Modeling CO2 Sequestration in Deep Saline Aquifers – Best Practices

Hassan Alzayer, Tareq Zahrani, A. Shubbar
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引用次数: 1

Abstract

Managing carbon emissions has become a major responsibility for the oil and gas industry in a drive to ensure sustainable energy and create a clean environment. Therefore, governments, research centers, IOC’s and NOC’s are actively adopting new guidelines and inventing new technologies to safely circulate carbons. In this paper, the process of modeling CO2 sequestration in a deep saline aquifer will be discussed. Carbon dioxide can be safely stored indefinitely in subsurface geological formations by four trapping mechanisms; structural, residual, soluble, and mineral trapping. These four trapping mechanisms can take hundreds or thousands of years to happen. Furthermore, the oil and gas industry standard recommend that any technology used to store CO2 needs to demonstrate a storage capacity of 1000 years with less than 0.1 per-cent leakage potential per year. Therefore, modelling such process should capture any existing trapping mechanism, even if it happens after several hundreds of years, to ensure long-term secure storage of the CO2. Using our in-house simulator "GigaPOWERS", many sequestration scenarios were conducted to come up with a recommended guideline to maximize the volume of CO2 trapped in deep saline aquifers. This study used a giant synthetic anticline model with a variation in geological properties. The residual and soluble trapping mechanisms were captured through relative permeability hysteresis and extended water PVT tables respectively. Injecting CO2 into water aquifers is a dynamic process where drainage and imbibition cycles are likely to happen. Such processes cause the CO2 to be trapped in the middle of the pores as an immobile phase, which can be a favorable phenomenon maximizing the security of CO2 sequestration. Since CO2 is soluble in water, when it contacts the water phase it will form a carbonated water that is denser than water itself and migrates downward in a phenomenon known as "CO2 fingering". The CO2 solubility in water depends mainly on the salinity and temperature which both need to be accurately captured in the simulation model. Depending on the long-term objective of the sequestration project, the development strategy can be altered to maximize the outcome using the detailed simulation model. In this paper, the simulation best practices for modeling CO2 sequestration for maximum secure long-term storage (1000+ years) are suggested. Carbon dioxide, CO2, sequestration in deep saline aquifers is a well-known method to reduce carbon emissions. However, there is very little published literature on the simulation best practices for modeling the CO2 sequestration process. Therefore, this paper will be a pioneer to guide the industry for accurate simulation of such process.
模拟深层盐水含水层的二氧化碳封存-最佳实践
在确保能源可持续发展和创造清洁环境的过程中,管理碳排放已成为油气行业的一项主要责任。因此,各国政府、研究中心、国际奥委会和国家石油公司都在积极采用新的指导方针和发明新的技术来安全循环碳。本文将讨论深层含盐含水层中CO2封存的模拟过程。通过四种捕集机制,二氧化碳可以安全地无限期地储存在地下地质构造中;结构、残留、可溶性和矿物捕获。这四种捕获机制可能需要数百年或数千年才能发生。此外,石油和天然气行业标准建议,任何用于储存二氧化碳的技术都需要证明其储存能力为1000年,每年泄漏的可能性低于0.1%。因此,模拟这一过程应该捕捉到任何现有的捕获机制,即使它发生在几百年后,以确保二氧化碳的长期安全储存。使用我们的内部模拟器“GigaPOWERS”,进行了许多封存方案,以提出建议的指导方针,以最大限度地提高深盐水含水层中捕获的二氧化碳量。本研究使用了一个地质性质变化的巨型合成背斜模型。通过相对渗透率滞后和扩展水PVT表分别捕获了残余和可溶性捕获机制。向含水层注入二氧化碳是一个动态过程,可能发生排水和吸胀循环。这些过程使CO2作为不流动相被困在孔隙中间,这是一个有利的现象,最大限度地提高了CO2封存的安全性。由于二氧化碳可溶于水,当它与水相接触时,会形成比水本身密度大的碳酸水,并向下迁移,这种现象被称为“二氧化碳指动”。CO2在水中的溶解度主要取决于盐度和温度,这两者都需要在模拟模型中准确捕获。根据封存项目的长期目标,可以改变开发策略,以使用详细的模拟模型使结果最大化。在本文中,提出了模拟二氧化碳最大安全长期储存(1000年以上)的最佳实践。在深层咸水层中封存二氧化碳是一种众所周知的减少碳排放的方法。然而,关于模拟CO2封存过程的最佳实践的已发表文献很少。因此,本文将成为指导行业对这一过程进行精确模拟的先驱。
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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