-
, are robust tracers of fluid origin, production mechanisms, and migration pathways. Helium, transported notably by CO₂ and hydrothermal fluids, is a key tracer of mantle contributions and deep sources of H
-
produced under conditions representative of rocket engines, for a selection of metals. After meticulous experimental characterization, the unique database obtained will be exploited to enhance the modeling
-
cameras to characterize flow and wave parameters. - Numerical modeling of laboratory experiments. This work is part of and funded by the ANR Slide2Wave program, coordinated by Philippe Gondret (FAST
-
of electrochemical effects into numerical and theoretical models describing the flows within LMBs. These flows, driven by magnetohydrodynamic or thermal phenomena, can become unstable and lead to a short circuit of
-
single fluid vortex and a liquid/gas interface in various configurations through theoretical/numerical modelling and stability analyses. The following configurations will be analysed : - a horizontal fluid
-
. These data will be integrated into TemisFlow (Themis) thermal models to reconstruct the thermal and subsidence history of the basins. The modeling will quantify the distribution of heat flow during
-
models indicate that the thermal structure of the European lithosphere remained stable during the Mesozoic, potentially due to small-scale convection at its base. To evaluate this hypothesis, the study
-
through the EU Research Framework Programme? Not funded by a EU programme Is the Job related to staff position within a Research Infrastructure? No Offer Description Within the current environmental context
-
reliable than the current state of the art, by exploiting techniques from semiclassical analysis, an area of pure mathematics specifically designed to study high-frequency problems. This will be achieved by