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Published on: October 5, 2019
Microbial-geochemical Interactions in Underground Reservoirs: Implications for Hydrogen Storage
Laura Fablet1, Arnaud Belcour2,3, Sylvain Stephant4
1BRGM, 3 Avenue Claude Guillemin, Orléans Cedex 2, 45060, France. fablet.laura@gmail.com.
Deep geological environments host diverse microbes influencing underground hydrogen storage. Salinity, carbon, and human activity shape microbial communities, with some potentially consuming stored hydrogen.
Area of Science:
- Geomicrobiology
- Environmental Science
- Subsurface Microbiology
Background:
- Understanding deep subsurface microbial ecosystems is critical for natural biogeochemical processes.
- Assessing microbial roles is essential for subsurface activities like underground hydrogen storage.
Purpose of the Study:
- To compare microbial communities and geochemistry in porous reservoirs versus salt caverns.
- To investigate factors influencing microbial structure and metabolic potential in deep geological settings.
Main Methods:
- Analysis of water chemistry.
- Characterization of microbial community composition.
- Assessment of microbial metabolic potential in contrasting geological environments.
Main Results:
- Porous reservoirs (esp. carbonate facies) have carbonate-rich fluids and anaerobic microbes (methanogens, fermenters, acetogens).
- Salt caverns contain salt-saturated brines and halophilic, chemoorganotrophic microbes adapted to high salinity.
- Anthropogenic activities and hydrogeological connections can alter reservoir geochemistry and microbial profiles.
Conclusions:
- Salinity, carbon availability, temperature, and human impact significantly influence microbial communities and their functions.
- Hydrogenotrophic microorganisms in reservoirs may consume injected hydrogen, impacting gas quality.
- Activity-based assessments of microbial hydrogen consumption are needed for effective mitigation strategies in underground hydrogen storage.
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