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Heat Transport in Fractures and Fracture Networks – Simulation, Inversion, Measurements

Project description

Deciphering the impact of fracture geometries on heat transfer efficiency

Fractured reservoirs, depending on their geometries, can be suitable for enhanced geothermal systems. They provide an ideal trajectory for circulating the working fluid while efficiently extracting heat. With the support of the Marie Skłodowska-Curie Actions programme, the HeatSIM project aims to study the coupled thermal-hydraulic processes in fractured rocks and the resulting heat transfer over different scales. It will first measure heat transfer in a variety of experimental fracture geometries and quantify the impact geometric parameters have on the outflow temperature. Then, using inverse modelling techniques, it will apply conceptual simplifications to the experimental geometries, together with numerical simulation to predict outflow temperatures. Several such models will be executed to calibrate their hydraulic and thermal properties from the experimental thermal breakthrough curves.

Objective

Fractured reservoirs are targets for enhanced geothermal systems (EGS), because a network of fractures in an otherwise solid rock is an optimal pathway for circulating the working fluid while efficiently extracting heat. The main ambition of HeatSIM (Heat Transport - Simulation, Inversion, Measurements) is to increase our comprehension of coupled thermal-hydraulic processes and the resulting heat transfer in fractured rocks over different scales, by experimental imaging, numerical simulation and inverse modeling of lab data. The first work package (WP1) will measure heat transfer in laboratory experiments, focusing on the influence of fracture wall topographies and local fracture apertures, dead-end fractures, fracture network topology, and fracture intersections. To this aim, a novel optical thermometry measurement technique, based on the temperature-dependent fluorescence of phosphor colloids, will provide the evolving temperature field within the fluid domain and solid matrix with high spatial and temporal resolutions. A sensitivity analysis will allow quantifying the influence of the various geometric parameters on the outflow temperature. HeatSIM’s WP2 will then propose conceptual simplifications to the experimental geometries, coupled to numerical simulation to predict outflow temperatures. Different such models will be implemented, and their hydraulic and thermal properties will be calibrated from the experimental thermal breakthrough curves. Their outflow temperature prediction capabilities will also be compared. Thanks to the applicant’s strong background in EGS, numerics and inverse modeling, and the host team’s expertise in fractured media, subsurface heat transport and lab experiments, HeatSIM will thus decipher the impact of fractured media’s geometry on heat transfer efficiency, and provide new insights into the prediction of geothermal sites’ efficiency and the optimization of geothermal energy energy extraction.

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HORIZON-TMA-MSCA-PF-EF - HORIZON TMA MSCA Postdoctoral Fellowships - European Fellowships

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(opens in new window) HORIZON-MSCA-2024-PF-01

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Coordinator

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 242 260,56
Address
RUE MICHEL ANGE 3
75794 PARIS
France

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Ile-de-France Ile-de-France Paris
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