咸水层地下储氢与储碳多尺度数值模拟

Numerical Simulation of Carbon Dioxide and Hydrogen Storage in Saline Aquifers

  • 摘要: 地下储氢和CO2地质封存已成为化石能源行业转型的热点领域。在微观上,通过建立孔隙网络两相模拟方法,表征了非润湿相的滞后效应,研究了H2和CO2在咸水层中的两相渗流特征和异同。据此开展了H2和CO2注入咸水层以及H2回采矿场尺度数值模拟,评估了气体储存量、储存安全性和回采率。结果表明:由于H2难以被压缩,CO2地下储集能力优于H2;由于润湿性的影响,CO2储存时发生泄漏的可能性大于H2。此外,优化设计了CO2作为垫气时的注入量,形成了H2回采率Pareto图版。该研究成果为咸水层地下储氢与碳封存技术的理论研究和工程应用提供了科学指导。

     

    Abstract: Underground hydrogen storage (UHS) and carbon dioxide capture and storage (CCS) have been the frontiers of energy transition of petroleum and coal industries. A pore-scale network simulation method incorporating non-wetting phase hysteresis effects has been developed to study the flow characteristics of hydrogen and carbon dioxide in saline aquifers. Field-scale numerical simulations of hydrogen and carbon dioxide injection, as well as hydrogen recovery, were conducted to evaluate gas storage capacity, storage safety, and recovery efficiency. The results indicate that carbon dioxide has a higher likelihood of leakage compared to hydrogen during storage. When the storage capacity of the reservoir is limited, carbon dioxide storage is more advantageous than hydrogen. Pre-injecting carbon dioxide as buffer gas can effectively enhance hydrogen recovery efficiency, where the Pareto digram for optimal hydrogen storage efficiency is provided. This research outcome offers scientific guidance for both theoretical studies and engineering practices of hydrogen storage and carbon sequestration in saline formations.

     

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