Projects of phase 2 of the research unit FOR 2125
Project 0 |
Coordination of the Research Unit |
Project 1 |
Phase stabilities of carbonates and reaction between carbonates and mantle minerals at high pressures and temperatures studied in the LH-DAC by Raman and time-resolved laser fluorescence spectroscopy |
Project 2 |
Structural, electronic and thermodynamic properties of carbonates at high pressures and temperatures by in situ spectroscopy and atomic-scale simulations |
Project 3 |
Electronic structure of Fe/Mg carbonates at conditions of the Earth's lower mantle: Implications for the formation of tetrahedrally coordinated carbon |
Project 4 |
X-ray spectroscopy and X-ray diffraction studies of element redistribution processes between carbonates and mantle phases at mantle conditions |
Project 6 |
Elastic properties of carbonates at high pressures and temperatures |
Project 7 |
Chemical reactions between carbonates and pyrolite mantle and the origin of ultradeep diamonds |
Project 8 |
Phase relations and melting in the system CaCO3–MgCO3 at high pressures and temperatures |
Project 9 |
Elasticity and structure evolution of carbonates at upper mantle conditions |
Projects of phase 1 of the research unit FOR 2125
Project 0 |
Coordination of the Research Unit and central facility for diamond shaping and sample preparation |
Project 1 |
Phase stabilities of carbonates at high pressures and temperatures studied in the LH-DAC by CARS and TRLFS |
Project 2 |
Structural, electronic and thermodynamic properties of carbonates at high pressures and temperatures by in situ spectroscopy and electronic structure calculations |
Project 4 |
X-ray fluorescence and X-ray absorption spectroscopy studies of element redistribution processes between carbonates and mantle phases at lower mantle conditions |
Project 5 |
Carbonates under shock compression: stability, phase transitions, and chemical reactions with silicates |
Project 6 |
Elastic properties of cabrbonates at high pressures and temperatures |
Project 7 |
Chemical reactions between carbonates and pyrolite mantle and the origin of ultradeep diamonds |