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{"title":"Reciprocal cross-correlation analysis of two-phase seepage processes and reservoir heterogeneities in CO2 saline aquifer sequestration","authors":"Yiyan Zhong, Qi Li, Liang Xu, Yiping Wen, Yukun Li","doi":"10.1002/ghg.2268","DOIUrl":null,"url":null,"abstract":"<p>When CO<sub>2</sub> saline aquifer storage is carried out, the heterogeneity of reservoir rock is an important factor affecting CO<sub>2</sub> transport, and the reservoir heterogeneity in numerical simulations is mainly manifested as the heterogeneity of the parameter field. Since the parameter distributions across the reservoir are not available with the existing probes, the stochastic finite element method is combined with a two-phase flow model to establish an unconditional random field of permeability, and computations are performed using the Monte Carlo method. The permeability, CO<sub>2</sub> maximum migration distance (<i>M<sub>d</sub></i>) and CO<sub>2</sub> sweep area (<i>S<sub>a</sub></i>) were analyzed for mutual correlation. The permeability correlation area affecting <i>M<sub>d</sub></i> and <i>S<sub>a</sub></i> was obtained, and the changes in the correlation area under the coefficient of variation (<i>C<sub>v</sub></i>) and correlation length (<i>λ<sub>x</sub></i>) of the permeability field in the different reservoirs were analyzed. The kriging superposition approach (KSA) was subsequently used to estimate both the <i>M<sub>d</sub></i> and <i>S<sub>a</sub></i> of the target reservoir by establishing conditional random fields based on the sampling parameters in regions with different correlations, resulting in errors of 0.66% for <i>M<sub>d</sub></i> and 0.96% for <i>S<sub>a</sub></i> in the high correlation region and 4.86% and 3.12% for <i>M<sub>d</sub></i> and <i>S<sub>a</sub></i> in the low correlation region, which suggested that the sampling results from the high correlation region were less biased in the estimation. Under limited sampling conditions, it is recommended that samples be collected in regions with high correlations to reduce the uncertainty of CO<sub>2</sub> transport analysis due to unknown heterogeneity. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.</p>","PeriodicalId":12796,"journal":{"name":"Greenhouse Gases: Science and Technology","volume":"14 3","pages":"356-370"},"PeriodicalIF":2.7000,"publicationDate":"2024-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Greenhouse Gases: Science and Technology","FirstCategoryId":"93","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/ghg.2268","RegionNum":4,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
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Abstract
When CO2 saline aquifer storage is carried out, the heterogeneity of reservoir rock is an important factor affecting CO2 transport, and the reservoir heterogeneity in numerical simulations is mainly manifested as the heterogeneity of the parameter field. Since the parameter distributions across the reservoir are not available with the existing probes, the stochastic finite element method is combined with a two-phase flow model to establish an unconditional random field of permeability, and computations are performed using the Monte Carlo method. The permeability, CO2 maximum migration distance (Md ) and CO2 sweep area (Sa ) were analyzed for mutual correlation. The permeability correlation area affecting Md and Sa was obtained, and the changes in the correlation area under the coefficient of variation (Cv ) and correlation length (λx ) of the permeability field in the different reservoirs were analyzed. The kriging superposition approach (KSA) was subsequently used to estimate both the Md and Sa of the target reservoir by establishing conditional random fields based on the sampling parameters in regions with different correlations, resulting in errors of 0.66% for Md and 0.96% for Sa in the high correlation region and 4.86% and 3.12% for Md and Sa in the low correlation region, which suggested that the sampling results from the high correlation region were less biased in the estimation. Under limited sampling conditions, it is recommended that samples be collected in regions with high correlations to reduce the uncertainty of CO2 transport analysis due to unknown heterogeneity. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.
二氧化碳含盐含水层封存中两相渗流过程和储层异质性的互为交叉相关分析
在进行二氧化碳含盐含水层封存时,储层岩石的异质性是影响二氧化碳输运的重要因素,数值模拟中的储层异质性主要表现为参数场的异质性。由于现有探井无法获得整个储层的参数分布,因此将随机有限元法与两相流模型相结合,建立无条件的渗透率随机场,并采用蒙特卡罗法进行计算。分析了渗透率、二氧化碳最大迁移距离(Md)和二氧化碳扫描面积(Sa)之间的相互关系。得到了影响 Md 和 Sa 的渗透率相关面积,并分析了不同储层渗透率场变异系数(Cv)和相关长度(λx)下相关面积的变化。随后采用克里金叠加法(KSA),根据不同相关性区域的取样参数建立条件随机场,估算目标储层的Md和Sa,结果高相关性区域的Md和Sa误差分别为0.66%和0.96%,低相关性区域的Md和Sa误差分别为4.86%和3.12%,说明高相关性区域的取样结果在估算中偏差较小。在有限的采样条件下,建议在相关性高的区域采集样品,以减少未知异质性对二氧化碳迁移分析的不确定性。© 2024 化学工业协会和约翰-威利父子有限公司版权所有。
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