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ExpeCO2SolTrap

Financiado

Experimental investigation of CO2 solubility trapping in heterogeneous 3D porous...

Experimental investigation of CO2 solubility trapping in heterogeneous 3D porous media Atmospheric CO2 contributes to 2/3 of the Earth’s global warming by greenhouse effect. Storing CO2 in deep geological formations is the main mitigation measure currently available. ExpeCO2SolTrap addresses solubility trapping (ST)... ver más

31/05/2024

UNIVREN

196K€

Presupuesto del proyecto: 196K€

Líder del proyecto

UNIVERSITE DE RENNES No se ha especificado una descripción o un objeto social para esta compañía.

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Financiación concedida El organismo HORIZON EUROPE notifico la concesión del proyecto el día 2024-05-31

HORIZON-MSCA-2021-PF-01-01: MSCA Postdoctoral Fellowships 2021 ExpectedOutcome:

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Cerrada hace 3 años

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2 Participantes

UNIVREN

195.91K€ | Lider

CNRS

N.D. | Participante

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Duración del proyecto: 24 meses Fecha Inicio: 2022-05-20
Fecha Fin: 2024-05-31

Líder del proyecto

UNIVERSITE DE RENNES No se ha especificado una descripción o un objeto social para esta compañía.

Presupuesto del proyecto 196K€

Descripción del proyecto Atmospheric CO2 contributes to 2/3 of the Earth’s global warming by greenhouse effect. Storing CO2 in deep geological formations is the main mitigation measure currently available. ExpeCO2SolTrap addresses solubility trapping (ST), a trapping mechanism of CO2 in dissolved form within the resident brine of the subsurface porous medium, which allows storing CO2 perennially by gravity. ST has been studied extensively in the last 10 years. But numerical studies cannot account for the pore scale heterogeneity of the flow, while most experiments cannot provide a full measurement of the system’ evolution (in particular its dissolution flux). Recent ground-breaking experiments by the host group and secondmend group of ExpeCO2SolTrap have shown that the growth of the instability is orders of magnitude faster than that predicted by a Darcy scale numerical simulation of the experimental process, due to coupling beween the gravitatitional instability and the heterogeneity of pore scale flow. This effect has been hitherto ignored in the literature. Furthermore, the impact of Darcy scale heterogeneity has hardly been studied, in particular not experimentally. ExpeCO2SolTrap proposes to (i) extend the experiments developed in the host group and secondment group to allow for pore scale measurement of fluid velocities three-dimensional (3D) granular porous media, in order to fully understand the aforementioned coupling, and (ii) to study the impact of Darcy scale (e.g., permeability/porosity) heterogeneity of the medium experimentally in granular porous media as well as in 3D-printed porous media of controlled heterogeneity. Two experiments, both relying on refractive index matching of the flowing liquid to the solid phase, but using respectively analogue fluids and dissolved CO2, will be used in parallel. Pore scale concentration fields will be measured by laser-induced fluorescence and scanning by laser sheets, while fluid velocities will be measured by stereo-PIV.

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