Experimental and molecular dynamic simulation assessment of H2/brine/cement interfacial interactions during underground hydrogen storage

Cement is widely used as a structural and sealing material to ensure hydrogen containment in geological formations. However, the influence of H 2 –brine–cement wettability and H 2 –brine interfacial tension (IFT) on the integrity and sealing efficiency of cemented caprocks remains poorly understood. Furthermore, previous studies provide limited insights into hydrogen adsorption and sorption behavior under subsurface storage conditions. In this study, wettability and IFT of H 2 –brine–cement systems were experimentally measured at pressures of 500–1000 psi and temperatures of 25–50 °C to evaluate hydrogen migration, trapping, and the performance of cemented seals. Molecular dynamics simulations were conducted at pressures of 500–3000 psi and temperatures of 25–100 °C to quantify hydrogen adsorption on cement surfaces and sorption within cement pores. The results show that variations in H 2 –brine IFT did not exceed 6 mN/m, while maximum contact angles remained below 70°, indicating a predominantly water-wet system favouring residual hydrogen trapping in brine-saturated pores . Molecular simulations revealed hydrogen adsorption energies of −0.2 kcal/mol to −7.84 kcal/mol, consistent with moderate physisorption dominated by dispersive interactions, and sorption energies of 3.07 to 29.24 kcal/mol, indicating that hydrogen can be temporarily retained within pore networks, with retention strength increasing at low temperatures and high pressures. These findings suggest that the cement matrix maintains its chemical and structural stability, and that hydrogen migration is governed primarily by the physical microstructure rather than chemical interactions, supporting the effectiveness of cemented barriers for underground hydrogen storage. • Wettability of H 2 -brine-cement systems and H 2 -brine IFT were studied. • MD simulations were conducted to quantify H 2 adsorption and sorption energies. • Change in H 2 -brine IFT did not exceed 6 mN/m and contact angles were less than 70°. • H 2 adsorption energies of −0.2 to −7.84 kcal/mol indicates very weak physisorption. • Sorption energies of 3.07 to 29.24 kcal/mol suggested moderate H 2 retention within cement pores.

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Publication Details

Journal
Geoenergy Science and Engineering
Published
2026-04-27
DOI
https://doi.org/10.1016/j.geoen.2026.214529
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
0.00

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article

Experimental and molecular dynamic simulation assessment of H2/brine/cement interfacial interactions during underground hydrogen storage

Surajudeen Sikiru, Ahmed Zarzor Al-Yaseri, Berihun Mamo Negash, Nurudeen Yekeen
Geoenergy Science and Engineering
CO2 Sequestration and Geologic Interactions
article

Experimental and molecular dynamic simulation assessment of H2/brine/cement interfacial interactions during underground hydrogen storage

Surajudeen Sikiru, Ahmed Zarzor Al-Yaseri, Berihun Mamo Negash, Nurudeen Yekeen
article en

Abstract

Cement is widely used as a structural and sealing material to ensure hydrogen containment in geological formations. However, the influence of H 2 –brine–cement wettability and H 2 –brine interfacial tension (IFT) on the integrity and sealing efficiency of cemented caprocks remains poorly understood. Furthermore, previous studies provide limited insights into hydrogen adsorption and sorption behavior under subsurface storage conditions. In this study, wettability and IFT of H 2 –brine–cement systems were experimentally measured at pressures of 500–1000 psi and temperatures of 25–50 °C to evaluate hydrogen migration, trapping, and the performance of cemented seals. Molecular dynamics simulations were conducted at pressures of 500–3000 psi and temperatures of 25–100 °C to quantify hydrogen adsorption on cement surfaces and sorption within cement pores. The results show that variations in H 2 –brine IFT did not exceed 6 mN/m, while maximum contact angles remained below 70°, indicating a predominantly water-wet system favouring residual hydrogen trapping in brine-saturated pores . Molecular simulations revealed hydrogen adsorption energies of −0.2 kcal/mol to −7.84 kcal/mol, consistent with moderate physisorption dominated by dispersive interactions, and sorption energies of 3.07 to 29.24 kcal/mol, indicating that hydrogen can be temporarily retained within pore networks, with retention strength increasing at low temperatures and high pressures. These findings suggest that the cement matrix maintains its chemical and structural stability, and that hydrogen migration is governed primarily by the physical microstructure rather than chemical interactions, supporting the effectiveness of cemented barriers for underground hydrogen storage. • Wettability of H 2 -brine-cement systems and H 2 -brine IFT were studied. • MD simulations were conducted to quantify H 2 adsorption and sorption energies. • Change in H 2 -brine IFT did not exceed 6 mN/m and contact angles were less than 70°. • H 2 adsorption energies of −0.2 to −7.84 kcal/mol indicates very weak physisorption. • Sorption energies of 3.07 to 29.24 kcal/mol suggested moderate H 2 retention within cement pores.

Geoenergy Science and EngineeringVol. 263
Edith Cowan University (AU), King Fahd University of Petroleum and Minerals (SA), Universiti Teknologi Petronas (MY), Universiti Teknologi MARA (MY)
King Fahd University of Petroleum and Minerals
Openalex Percentile: Top 15%
CO2 Sequestration and Geologic Interactions
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