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Underground hydrogen storage (UHS) is one way of industrial-scale storage of hydrogen in geologic porous media for withdrawal on demand. The withdrawal of hydrogen from these repositories requires replacement gas (called cushion gas) to maintain pressure. CO2 and methane are two possible cushion gases. How does the presence of these gases impact the behavior of hydrogen at molecular scale? What role do the pore characteristics like surface area, tortuosity and pore connectivity play in this? We try to address these questions in this paper.

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This page is a summary of: Adsorption of hydrogen, methane, CO 2 and their binary mixtures in silicalite-1: role of pore characteristics revealed by molecular simulations, RSC Advances, January 2025, Royal Society of Chemistry,
DOI: 10.1039/d5ra06520h.
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