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of the CNRS National Institute of Physics (CIMI - ECHO - KEMTRONIX - PulSAr - VoltEdge - SAMSON). The PhD student will join the ECHO Team. This work is in the context of two projects ANR both
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for the heliophysics component, and LISN in Orsay for the computer science and natural language processing component. Status meetings every two weeks, alternately at LIRA in Meudon and at LISN in Orsay. The PhD thesis
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minerals which precipitate at the interface between two grains enhance the mechanical properties of the porous media. We invite application for a PhD at the CNRS-University of Toulouse to gain a better
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global ocean model (ECCO-Darwin-type sediment module) to quantify alkalinity generation and associated CO2 storage. This PhD investigates the dissolution of calcium carbonate (CaCO3) in the deep sea, with
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competition between zones of advective transfer and zones of diffusive transfer where the fluxes of leaching reagents and products are very low. We invite application for a PhD at the CNRS-University
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technicians, and administrative staff) and around 50 PhD students and postdoctoral researchers. The successful candidate will be assigned to the LMV's petrology team, which reports directly to the Director of
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2 Aug 2026 Job Information Organisation/Company CNRS Department Institut de Recherche sur les Archéomatériaux Research Field History History » Archaeology History » Medieval history Researcher Profile First Stage Researcher (R1) Application Deadline 22 Aug 2026 - 23:59 (UTC) Country France Type...
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Research Infrastructure? No Offer Description This PhD project is part of a long-standing collaboration between the LOCEAN laboratory (UMR 7159) and the LJK laboratory (UMR 5224), which has already resulted
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number of undergraduate and graduate students—including many PhD candidates—as well as postdoctoral researchers and visiting scientists. The laboratory covers a wider range of topics than its name suggests
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at the glacier scale (Braconnot et al., 2019; Cretat et al., 2020). During this PhD, the candidate will study the relationships between high-altitude climate, geomorphological context, and glacier evolution during