Projects

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