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Paris Cardiovascular Research Center, Inserm U970 | Paris 15, le de France | France | about 11 hours ago
new strategies to promote cerebrospinal fluid drainage. Missions` Characterization of brain drainage pathways in genetically modified mice The fellow will characterize dural and extracranial lymphatics
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extensive experience on Von Karman swirling flows with fluids ranging from water, to Superfluid. Measurement techniques have thus been developed over the years and research is being out using state of the art
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(for 12 months) will be to study new methods for the synthesis and post-synthetic treatments of coordination polymers using supercritical fluids such as CO2 and NH3. The unexplored frontier between
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occasional “local contact” researchers from Grenoble laboratories. The researcher will report to the manager of the two beamlines. Where to apply Website https://emploi.cnrs.fr/Candidat/Offre/UPR2940-ELOBER
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institute of the Université Paris Cité. Bringing together more than 500 people, the IPGP studies the Earth and the planets from the core to the most superficial fluid envelopes, through observation
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(s) Number of offers available1Company/InstituteLaboratoire de Mécanique des Fluides de Lille - Kampé de FérietCountryFranceCityVILLENEUVE D ASCQGeofield Contact City VILLENEUVE D ASCQ Website https
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manager is Sabine Rode. The recruited researcher will simulate flows within membrane modules using ANSYS Fluent computational fluid dynamics software. He or she will study the nature of flows and solute
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differential equations in fluid mechanics involving free surfaces and/or stratification. - Writing skills, ability to formulate a scientific project, publish and promote research. - Ability to work in a team
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(velocity, interface topology…) in the vicinity of interface with complex shape. We will design and manufacture fully new experiments that include fluid conduit, reservoir, heaters, electro-electric field
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resource accumulations (such as natural hydrogen, lithium and copper) result from fluid flow, heat transfer and fluid–rock interactions over geological timescales. In order to understand these systems and