Hydrogen Storage Law and Nanoscale Occurrence Mechanism of Anthracite Containing Depleted CH<sub>4</sub>: Insights from Experiment and Molecular Simulation

Hydrogen energy is pivotal for driving sustainable development and achieving deep decarbonization; yet, its storage remains a significant challenge. Notably, depleted methane reservoirs can serve as a promising large-scale solution for underground hydrogen storage (UHS). Based on adsorption experiments, Monte Carlo and molecular dynamics methods, the adsorption behavior of H<sub>2</sub> and CH<sub>4</sub> in anthracite and the applicability of five models were discussed. The occurrence space and competitive adsorption law of H<sub>2</sub> and residual CH<sub>4</sub> in anthracite were analyzed, and the H<sub>2</sub> storage law and nanoscale occurrence mechanism of anthracite were revealed to evaluate the feasibility of high-pressure H<sub>2</sub> storage in depleted CH<sub>4</sub> reservoirs. The results show that the H<sub>2</sub> isotherm exhibited a linear trend. The Langmuir model can accurately describe H<sub>2</sub> adsorption, and the temperature inhibits H<sub>2</sub> uptake. Both D-A and Freundlich models are also capable of precisely fitting CH<sub>4</sub> and H<sub>2</sub> adsorption, while the BET model shows the poorest performance. The adsorption difference between CH<sub>4</sub> and H<sub>2</sub> narrows under a high pressure. The isosteric heat of adsorption for H<sub>2</sub> is lower than that of CH<sub>4</sub>, and the depleted reservoir's low methane pressure exhibits minimal impact on high-pressure H<sub>2</sub> adsorption. When the H<sub>2</sub> molar fraction reaches 0.9, its adsorption capacity exceeds that of CH<sub>4</sub>, with this difference amplifying under increasing partial pressure, which highlight the potential of high-pressure H<sub>2</sub> storage in CH<sub>4</sub>-depleted reservoirs. Radial distribution function and coordination number analyses reveal that CH<sub>4</sub> exhibits a denser distribution around coal molecules compared to H<sub>2</sub>. However, H<sub>2</sub> demonstrates a diffusion coefficient 1 order of magnitude higher than that of CH<sub>4</sub>, facilitating rapid hydrogen storage. Furthermore, H<sub>2</sub> occupies approximately 70% and 30% of the adsorbed and free spaces in coal, respectively, compared to 90% and 10% for CH<sub>4</sub>. This study is expected to provide scientific guidance for H<sub>2</sub> energy storage in depleted coal seams.

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Journal
Langmuir
Published
2025-09-09
DOI
https://doi.org/10.1021/acs.langmuir.5c02464
Primary Topic
Coal Properties and Utilization
Type
article
Field-Weighted Citation Impact
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Hydrogen Storage Law and Nanoscale Occurrence Mechanism of Anthracite Containing Depleted CH4: Insights from Experiment and Molecular Simulation

Baisheng Nie, Chunhui Lv, Shuhao Zhang, Zhifeng Chen et al.
Langmuir
Coal Properties and Utilization
article

Hydrogen Storage Law and Nanoscale Occurrence Mechanism of Anthracite Containing Depleted CH4: Insights from Experiment and Molecular Simulation

Baisheng Nie, Chunhui Lv, Shuhao Zhang, Zhifeng Chen, Xiaowei Li, Xiangchun Li, Haonan Song
article en

Abstract

Hydrogen energy is pivotal for driving sustainable development and achieving deep decarbonization; yet, its storage remains a significant challenge. Notably, depleted methane reservoirs can serve as a promising large-scale solution for underground hydrogen storage (UHS). Based on adsorption experiments, Monte Carlo and molecular dynamics methods, the adsorption behavior of H<sub>2</sub> and CH<sub>4</sub> in anthracite and the applicability of five models were discussed. The occurrence space and competitive adsorption law of H<sub>2</sub> and residual CH<sub>4</sub> in anthracite were analyzed, and the H<sub>2</sub> storage law and nanoscale occurrence mechanism of anthracite were revealed to evaluate the feasibility of high-pressure H<sub>2</sub> storage in depleted CH<sub>4</sub> reservoirs. The results show that the H<sub>2</sub> isotherm exhibited a linear trend. The Langmuir model can accurately describe H<sub>2</sub> adsorption, and the temperature inhibits H<sub>2</sub> uptake. Both D-A and Freundlich models are also capable of precisely fitting CH<sub>4</sub> and H<sub>2</sub> adsorption, while the BET model shows the poorest performance. The adsorption difference between CH<sub>4</sub> and H<sub>2</sub> narrows under a high pressure. The isosteric heat of adsorption for H<sub>2</sub> is lower than that of CH<sub>4</sub>, and the depleted reservoir's low methane pressure exhibits minimal impact on high-pressure H<sub>2</sub> adsorption. When the H<sub>2</sub> molar fraction reaches 0.9, its adsorption capacity exceeds that of CH<sub>4</sub>, with this difference amplifying under increasing partial pressure, which highlight the potential of high-pressure H<sub>2</sub> storage in CH<sub>4</sub>-depleted reservoirs. Radial distribution function and coordination number analyses reveal that CH<sub>4</sub> exhibits a denser distribution around coal molecules compared to H<sub>2</sub>. However, H<sub>2</sub> demonstrates a diffusion coefficient 1 order of magnitude higher than that of CH<sub>4</sub>, facilitating rapid hydrogen storage. Furthermore, H<sub>2</sub> occupies approximately 70% and 30% of the adsorbed and free spaces in coal, respectively, compared to 90% and 10% for CH<sub>4</sub>. This study is expected to provide scientific guidance for H<sub>2</sub> energy storage in depleted coal seams.

LangmuirVol. 41(37)
Chongqing University (CN), China University of Mining and Technology (CN), Institute of Disaster Prevention (CN), Xinjiang Institute of Engineering (CN)
Openalex Percentile: Top 70%
Coal Properties and Utilization
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