Pore-scale modelling of subsurface biomineralization for carbon mineral storage
This work is framed within the topic of microbially enhanced carbon mineralization: biological catalysts are utilized to alter reaction rates and enhance carbon mineralization in the context of CO2 storage in highly reactive minerals formations. We propose a micro-continuum Eulerian formulation of c...
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| Published in | Advances in water resources Vol. 185; p. 104641 |
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| Main Authors | , |
| Format | Journal Article |
| Language | English |
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01.03.2024
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| Abstract | This work is framed within the topic of microbially enhanced carbon mineralization: biological catalysts are utilized to alter reaction rates and enhance carbon mineralization in the context of CO2 storage in highly reactive minerals formations. We propose a micro-continuum Eulerian formulation of coupled flow and bio-geochemical reactive transport at the pore-scale, in which the reactive transport model is fully coupled with a biomass-nutrient growth model treated with Monod’s equation. In order to assess the role of biological catalysts in enhancing carbon mineralization, we then present simulations results and sensitivity studies of an application case of carbon mineralization in an idealized porous geometry with and without biomass growth at conditions relevant to CO2 storage in ultramafic rocks. Results clearly highlight the role of the biomass in enhancing the pH of the aqueous solution, a process called bioalkalinization, thereby leading in a highly non-linear way to enhanced calcite precipitation, resulting in an interesting potential methodology for CO2 immobilization.
•We study subsurface biomineralization as a potential method for CO2 storage.•We propose a pore-scale model of coupled flow and bio-geochemical reactive transport.•We present simulation results of a relevant application case of biomineralization.•Biological catalysts enhance carbon mineralization by increasing the local pH.•The enhanced precipitation depends on the mass ratio of enzyme urease to biofilm. |
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| AbstractList | This work is framed within the topic of microbially enhanced carbon mineralization: biological catalysts are utilized to alter reaction rates and enhance carbon mineralization in the context of CO2 storage in highly reactive minerals formations. We propose a micro-continuum Eulerian formulation of coupled flow and bio-geochemical reactive transport at the pore-scale, in which the reactive transport model is fully coupled with a biomass-nutrient growth model treated with Monod’s equation. In order to assess the role of biological catalysts in enhancing carbon mineralization, we then present simulations results and sensitivity studies of an application case of carbon mineralization in an idealized porous geometry with and without biomass growth at conditions relevant to CO2 storage in ultramafic rocks. Results clearly highlight the role of the biomass in enhancing the pH of the aqueous solution, a process called bioalkalinization, thereby leading in a highly non-linear way to enhanced calcite precipitation, resulting in an interesting potential methodology for CO2 immobilization.
•We study subsurface biomineralization as a potential method for CO2 storage.•We propose a pore-scale model of coupled flow and bio-geochemical reactive transport.•We present simulation results of a relevant application case of biomineralization.•Biological catalysts enhance carbon mineralization by increasing the local pH.•The enhanced precipitation depends on the mass ratio of enzyme urease to biofilm. |
| ArticleNumber | 104641 |
| Author | Sanchez-Vila, X. Starnoni, M. |
| Author_xml | – sequence: 1 givenname: M. orcidid: 0000-0002-8552-6997 surname: Starnoni fullname: Starnoni, M. email: michele.starnoni@upc.edu – sequence: 2 givenname: X. surname: Sanchez-Vila fullname: Sanchez-Vila, X. |
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| Keywords | Biomineralization CO2 storage Biogeochemistry Microbial carbon mineralization Pore-scale modelling Reactive transport modelling |
| Language | English |
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