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{"title":"Numerical simulation of CO2 geological sequestration and CO2-ECBM in coal beds of Longtan Formation, Xiangzhong Depression, Hunan Province, China","authors":"Mingjun Zou, Zibin Ding, Yiyi Cheng, Linlin Yao, Yue Sun, Keying Wang","doi":"10.1002/ghg.2296","DOIUrl":null,"url":null,"abstract":"<p>Geological sequestration of carbon dioxide (CO<sub>2</sub>) is an effective method to reduce greenhouse gases and an important technology for carbon neutralization. Among all geological sequestration sites, coal reservoirs are potentially effective and practicable. The Xiangzhong Depression of Hunan Province of China is selected as the research area, and the coal seam of Longtan Formation is the target reservoir in this paper. CO<sub>2</sub>-enhanced coalbed methane (CO<sub>2</sub>-ECBM) and CO<sub>2</sub> sequestration capacity are both simulated according to the laboratory experiments on reservoir parameters. During simulation, four production wells and one injection well were designed, and the simulation process can be divided into two stages: CO<sub>2</sub>-ECBM and CO<sub>2</sub> geological storage. The CO<sub>2</sub>-ECBM stage refers to CO<sub>2</sub> injection for increasing methane production, and the CO<sub>2</sub> geological storage stage aims to predict the CO<sub>2</sub> sequestration capacity. After that, sensitivity analyses of sequestration effect are carried out. During the simulation, when maintaining a constant pressure injection of CO<sub>2</sub> under the original conditions of 0.01 mD permeability, 9% porosity, and 1.47 MPa reservoir methane pressure, the total storage amount is only 0.14 × 10<sup>6</sup> m<sup>3</sup>. However, the storage amount increases significantly to 6.62 × 10<sup>6</sup> m<sup>3</sup> if the permeability increases to 1.5 mD. Orthogonal simulation indicates that permeability has the greatest impact on CO<sub>2</sub> sequestration. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.</p>","PeriodicalId":12796,"journal":{"name":"Greenhouse Gases: Science and Technology","volume":"14 5","pages":"743-759"},"PeriodicalIF":2.7000,"publicationDate":"2024-08-10","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.2296","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
Geological sequestration of carbon dioxide (CO2 ) is an effective method to reduce greenhouse gases and an important technology for carbon neutralization. Among all geological sequestration sites, coal reservoirs are potentially effective and practicable. The Xiangzhong Depression of Hunan Province of China is selected as the research area, and the coal seam of Longtan Formation is the target reservoir in this paper. CO2 -enhanced coalbed methane (CO2 -ECBM) and CO2 sequestration capacity are both simulated according to the laboratory experiments on reservoir parameters. During simulation, four production wells and one injection well were designed, and the simulation process can be divided into two stages: CO2 -ECBM and CO2 geological storage. The CO2 -ECBM stage refers to CO2 injection for increasing methane production, and the CO2 geological storage stage aims to predict the CO2 sequestration capacity. After that, sensitivity analyses of sequestration effect are carried out. During the simulation, when maintaining a constant pressure injection of CO2 under the original conditions of 0.01 mD permeability, 9% porosity, and 1.47 MPa reservoir methane pressure, the total storage amount is only 0.14 × 106 m3 . However, the storage amount increases significantly to 6.62 × 106 m3 if the permeability increases to 1.5 mD. Orthogonal simulation indicates that permeability has the greatest impact on CO2 sequestration. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.
中国湖南省湘中凹陷龙潭地层煤层二氧化碳地质封存和二氧化碳-ECBM数值模拟
二氧化碳(CO2)的地质封存是减少温室气体的有效方法,也是碳中和的一项重要技术。在所有地质封存地点中,煤炭储层具有潜在的有效性和可行性。本文选择中国湖南省湘中坳陷为研究区域,以龙潭地层煤层为目标储层。根据储层参数的实验室实验,模拟了二氧化碳强化煤层气(CO2-ECBM)和二氧化碳封存能力。在模拟过程中,设计了四口生产井和一口注入井,模拟过程可分为两个阶段:CO2-ECBM 和 CO2 地质封存两个阶段。CO2-ECBM 阶段指的是注入 CO2 以增加甲烷产量,而 CO2 地质封存阶段旨在预测 CO2 封存能力。然后,对封存效果进行敏感性分析。在模拟过程中,在渗透率 0.01 mD、孔隙度 9%、储层甲烷压力 1.47 MPa 的原始条件下,保持恒压注入 CO2 时,总封存量仅为 0.14 × 106 m3。然而,如果渗透率增加到 1.5 mD,储量就会大幅增加到 6.62 × 106 m3。正交模拟表明,渗透率对二氧化碳封存的影响最大。© 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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