Real time monitoring of hydrogenotrophic methanogenesis under deep saline aquifers conditions.

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Autori principali: Vidal, Emeline, Cario, Anaïs, Jouvin, Mathilda, Abadie, Maïder, Nguyen, Olivier, Erriguible, Arnaud, Ranchou-Peyruse, Anthony, Marre, Samuel
Natura: Artículo científico
Lingua:en
Pubblicazione: Journal of biological engineering 2026
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author Vidal, Emeline
Cario, Anaïs
Jouvin, Mathilda
Abadie, Maïder
Nguyen, Olivier
Erriguible, Arnaud
Ranchou-Peyruse, Anthony
Marre, Samuel
author_facet Vidal, Emeline
Cario, Anaïs
Jouvin, Mathilda
Abadie, Maïder
Nguyen, Olivier
Erriguible, Arnaud
Ranchou-Peyruse, Anthony
Marre, Samuel
Vidal, Emeline
Cario, Anaïs
Jouvin, Mathilda
Abadie, Maïder
Nguyen, Olivier
Erriguible, Arnaud
Ranchou-Peyruse, Anthony
Marre, Samuel
collection PubMed - marine biology
contents Real time monitoring of hydrogenotrophic methanogenesis under deep saline aquifers conditions. Vidal, Emeline Cario, Anaïs Jouvin, Mathilda Abadie, Maïder Nguyen, Olivier Erriguible, Arnaud Ranchou-Peyruse, Anthony Marre, Samuel To investigate the microbial response to deep underground gas injection, specifically CO2 and H2, a new optically transparent high-pressure reactor was developed to monitor autotrophic microbial growth via in situ and ex situ characterization techniques. The main advantages rely on avoiding any decompression phases during the entire process, thanks to direct optical access. Here, we monitored the growth of the model methanogenic strain Methanothermococcus thermolithotrophicus by applying different H2/CO2 partial pressures at a total pressure of 100 bar, which is representative of the deep underground storage environment. These reactors can be used to investigate deep microbial strains under pressure conditions close to their natural environments, eliminating decompression biases. Additionally, we measured the methane production of the strain at the end of the incubation, with or without stirring. The results showed an increase in methane production with increasing CO2 and H2 partial pressures, up to p(H2/CO2, 80/20 mol%) = 15 bar for unstirred conditions and p(H2/CO2, 80/20 mol%) = 30 bar for stirred conditions, respectively. This difference in behavior depending on stirring conditions was clearly observed through biofilm formation in the absence of stirring, favoring methane production and extending the range of H2 / CO2 partial pressures under which the strain can grow.
format Artículo científico
id pubmed_41559801
institution PubMed
language en
publishDate 2026
publisher Journal of biological engineering
record_format pubmed
spellingShingle Real time monitoring of hydrogenotrophic methanogenesis under deep saline aquifers conditions.
Vidal, Emeline
Cario, Anaïs
Jouvin, Mathilda
Abadie, Maïder
Nguyen, Olivier
Erriguible, Arnaud
Ranchou-Peyruse, Anthony
Marre, Samuel
Real time monitoring of hydrogenotrophic methanogenesis under deep saline aquifers conditions. Vidal, Emeline Cario, Anaïs Jouvin, Mathilda Abadie, Maïder Nguyen, Olivier Erriguible, Arnaud Ranchou-Peyruse, Anthony Marre, Samuel To investigate the microbial response to deep underground gas injection, specifically CO2 and H2, a new optically transparent high-pressure reactor was developed to monitor autotrophic microbial growth via in situ and ex situ characterization techniques. The main advantages rely on avoiding any decompression phases during the entire process, thanks to direct optical access. Here, we monitored the growth of the model methanogenic strain Methanothermococcus thermolithotrophicus by applying different H2/CO2 partial pressures at a total pressure of 100 bar, which is representative of the deep underground storage environment. These reactors can be used to investigate deep microbial strains under pressure conditions close to their natural environments, eliminating decompression biases. Additionally, we measured the methane production of the strain at the end of the incubation, with or without stirring. The results showed an increase in methane production with increasing CO2 and H2 partial pressures, up to p(H2/CO2, 80/20 mol%) = 15 bar for unstirred conditions and p(H2/CO2, 80/20 mol%) = 30 bar for stirred conditions, respectively. This difference in behavior depending on stirring conditions was clearly observed through biofilm formation in the absence of stirring, favoring methane production and extending the range of H2 / CO2 partial pressures under which the strain can grow.
title Real time monitoring of hydrogenotrophic methanogenesis under deep saline aquifers conditions.
url https://pubmed.ncbi.nlm.nih.gov/41559801/