Clay-hydrogen and clay-cushion gas interfacial tensions: Implications for hydrogen storage. (22nd May 2022)

• Record Type: Journal Article
• Authors: Yekeen, Nurudeen; Al-Yaseri, Ahmed; Negash, Berihun Mamo; Ali, Muhammad; Giwelli, Ausama; Esteban, Lionel; Sarout, Joel
• Is Part Of: International journal of hydrogen energy. Volume 47:Number 44(2022)
• Page Start: 19155
• Page End: 19167
• Publication Date: 2022-05-22
• Subjects: Clay-gas interfacal tension -- Clay minerals -- Hydrogen -- Carbon dioxide -- Underground hydrogen storage; Hydrogen as fuel -- Periodicals; Hydrogène (Combustible) -- Périodiques; Hydrogen as fuel; Periodicals; 665.81
• DOI: 10.1016/j.ijhydene.2022.04.103
• Languages: English
• ISSNs: 0360-3199

Abstract

Abstract: Rock/fluid interfacial tension ( γ rock − f l u i d ) govern the fluid flow dynamics, the injection/withdrawal rates, the gas storage capacity, and containment integrity during gas (H2, CO2, N2 ) geo-storage. Clay-gas interfacial tension ( γ clay − g a s ) data, especially for the clay-H2 ( γ clay − H 2 ), the clay-N2 ( γ clay − N 2 ) and the clay-CO2 ( γ clay − C O 2 ) systems, have rarely been reported in the literature due to the challenging nature of these measurements in the laboratory. In this study, Neumann's equation of state and Young-Laplace equation was combined to compute clay-gas and clay-brine interfacial tensions (IFT) parameters at realistic geo-storage temperature (333 K) and pressure (5–20 MPa). Our results show that at similar thermodynamic conditions: γ clay − H 2 > γ clay − N 2 > γ clay − C O 2 . Our calculations also showed that: γ kaolinite − N 2 > γ illite − N 2 > γ montmorillonite − N 2, and γ kaolinite − C O 2 > γ illite − C O 2 > γ montmorillonite − C O 2 . In contrast, for hydrogen a negligible difference in γ clay − H 2 was obtained for the three clay types, although, the IFT between clay minerals and brine in presence of hydrogen is different for these three clay types. Overall, computed γ clay − H 2 values were higher than γ clay − N 2 and γ clay − C O 2 values, whereas computed clay-brine interfacial tension was lower in presence of hydrogen compared to carbon dioxide and nitrogen. These results suggest that nitrogen and carbon dioxide could be used as favorable cushion gas for maintaining formation pressure during underground hydrogen storage. We also demonstrated a remarkable relationship between clay/gas IFT and gas density that could serve as a helpful tool for quick estimation of rock-fluid interfacial tension. Highlights: Clay gas interfacial tensions ( γ c l a y − gas ) were predicted for hydrogen and cushion gases. ( γ c l a y − gas ) follows the order γ c l a y − H 2 > γ c l a y − N 2 > γ c l a y − C O 2 . γ c l a y − H 2 and γ c l a y − C O 2 follow the order γ k a o l i n i t e − g a s > γ i l l i t e − g a s > γ m o n t m o r i l o n i t e − g a s . There was a negligible difference in γ c l a y − H 2 for kaolinite, illite and montmorillonite. Remarkable relationship exists between clay/gas IFT and gas (H2, CO2, N2 ) density.