Carbonated Water Injection Effects on Lacustrine Carbonates of Mupe Member, Lower Purbeck Group (Upper Jurassic), United Kingdom

IF 2.1 4区 工程技术 Q3 ENERGY & FUELS
Isabela D. de Albuquerque, S. L. B. Bermúdez, G. C. Stael, C. Rabe, C. Harper
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Abstract

This paper describes the study of dissolution and mineralogical alteration caused by saline carbonated water injection (CWI) and its effects on the petrophysical properties (porosity and permeability) of limestone samples from the Mupe Member, composed of lacustrine microbialites from the Upper Jurassic, part of the Purbeck Group lower portion. These limestones are a partial analog of the Brazilian presalt Aptian carbonates, the most important oil reservoir in Brazil. These reservoirs present large amounts of CO2 that are reinjected into the formation, which given the high reactivity of carbonate rocks in the presence of carbonic acid generated by the reaction between CO2 and water, can cause damage to the rock’s pore space. To achieve the proposed objectives, four laminated/massive samples with very low permeability (<5 md) and two vuggy/microbial samples with very high permeability (>1,700 md) underwent laboratory tests carried out before, during, and after CWI, including gas porosity and permeability measurement, nuclear magnetic resonance (NMR), microcomputed tomography (micro-CT), and ion chromatography. X-ray diffraction (XRD) analysis and petrographic thin-section observations were also performed. The experimental results showed that samples with high permeability showed a small decrease in permeability, possibly indicating formation damage, while low-permeability samples presented a significant increase in permeability with little change in porosity, indicating feasibility for carbon capture and storage (CCS) in similar samples in likewise experimental conditions (20°C and 500 psi). For samples with more pore volumes injected, the pressure stabilization seems to have favored dissolution in the later injection stages, indicated by the highest output of calcium ions. In all samples occurred salt precipitation during injection, especially in the more heterogeneous rocks, presenting a possible issue.
碳酸水注入对英国上侏罗统下Purbeck组Mupe段湖相碳酸盐岩的影响
本文研究了含盐碳酸水注入(CWI)引起的溶蚀和矿物学蚀变及其对上侏罗统Purbeck组下段湖相微生物岩组成的Mupe段石灰岩样品岩石物性(孔隙度和渗透率)的影响。这些石灰岩部分类似于巴西最重要的储层——阿普提亚盐下碳酸盐岩。这些储层中含有大量的二氧化碳,这些二氧化碳被重新注入地层中,由于碳酸盐岩在二氧化碳与水反应产生的碳酸中具有很高的反应性,这可能会对岩石的孔隙空间造成破坏。为了实现所提出的目标,在CWI之前、期间和之后对4个渗透率极低(1,700 md)的层压/大块样品进行了实验室测试,包括气体孔隙度和渗透率测量、核磁共振(NMR)、微计算机断层扫描(micro-CT)和离子色谱。并进行了x射线衍射(XRD)分析和岩石薄片观察。实验结果表明,高渗透率样品的渗透率下降幅度较小,可能表明地层受到了破坏,而低渗透率样品的渗透率明显增加,孔隙度变化不大,表明在类似的实验条件下(20°C和500 psi),在类似的样品中进行碳捕集与封存(CCS)是可行的。对于注入孔隙体积较大的样品,压力稳定似乎有利于后期注入阶段的溶解,表现为钙离子的最高输出。所有样品在注入过程中都发生了盐沉淀,特别是在非均质岩石中,这可能是一个问题。
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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来源期刊
CiteScore
5.30
自引率
0.00%
发文量
68
审稿时长
12 months
期刊介绍: Covers the application of a wide range of topics, including reservoir characterization, geology and geophysics, core analysis, well logging, well testing, reservoir management, enhanced oil recovery, fluid mechanics, performance prediction, reservoir simulation, digital energy, uncertainty/risk assessment, information management, resource and reserve evaluation, portfolio/asset management, project valuation, and petroleum economics.
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