Geological modeling uncovers regional variations in natural hydrogen potential across diverse source rock systems, highlighting scalable exploration pathways for clean energy development.
This study presents the first quantitative evaluation of natural hydrogen prospectivity in Italy, developed within the EU-funded NHEAT—Natural Hydrogen for Energy trAnsiTion—project. It integrates geological, geochemical, and geophysical data through a reaction-specific workflow, and introduces a semi-quantitative hydrogen prospectivity index to classify and rank potential exploration target areas, primarily based on source rocks. The results identify Tuscany as the top-priority region, where granitoid-hosted hydrothermal systems are associated with documented H 2 emissions. The Voltri Massif shows moderate potential linked to active serpentinization, while the Northern Apennines may potentially preserve fossil H 2 . In the Ivrea–Verbano Zone, granitoids of Calabria and Sardinia, and in the Western and Central Alps, H 2 could be generated from low-temperature secondary oxidation reactions. The Po Basin may sustain organic-related H 2 production. This national-scale assessment highlights Italy as a natural laboratory for diverse hydrogen systems and provides a transferable workflow for identifying and developing natural hydrogen resources worldwide.
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Spagnolo et al. (2026) studied this question.
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