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PhD Research Fellow in ML-assisted reservoir characterization/modelling for CO2 storage (ref 290702)
strong machine learning and numerical modelling background to add knowledge on the impact of geological heterogeneity and subsurface environments (e.g., depth, exhumation, temperature, pressure) to de-risk
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model by integrating the newly developed approaches into the numerical program developed in the ‘OceanCoupling ’ project. We would like the successful applicant to start in the first quarter of 2026
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(or equivalent) in both the thesis and the master's degree. Expertise in numerical modeling, programming, handling large amounts of data, and experience with AI and machine learning is an advantage. Good
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and dynamic reservoir modelling, and flow simulation. The candidate will work in a team of geologists, geophysicists, geochemists and staff with strong machine learning and numerical modelling
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to modern data-rich approaches, in which the underlying initial-boundary value problem is reformulated in such a way that loads, boundary conditions and constitutive models are completely or partially
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reformulated in such a way that loads, boundary conditions and constitutive models are completely or partially replaced by some form of experimental data. The research activities associated to the position
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Cathodoluminescence microscopy. Image analysis. Vitrinite Reflectance analysis. Raman spectroscopy. Porosity and permeability analysis. Relevant experience from rock deformation experimental work and/or numerical
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, geochemists and staff with strong machine learning and numerical modelling background to add knowledge on the impact of geological heterogeneity and subsurface environments (e.g., depth, exhumation, temperature
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Reflectance analysis. Raman spectroscopy. Porosity and permeability analysis. Relevant experience from rock deformation experimental work and/or numerical modelling is an advantage. Evidence of ability
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. Numerical simulations and theoretical membrane models will be developed, aiming to couple viscous interfacial fluid flow, elastic deformations and wetting-like processes at cellular membranes. The theoretical