Hydrogen and Carbon Dioxide Kinetic Adsorption and Diffusion Behavior into Organic-Rich Shale: Implications of Mineralogy and Organic Content

IF 5.2 3区 工程技术 Q2 ENERGY & FUELS
Amer Alanazi*, Hussein Abid, Saleh A. Bawazeer, Norah Aljeban, Israa S. Abu-Mahfouz, Alireza Keshavarz, Stefan Iglauer and Hussein Hoteit, 
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Abstract

Geological storage of hydrogen (GSH) is a pivotal technology for advancing an industrial-scale hydrogen economy. Shale formations, known for their impermeable sealing and abundance, offer promising potential for secure GSH applications. However, the complex mineralogy and organic content of shale necessitate a detailed investigation. This study examines the potential of organic-rich shale samples from Jordanian oil source rocks for hydrogen (H2) storage and carbon dioxide (CO2) sequestration. Adsorption kinetics were measured at two different temperatures (303 and 333 K) and pressures (15 and 45 bar) using a volumetric experimental approach. Common mathematical models were applied to evaluate the adsorption data and calculate the diffusion coefficients. The results indicate that H2 adsorption on shale surfaces occurs at significantly lower rates than CO2, with H2 being adsorbed approximately 2–7 times less as pressure increases from 0.1 to 68 bar. Both gases show increased adsorption with rising pressure and decreased adsorption at higher temperatures. The superior adsorption capacity of CO2 highlights its potential as a cushion gas, facilitating the preferential in situ separation of H2 during extraction processes. This study also uses two distinct shale samples to explore the impact of varying total organic carbon (TOC) and calcite contents on gas adsorption capacity. The diffusion coefficients for H2 were found to be approximately 10 times higher than those for CO2, offering critical insights into the dynamics of H2 storage and retrieval in geological formations. The findings provide insights into H2 storage and retrieval in geological formations and enhance the feasibility of utilizing shale formations as reliable seals or storage media for H2.

氢和二氧化碳在富有机质页岩中的吸附和扩散动力学行为:矿物学和有机质含量的意义
地质储氢(GSH)是推进工业规模氢经济的关键技术。页岩地层以其不透水密封和储量丰富而闻名,为安全的GSH应用提供了巨大的潜力。然而,页岩复杂的矿物学和有机质含量需要进行详细的调查。本研究考察了来自约旦油源岩的富有机质页岩样品在氢气(H2)储存和二氧化碳(CO2)封存方面的潜力。采用体积实验方法测量了两种不同温度(303和333 K)和压力(15和45 bar)下的吸附动力学。采用常用的数学模型对吸附数据进行评估,并计算扩散系数。结果表明,H2在页岩表面的吸附速率明显低于CO2,当压力从0.1 bar增加到68 bar时,H2的吸附量减少约2-7倍。两种气体的吸附均随压力升高而增加,而在温度升高时吸附量减少。CO2优越的吸附能力凸显了其作为缓冲气体的潜力,促进了萃取过程中H2的优先原位分离。本研究还利用两种不同的页岩样品,探讨了总有机碳(TOC)和方解石含量对气体吸附能力的影响。研究发现,氢气的扩散系数大约是二氧化碳的10倍,这为地质构造中氢气的储存和回收动力学提供了重要的见解。这一发现为地质地层中氢气的储存和回收提供了新的思路,并提高了利用页岩地层作为可靠的密封或储存介质的可行性。
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来源期刊
Energy & Fuels
Energy & Fuels 工程技术-工程:化工
CiteScore
9.20
自引率
13.20%
发文量
1101
审稿时长
2.1 months
期刊介绍: Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.
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