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on ice will be performed in the cryo-deformation facility at Institut des Géosciences de l'Environnement (IGE, Grenoble, FR). The PhD will be cosupervised by Andréa Tommasi (Géosciences Montpellier) and M
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major challenge for environmental fluid mechanics, as the mechanisms at work in the generation of these waves are highly complex, with three interacting phases: solid grains, interstitial gas and water
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the properties of smectite, a swelling clay mineral that form the core of many of the fault zones and that is able to adsorb significant amounts of water in-between nanometric interlayers. Despite their potential
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continuum theory expectations, and many of the observed phenomena still defy explanation. In particular, while water dynamics are expected to remain largely classical under extreme confinement, several
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ultimate objective, we aim at investigate the catalytic properties of these supported catalysts in the context of water electrolysis occurring in an alkaline environment. The researcher (M/F), recruited
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dissipation, fluid motion can induce electron currents. This type of effect, linked to the Coulomb and phonon drag phenomena, has been measured for water transport in carbon nanotubes, and in experiments
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the experimental results of flow tunneling to fluid mixtures, and in particular to water-glycerol mixtures as a model system. The aim will be to study fluid separation induced by a difference in the overlap
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approaches in culture and photophysiology (photosynthesis, sugar production). The symbiotic microalgae will be collected at sea during sampling campaigns. Requirements Research FieldBiological
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exhibit isotopic fractionation. This process leaves a fingerprint on the products of these reactions. If records of these products are preserved, as in the case of ice cores, for example, the isotopic
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on ice will be performed in the cryo-deformation facility at Institut des Géosciences de l'Environnement (IGE, Grenoble, FR). The PhD will be cosupervised by Andréa Tommasi (Géosciences Montpellier) and M