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{"title":"A bio-reactive transport model for biomethanation in hydrogen underground storage sites","authors":"Jean Donald Minougou, Siroos Azizmohammadi, Raoof Gholami, Holger Ott","doi":"10.1002/ghg.2307","DOIUrl":null,"url":null,"abstract":"<p>Underground biomethanation, which relies on the subsurface microbial activity to convert hydrogen and carbon dioxide into methane, is a promising approach to support carbon capture, utilization, and storage technology. The process involves injecting hydrogen with captured CO<sub>2</sub> into depleted oil and gas reservoirs or aquifers colonized by hydrogenotrophic methanogens that can convert these two substrates into methane. Despite the attractiveness of this technology, there are still uncertainties about the efficiency of the conversion process, particularly the impact of microbial parameters. To investigate the efficiency of the hydrogen conversion process, we relied on a bio-reactive transport model that can mimic microbial growth and decay, consumption of substrates, and transport of reactants and products. It was found that the methane concentration peaks near the injection well when the hydrogen fraction is in the range of 75% to 80% of the injected gas composition. In addition, a noticeable hydrogen sulfide concentration can be produced due to sulfide ions in the brine. Using the Kozeny-Carman relation, an attempt was made to correlate microbial growth with reduced porosity and permeability. It was then revealed that substrate consumption by microbes leads to a drastic increase in the microbial population in the subsurface, which can reduce the petrophysical properties of the reservoir, especially in the near wellbore area. The results obtained from a series of parametric analyses showed that the hydrogen concentration in the injected gas, pressure, well spacing, and injection rate are some of the most important parameters contributing to the biomethanation process. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.</p>","PeriodicalId":12796,"journal":{"name":"Greenhouse Gases: Science and Technology","volume":"14 6","pages":"977-994"},"PeriodicalIF":2.7000,"publicationDate":"2024-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/ghg.2307","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.2307","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
Underground biomethanation, which relies on the subsurface microbial activity to convert hydrogen and carbon dioxide into methane, is a promising approach to support carbon capture, utilization, and storage technology. The process involves injecting hydrogen with captured CO2 into depleted oil and gas reservoirs or aquifers colonized by hydrogenotrophic methanogens that can convert these two substrates into methane. Despite the attractiveness of this technology, there are still uncertainties about the efficiency of the conversion process, particularly the impact of microbial parameters. To investigate the efficiency of the hydrogen conversion process, we relied on a bio-reactive transport model that can mimic microbial growth and decay, consumption of substrates, and transport of reactants and products. It was found that the methane concentration peaks near the injection well when the hydrogen fraction is in the range of 75% to 80% of the injected gas composition. In addition, a noticeable hydrogen sulfide concentration can be produced due to sulfide ions in the brine. Using the Kozeny-Carman relation, an attempt was made to correlate microbial growth with reduced porosity and permeability. It was then revealed that substrate consumption by microbes leads to a drastic increase in the microbial population in the subsurface, which can reduce the petrophysical properties of the reservoir, especially in the near wellbore area. The results obtained from a series of parametric analyses showed that the hydrogen concentration in the injected gas, pressure, well spacing, and injection rate are some of the most important parameters contributing to the biomethanation process. © 2024 Society of Chemical Industry and John Wiley & Sons, Ltd.
地下储氢场生物甲烷化的生物反应迁移模型
地下生物甲烷化依靠地下微生物活动将氢和二氧化碳转化为甲烷,是支持碳捕获、利用和储存技术的一种很有前途的方法。该过程包括将含有捕获的二氧化碳的氢气注入枯竭的油气储层或蓄水层,这些储层或蓄水层由产氢甲烷菌组成,这些产氢甲烷菌可以将这两种基质转化为甲烷。尽管这项技术很有吸引力,但转化过程的效率仍然存在不确定性,特别是微生物参数的影响。为了研究氢转化过程的效率,我们依赖于一个生物反应传输模型,该模型可以模拟微生物的生长和衰变、底物的消耗以及反应物和产物的传输。结果表明,当氢组分占注入气组分的75% ~ 80%时,甲烷浓度在注水井附近达到峰值。此外,由于卤水中的硫化物离子,可以产生明显的硫化氢浓度。利用Kozeny-Carman关系,试图将微生物的生长与孔隙度和渗透率的降低联系起来。研究表明,微生物对基质的消耗会导致地下微生物数量急剧增加,从而降低储层的岩石物性,尤其是在近井筒区域。一系列参数分析结果表明,注入气体中的氢浓度、压力、井距和注入速率是影响生物甲烷化过程的重要参数。©2024化学工业协会和John Wiley &;儿子,有限公司
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