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Reservoir simulation of CO_2 sequestration pilot in Frio brine formation, USA Gulf Coast

机译:美国墨西哥湾沿岸Frio盐水层中CO_2封存试点的油藏模拟

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Reservoir simulation studies were performed to investigate compositional effects between aquifer fluid (brine) and injected supercritical CO_2 during the sequestration process in the Frio brine formation. Accurate data calibrations of CO_2 solubility and density, as well as brine density and viscosity, were performed. Hysteresis relative permeability was taken into consideration to account for the effect of trapped gas in the aquifer. In addition, real aquifer data obtained from the test site were used in order to characterize the Frio aquifer. The Frio Brine Storage Project is a study in USA that was conducted by the Bureau of Economic Geology (BEG) at the University of Texas at Austin as a pilot to investigate the CO_2 sequestration process in an aquifer as the first closely monitored case study. The objective of monitoring this pilot study, which was conducted by a collaboration of several research organizations including BEG, Lawrence Berkley National Laboratory (LBNL), Sandia Technologies LLC, US Geological Survey (USGS), and Schlumberger, and funded by the DOE's National Energy Technology Laboratory (NETL), was to observe the behavior of supercritical CO_2 in the subsurface, investigate the physics of the process, and obtain data for further validation of simulation results. This simulation study was carried out before the pilot began, and the results were verified against the early results of the field experiment. Different scenarios were simulated to investigate the lateral and vertical spread of the CO_2 plume in the aquifer. Local grid refinement around both injection and monitoring wells helped to obtain accurate results. According to our studies, at the end of the simulation period (10 years from the injection date), a significant part of the injected CO_2 will be in the form of trapped gas or will be dissolved in the aqueous phase. Considering the proposed injection plan, and since only a small portion of the injected CO_2 will be in the form of free gas, the possibility of CO_2 escape through the shale cap rock will be very low.
机译:进行了储层模拟研究,以研究在Frio盐水形成过程中螯合过程中含水层流体(盐水)和注入的超临界CO_2之间的组成效应。进行了CO_2溶解度和密度以及盐水密度和粘度的准确数据校准。考虑了滞后相对渗透率,以考虑含水层中截留气体的影响。此外,还使用从测试地点获得的真实含水层数据来表征Frio含水层。 Frio盐水储存项目是由美国德克萨斯州奥斯汀大学经济地质局(BEG)进行的一项美国研究,作为研究第一个受到密切监视的案例研究的含水层中CO_2固存过程的试点。监视这项试验研究的目的是由美国能源部国家能源基金资助的几个研究组织的合作,包括BEG,劳伦斯·伯克利国家实验室(LBNL),桑迪亚技术有限责任公司,美国地质调查局(USGS)和斯伦贝谢技术实验室(NETL)旨在观察地下超临界CO_2的行为,研究过程的物理过程,并获取数据以进一步验证模拟结果。该模拟研究是在飞行员开始之前进行的,其结果已与现场实验的早期结果进行了验证。模拟了不同的情景,以研究含水层中CO_2羽流的横向和垂直扩散。围绕注入井和监测井进行局部网格优化有助于获得准确的结果。根据我们的研究,在模拟期结束时(从注入日期算起的10年),注入的CO_2的很大一部分将以捕集的气体形式或溶解在水相中。考虑到拟议的注入计划,由于注入的CO_2中只有一小部分为游离气体,因此CO_2通过页岩盖岩逸出的可能性非常小。

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