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Postdoctoral researcher (M/F). Modeling damage during earthquakes. Comparison with geophysical data.
(# ANR-22-CE01-0028) funded by the ANR. This two-year project (01/04/26 to 31/03/28) aims to explore the link between the dynamics of rupture on seismic faults and the structure of the damage zone
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the Norwegian Institute for Nature Research (NINA) and partners in 14 countries. For more information, see: https://seatrack.net . This is a fixed termed position for 3 years in our section for terrestrial
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(based for instance on classical and/or ab initio molecular dynamics, combined with ONIOM-type QM/MM approaches) to gain deeper insight into the structure of the HFIP solvent, its coordination properties
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system housing the two arms of the PET-SCAN system - Develop a simulation tool to optimize the prototype structure - Develop software tools for data acquisition and processing This work is being carried
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: 019318 Prior to application, further information (including application procedure) should be obtained from the Work at UCD website: https://www.ucd.ie/workatucd/jobs/ Applications are invited from suitably
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of warming, nutrient enrichment and species invasions using size- or stage-structured population models (e.g., in R, Matlab, or Python). Writing scientific manuscripts and presenting findings at conferences
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also take into consideration market benchmarks, if and when appropriate, and internal equity to ensure fair compensation relative to the university’s broader compensation structure. We are committed
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Mohammed (Maurice Halbwachs Center, CNRS). This research project is structured around five axes: analysis of police and court records; sociology of the anti-drug police enforcement; analysis of the social
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broader compensation structure. We are committed to offering competitive and flexible compensation packages to attract and retain top talent. Benefits Rutgers provides a comprehensive benefits package to
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the boundary layer and the turbines, but also at the center. This should shed some new light on the dissipative structures and extreme events possibly responsible for the large scale evolution of the flow