Exploring the cycle of H2 gas using numerical modelling in the context of a deep geological repository

Hydrogen gas (H2) generation due to microbially influenced corrosion (MIC) is an important evaluation to build confidence in long term safety of the Canada’s proposed high level nuclear waste deep geological repository (DGR). Numerical modelling can be a powerful tool as the DGR design life far exce...

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Bibliographic Details
Main Authors: Md Abdullah Asad, Tarek L. Rashwan, Ian L. Molnar, Mehran Behazin, Peter G. Keech, Magdalena M. Krol
Format: Article
Language:English
Published: Elsevier 2025-09-01
Series:Results in Engineering
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Online Access:http://www.sciencedirect.com/science/article/pii/S2590123025020808
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Summary:Hydrogen gas (H2) generation due to microbially influenced corrosion (MIC) is an important evaluation to build confidence in long term safety of the Canada’s proposed high level nuclear waste deep geological repository (DGR). Numerical modelling can be a powerful tool as the DGR design life far exceeds the timescales of laboratory or field studies. This work presents the first numerical modelling study exploring long-term H2 dynamics under DGR environments. The key processes relevant to H2 production and consumption are identified and two numerical models are presented; one that focuses on H2 transport through the bentonite buffer and host rock, and another that considers production of H2 through MIC and the biotic H2 consumption (modelled through a simplified approach). This work is to investigate whether the net amount of H2 would surpass the solubility limit leading to H2 gas formation, using conservative assumptions of HS− and H2 flux conversion when sulfate is a non-limiting species. The modelling study showed that long-term H2 production from MIC may depend on HS− supply to the UFC, H2 transport properties, and biotic H2 consumption processes. While the HS− supply could increase the H2 formation, H2 transport through the rock and biotic H2 consumption processes were shown to control the accumulation of H2. Amongst various modelling scenarios, the H2 solubility limit was never surpassed, indicating the unlikelihood of H2 gas pressure build-up in a DGR under these modelling conditions. Altogether, this study provides valuable insight into H2 production, consumption, and transport dynamics in a DGR environment.
ISSN:2590-1230