EGU25-6528, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-6528
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 16:15–16:25 (CEST)
 
Room -2.31
Preliminary Laboratory Studies on Hydrogen Storage in a Salt Cavern of the Eocene Barbastro Formation, Southern Pyrenees, Spain
Timea Kovács1, José Mediato1, Berta Ordóñez1, Nuria Garcia2, Emilio Pueyo1, José Sanchez Guzman3, Jesús Gracia3, and Edgar Berrezueta1
Timea Kovács et al.
  • 1Instituto Geológico y Minero de España, Spain (t.kovacs@igme.es)
  • 2Centro Nacional del Hidrógeno, Spain
  • 3Salmueras Depuradas S.L., Spain

The transition to a greener economy requires scalable, reliable, and efficient energy storage solutions. Hydrogen (H2), a key component of future renewable energy systems, must be stored in gigaton-scale quantities to balance supply and demand globally. Underground hydrogen storage (UHS) in salt rock caverns is emerging as the most promising solution due to the exceptional properties of rock salt (halite), such as low permeability, self-healing capacity, and geochemical stability. However, significant scientific and technological challenges remain, requiring further study to ensure the safe and efficient deployment of this technology (Berrezueta et al., 2024).

Among these challenges, the geomechanical and geochemical evolution of rock salt during cyclic H2 injection and extraction requires further knowledge to address potential integrity problems of the reservoir. Key uncertainties arise from the complex interplay of heterogeneous mineralogy, variable brine compositions, and the dynamic temperature and pressure conditions within the reservoir. Addressing these uncertainties begins with the development of a robust laboratory testing protocol to simulate and analyze the interaction of hydrogen within rock salt under reservoir-like conditions.

This study presents experimental data from an autoclave setup designed to replicate reservoir conditions of pressure and temperature. Samples of the Eocene Barbastro Fm. (Southern Pyrenees) were obtained from a deep borehole drilled in a salt structure considered for hydrogen storage. The experiments using pure halite samples and halite with various impurities provide insights into the reactivity of non-halite phases and their impact on the properties of the rock salt. The findings contribute to addressing critical knowledge gaps and improving the safety and reliability of underground hydrogen storage in salt caverns. By advancing our understanding of the processes governing UHS in salt formations, this research supports the development of robust, science-based solutions for the global energy transition.

This work is funded by the Project UES365 of the Convocatoria Misiones-CDTI (Spain).

References:

Berrezueta, E.; Kovács, T.; Herrera-Franco, G.; Caicedo-Potosí, J.; Jaya-Montalvo, M.; Ordóñez-Casado, B.; Carrión-Mero, P.; Carneiro, J. Laboratory Studies on Underground H2 Storage: Bibliometric Analysis and Review of Current Knowledge. Appl. Sci. 2024, 14, 11286. https://doi.org/10.3390/app142311286

How to cite: Kovács, T., Mediato, J., Ordóñez, B., Garcia, N., Pueyo, E., Sanchez Guzman, J., Gracia, J., and Berrezueta, E.: Preliminary Laboratory Studies on Hydrogen Storage in a Salt Cavern of the Eocene Barbastro Formation, Southern Pyrenees, Spain, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-6528, https://doi.org/10.5194/egusphere-egu25-6528, 2025.