H2, CH4 and CO2 adsorption on Cameo coal: Insights into the role of cushion gas in hydrogen geological storage

被引:21
|
作者
Li, Xiaoqiang [1 ]
Sun, Xun [1 ]
Walters, Clifford C. [1 ]
Zhang, Tongwei [1 ]
机构
[1] Univ Texas Austin, Bur Econ Geol, Austin, TX 78713 USA
关键词
Energy transition; Hydrogen underground storage; Competitive adsorption; Hydrogen loss; HIGH-PRESSURE CH4; CARBON-DIOXIDE; METHANE ADSORPTION; SORPTION ISOTHERMS; ACTIVATED CARBONS; PORE STRUCTURE; SHALE; EMBRITTLEMENT; OPPORTUNITIES; EXPLORATION;
D O I
10.1016/j.ijhydene.2023.08.185
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Large-scale hydrogen underground storage is widely considered as an important solution for energy transition to mitigate global warming, however, our understanding on the various chemical and physical processes leading to H-2 loss during geo-storage remains largely unknown. We conducted adsorption isotherms measurements of H-2, CH4 and CO2 on Cretaceous Cameo coal at 35, 50 and 65 degrees C, to explore adsorption mechanisms of H-2 and deciphering the effect of cushion gas (e.g., CH4, CO2) on H-2 loss in the subsurface. The adsorbed amounts of H-2 are just 12% and 6% of CH4 and CO2 at temperature of 35 degrees C and pressure of 2.3 MPa, respectively, and H-2 adsorption behavior on Cameo coal can be described well by Langmuir monolayer theory. The extremely high Langmuir pressures (35-49 MPa) for H-2 indicate very weak affinity with coal, compared to CH4 and CO2. Differences of Langmuir adsorption capacities suggest that the gas adsorption of H-2 and CH4 are mainly by physical interactions while both physical and chemical bonding with coal structures occurs for CO2. The affinity with solid materials for the three gases can be quantitatively evaluated by the heat of adsorption, which was determined to be similar to 9.2 kJ/mol for H-2. Extrapolation of our experimental results to natural coal seams indicates that H-2 presents much smaller adsorption amounts at depth up to 2000 m, corresponding to temperatures lower than 65 degrees C and pressure less than 30 MPa, geological conditions that are suitable for hydrogen underground storage. This study confirms that the injection of CH4 or CO2 as cushion gas can largely reduce the H-2 loss by adsorption in the subsurface. Empirical calculation suggests H-2 adsorption will be insignificant with chemical composition of CH4 above 8% or CO2 above 2% at the storage sites (e.g., abandoned mines, depleted coal seams). Our study lays a foundation on the understanding of the risk of H-2 loss in large-scale hydrogen underground storage. (c) 2023 Hydrogen Energy Publications LLC. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:879 / 892
页数:14
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