Developing a Prospecting Methodology for Natural Hydrogen in the Voronezh Region. Part 1: Theoretical Foundations
DOI:
https://doi.org/10.17308/geology/1609-0691/2026/1/4-17Keywords:
hydrogen,, circument,, crystalline basement, helium, methaneAbstract
by its institutional recognition: in 2021, Australia became the first country to include it in its list of minerals, and since 2023, it has been added to the Russian Classification of Minerals. A key confirmation of the resource's potential is the commercial extraction of hydrogen in Mali. Scientists identify several hypotheses for the origin of hydrogen in the Earth's crust: deep-seated degassing, serpentinization, water radiolysis, biogenic decomposition of organic matter, and others. Its accumulations are associated with ophiolite belts, fault zones, and iron-rich Precambrian strata, while the preservation of deposits depends on the integrity of cap rocks that prevent its degassing. Ring structures – circuments, clearly visible in satellite images – are considered a promising exploration indicator. They may indicate gas transport systems or deep traps and mark areas of hydrogen degassing. However, their direct link to hydrogen degassing requires further study.
Methodology Development: for the first time in Russia, the authors have proposed a methodology for conducting hydrogen exploration works. During the exploration for natural hydrogen, a combination of desk-based, field, and laboratory research methods was applied, ensuring a multi-stage assessment of the hydrogen degassing potential in the study area. Desk-based studies served as the basis for regional forecasting and localization of promising areas. This phase included the compilation of specialized maps of potential hydrogen sources in Precambrian formations, based on the analysis of geological maps, deep structure data, mineralogical-petrographic characteristics of rocks, and existing geodynamic models of hydrogen generation (serpentinization, deep degassing, radiolysis, etc.). Mapping of potential hydrogen trap structures in the sedimentary cover involved identifying lithological seals capable of accumulating hydrogen fluids. The identification of promising and priority areas for gas sampling allowed for the ranking of territories by prospectivity based on a comprehensive analysis of geological, geophysical, and geochemical data. Interpretation of Earth remote sensing (ERS) data within the identified areas made it possible to delineate ring structures (circuments), which may mark zones of deep hydrogen degassing. Field studies provided direct verification of predictive models and the acquisition of factual data on the presence of hydrogen emanations. Laboratory studies enabled the determination of concentrations of helium dissolved in water, which serves as a reliable indicator of deep degassing, and its anomalous concentrations correlate with zones of hydrogen emission.
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