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- l'institut du thorax, INSERM, CNRS, Nantes Université
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self-supervised learning model, -Evaluating model performance using both simulations and experimental data, -Transitioning from a task-specific model to a foundation model, -Benchmarking results against
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) at multiple microwave frequencies. This work will be complemented by the systematic quantitative analysis of experimental data through spectral simulation, in combination with the use of various substrates
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molecular dynamics simulations with LAMMPS, and data curation. Scientific context: Our current understanding of polymer viscoelasticity is founded on single-chain models [2]. Such models draw on the fact
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l'institut du thorax, INSERM, CNRS, Nantes Université | Nantes, Pays de la Loire | France | 15 days ago
Devices" ). • Bring various improvements on the synthetic model (vasculature shape / aneurysm / background noise modelling) • Numerical simulations will be performed on a GPU HPC cluster. • Programming in
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. The postdoctoral researcher will develop numerical simulations that couple viscous flow in a magmatic dike with fracturing of the surrounding elastic lithosphere, building on existing numerical frameworks
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accessible observables in attoscience. The postdoctoral researcher will carry out methodological developments and advanced numerical simulations to explore these ultrafast dynamics in exotic systems. -Develop
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performing DFT/MLIP molecular dynamics simulations; - Analyzing and exploiting results, as well as writing activity reports and scientific publications and presenting results at conferences and working groups
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data, etc.). Build, calibrate, and validate numerical hydrogeological models (e.g., MODFLOW, FEFLOW, or equivalent) adapted to volcanic aquifer systems. Perform hydrological scenario simulations
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numerical approaches or simulations. A PhD in Physics, Materials Science, Earth and Planetary Sciences, or a related field is required for this position. Additional comments The candidate (M/F) is invited
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observation of the geomagnetic field from space on the one hand, and of advanced numerical simulations of the geodynamo on the other hand, have opened new avenues for our understanding of the dynamics at play