Sort by
Refine Your Search
-
matter exist in theories beyond the SM, and the WIMP (Weakly Interacting Massive Particle) is one of the best motivated of these candidates, as it allows to also solve the SM hierarchy problem, directly
-
validation. The postdoctoral researcher will work within the Metasurface Team at CRHEA, in close interaction with permanent researchers, postdoctoral fellows, PhD students, engineers, and external
-
developed high-sensitivity detectors to probe newly discovered anomalous quantum Hall effect phases in rhombohedral graphene. In particular, we wish to study phases that, due to interaction, exhibit
-
combine density functional theory (DFT), molecular simulations, and machine-learning force field (ML-FF) development to uncover the factors controlling NHC–surface interactions and to model realistic
-
dilution while minimizing by-products. He or she will need to implement various techniques to best characterize the grafted functions. In particular, they will interact with the MolQIf consortium teams
-
Postdoctoral researcher (M/F). Modeling damage during earthquakes. Comparison with geophysical data.
), an internationally renowned laboratory that combines fieldwork, experimentation, and modeling to advance understanding of geological processes, continental surface dynamics, fracture-fluid interactions, and natural
-
validation. The postdoctoral researcher will work within the Metasurface Team at CRHEA, in close interaction with permanent researchers, postdoctoral fellows, PhD students, engineers, and external
-
Phase Field). The postdoctoral researcher will join the METAL team at the MateIS laboratory and will work in close collaboration with the IM2NP laboratory in Marseille. Interactions with the partners
-
complex datasets. Experience in the process of writing and publishing scientific articles in peer-reviewed journals. Experience in the themes of nanoparticle-plant interactions and the fate of associated
-
models) to estimate regional and local past land cover. This postdoc position offers a unique opportunity to contribute to our understanding of historical land-cover/erosion interactions and to feed