion effect resulted in surfactant or weak foam flooding in the tight matrix and hence improved the invading fluids flow in it. Meanwhile, the low-IFT property of the foaming formulation mobilized the remaining oil in the matrix. This oil mobilization effect of low-IFT formulation achieved lower remaining oil saturation in the swept zones compared with the formulation lacking low-IFT property with oil. The limestone geochemical instability caused additional challenges for the low-IFT foam process in limestone reservoirs compared to dolomite reservoirs. The reactions of calcite with injected fluids, such as mineral dissolution and the exchange of Calcium and Magnesium, were found to increase the Ca2+ concentration in the produced fluids. Because the low-IFT foam process is sensitive to brine salinity, the additional Ca2+ may cause potential surfactant precipitation and unfavorable over-optimum conditions. It therefore may cause injectivity and phase trapping issues especially in the homogenous limestone. Results in this work demonstrated that despite the challenges associated with limestone dissolution, a low-IFT foam process can remarkably extend chemical EOR in fractured oil-wet tight reservoirs with matrix permeability as low as 5 mD.
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