Abstract
Salt caverns are promising sites for hydrogen (H₂) storage, but microbial activity in these high-salinity environments poses risks, including H₂ consumption and subsequent toxic hydrogen-sulfide (H₂S) production by sulphate-reducing bacteria. While salinity influences microbial diversity, the role of chaotropicity, defined as a membrane-disrupting effect of salts like magnesium chloride (MgCl2) and calcium chloride (CaCl2), remains unexplored. We introduce a novel method using oscillatory rheology to measure solute-induced changes in agar gel point temperature, enabling prediction of chaotropicity and subsequent microbial activity. We assessed individual salts, salt mixtures, literature data, and original brine samples from four salt caverns. Our results show that chaotropic conditions arise when the ionic strength (I) of solution exceeds 3 mol/L with 55% MgCl₂, or 6 mol/L with 40% MgCl₂. One tested cavern exhibited chaotropic properties, suggesting reduced microbial risk. Microbial analysis and growth tests confirmed missing microbial activity and minimal cell numbers in the chaotropic cavern, in contrast to the more kosmotropic caverns. Therefore, we propose a strategy to mitigate microbial threats by adjusting salt cavern brine composition to induce chaotropicity as one additional factor to limit activity, which offers a new framework for microbial risk management.
Data availability
The authors declare that the data supporting the findings of this study are available within the paper and its supplementary information files.
References
Böttcher, N., Görke, U. J., Kolditz, O. & Nagel, T. Thermo-mechanical investigation of salt caverns for short-term hydrogen storage. Environ. Earth Sci. 76, 98. https://doi.org/10.1007/s12665-017-6414-2 (2017).
Dopffel, N. et al. Microbial hydrogen consumption leads to a significant pH increase under high-saline-conditions: implications for hydrogen storage in salt caverns. Sci. Rep. 13, 10564. https://doi.org/10.1038/s41598-023-37630-y (2023).
Ramesh Kumar, K., Honorio, H., Chandra, D., Lesueur, M. & Hajibeygi, H. Comprehensive review of geomechanics of underground hydrogen storage in depleted reservoirs and salt caverns. J. Energy Storage. 73, 108912. https://doi.org/10.1016/j.est.2023.108912 (2023).
Osman, A. I. et al. Hydrogen production, storage, utilisation and environmental impacts: a review. Environ. Chem. Lett. 20, 153–188. https://doi.org/10.1007/s10311-021-01322-8 (2022).
Miocic, J. et al. Underground hydrogen storage: a review. Geol. Soc. Lond. Special Publications. 528, 73–86. https://doi.org/10.1144/SP528-2022-88 (2023).
Dopffel, N. et al. Exploring Microbiological Dynamics in a Salt Cavern for Potential Hydrogen Storage Use. Environ. Microbiol. Rep. 17, e70064. https://doi.org/10.1111/1758-2229.70064 (2025).
Bordenave, S., Chatterjee, I. & Voordouw, G. Microbial community structure and microbial activities related to CO2 storage capacities of a salt cavern. Int. Biodeterior. Biodegrad. 81, 82–87 (2013).
Schwab, L. et al. Structural analysis of microbiomes from salt caverns used for underground gas storage. Int. J. Hydrog. Energy. 47, 20684–20694. https://doi.org/10.1016/j.ijhydene.2022.04.170 (2022).
Lee, C. J. D. et al. NaCl-saturated brines are thermodynamically moderate, rather than extreme, microbial habitats. FEMS Microbiol. Rev. 42, 672–693. https://doi.org/10.1093/femsre/fuy026 (2018).
Belilla, J. et al. Archaeal overdominance close to life-limiting conditions in geothermally influenced hypersaline lakes at the Danakil Depression, Ethiopia. Environ. Microbiol. 23, 7168–7182. https://doi.org/10.1111/1462-2920.15771 (2021).
Belilla, J. et al. Hyperdiverse archaea near life limits at the polyextreme geothermal Dallol area. Nat. Ecol. Evol. 3, 1552–1561. https://doi.org/10.1038/s41559-019-1005-0 (2019).
Moors, H., De Craen, M., Smolders, C., Provoost, A. & Leys, N. The waterbodies of the halo-volcanic Dallol complex: earth analogs to guide us, where to look for life in the universe. Front. Microbiol. 14–2023. https://doi.org/10.3389/fmicb.2023.1134760 (2023).
Payler, S. J. et al. An Ionic Limit to Life in the Deep Subsurface. Front. Microbiol. 10–2019 https://doi.org/10.3389/fmicb.2019.00426 (2019).
14 Oren, A. Novel insights into the diversity of halophilic microorganisms and their functioning in hypersaline ecosystems. npj Biodivers. 3, 18. https://doi.org/10.1038/s44185-024-00050-w (2024).
Fox-Powell, M. G., Hallsworth, J. E., Cousins, C. R. & Cockell, C. S. Ionic Strength Is a Barrier to the Habitability of Mars. Astrobiology 16, 427–442. https://doi.org/10.1089/ast.2015.1432 (2016).
Hallsworth, J. E., Heim, S. & Timmis, K. N. Chaotropic solutes cause water stress in Pseudomonas putida. Environ. Microbiol. 5, 1270–1280. https://doi.org/10.1111/j.1462-2920.2003.00478.x (2003). https://doi.org/.
Ball, P. & Hallsworth, J. E. Water structure and chaotropicity: their uses, abuses and biological implications. Phys. Chem. Chem. Phys. 17, 8297–8305. https://doi.org/10.1039/C4CP04564E (2015).
Cray, J. A., Russell, J. T., Timson, D. J., Singhal, R. S. & Hallsworth, J. E. A universal measure of chaotropicity and kosmotropicity. Environ. Microbiol. 15, 287–296. https://doi.org/10.1111/1462-2920.12018 (2013).
Hallsworth, J. E. et al. Limits of life in MgCl2-containing environments: chaotropicity defines the window. Environ. Microbiol. 9, 801–813. https://doi.org/10.1111/j.1462-2920.2006.01212.x (2007).
Cray, J. A. et al. Chaotropicity: a key factor in product tolerance of biofuel-producing microorganisms. Curr. Opin. Biotechnol. 33, 228–259. https://doi.org/10.1016/j.copbio.2015.02.010 (2015). https://doi.org/https://doi.org/
Steinle, L. et al. Life on the edge: active microbial communities in the Kryos MgCl(2)-brine basin at very low water activity. Isme j. 12, 1414–1426. https://doi.org/10.1038/s41396-018-0107-z (2018).
Yakimov, M. M. et al. Microbial community of the deep-sea brine Lake Kryos seawater-brine interface is active below the chaotropicity limit of life as revealed by recovery of mRNA. Environ. Microbiol. 17, 364–382. https://doi.org/10.1111/1462-2920.12587 (2015).
Gómez, F. et al. Ultra-small microorganisms in the polyextreme conditions of the Dallol volcano, Northern Afar, Ethiopia. Sci. Rep. 9, 7907. https://doi.org/10.1038/s41598-019-44440-8 (2019).
Belilla, J. et al. Active Microbial Airborne Dispersal and Biomorphs as Confounding Factors for Life Detection in the Cell-Degrading Brines of the Polyextreme Dallol Geothermal Field. mBio 13, e00307–00322. https://doi.org/10.1128/mbio.00307-22 (2022).
Smith, S. M. & Poulson, S. R. Agar Gelation Spectrophotometric Assay of Chao- and Kosmo-Tropicity of Inorganic Salts, and Implications for Life in Terrestrial and Martian Brines. Congress on Brines in the Solar System: Modern Brines, 25-28 October 2021. LPI Contrib. No. 2614 (2021)
Ovreås, L., Forney, L., Daae, F. L. & Torsvik, V. Distribution of bacterioplankton in meromictic Lake Saelenvannet, as determined by denaturing gradient gel electrophoresis of PCR-amplified gene fragments coding for 16S rRNA. Appl. Environ. Microbiol. 63, 3367–3373 (1997).
Crisler, J. D., Newville, T. M., Chen, F., Clark, B. C. & Schneegurt, M. A. Bacterial growth at the high concentrations of magnesium sulfate found in martian soils. Astrobiology 12, 98–106. https://doi.org/10.1089/ast.2011.0720 (2012).
Ollivier, B., Hatchikian, C. E., Prensier, G., Guezennec, J. & Garcia, J. L. Desulfohalobium retbaense gen. nov., sp. nov., a Halophilic Sulfate-Reducing Bacterium from Sediments of a Hypersaline Lake in Senegal. Int. J. Syst. Evol. MicroBiol. 41, 74–81. https://doi.org/10.1099/00207713-41-1-74 (1991).
Lerman, A. & Mackenzie, F. T. in in Encyclopedia of Geochemistry: A Comprehensive Reference Source on the Chemistry of the Earth. 206–226 (eds White, W. M.) (Springer International Publishing, 2018).
Dopffel, N., An-Stepec, B. A., Bombach, P., Wagner, M. & Passaris, E. Microbial life in salt caverns and their influence on H2 storage – Current knowledge and open questions. Int. J. Hydrog. Energy. 58, 1478–1485. https://doi.org/10.1016/j.ijhydene.2024.01.334 (2024).
Acknowledgements
We want to thank Ben Heydolph for his support in the lab.
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Open access funding provided by NORCE Research AS. This study was funded by Equinor ASA.
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A.K.: conceptualization, methodology, writing; K.M.: methodology, review and editing; J.B: review and editing, resources; S.H.: writing – review and editing, resources; N.D.: idea and conceptualization, methodology, writing.
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S. Hoth and J. Beeder are working for the company Equinor ASA, which is working towards hydrogen storage in salt caverns. All other authors have no competing interests.
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Kedir, A., Mayers, K., Beeder, J. et al. Predicting microbial activity potential in salt caverns based on brine chaotropicity analysis. Sci Rep (2026). https://doi.org/10.1038/s41598-026-40866-z
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DOI: https://doi.org/10.1038/s41598-026-40866-z