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FOR 741:  Nanoscale Processes and Geomaterials Properties

Subject Area Geosciences
Term from 2007 to 2016
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 22341081
 
Nanometer scale structures in geological materials such as crystal defects, grain- and phase boundaries and small scale chemical zoning patterns may provide insight into the processes, which occur on the atomic or molecular level and control the kinetics of mineral reactions. The processes involved in breaking and establishing bonds at reaction sites and in material transport in between, govern the development of microstructures and textures and this way coin the geodynamic record contained in the phase assemblage and in the fabric of a rock. In addition, they determine how and at what rate bulk rock properties change in response to external forcing and possibly feed back into geodynamic processes. Both, reading the information stored in rock fabrics as well as a better understanding of the feedback between transient bulk material properties and geodynamics require a thorough understanding of the processes underlying phase and fabric change in geological materials.
The objective of this Research Unit is to stimulate coordinated research, which is focused on grain- and phase boundary processes and their implications for reaction kinetics, microstructure development and bulk material properties. This research builds on well established concepts from equilibrium thermodynamics and reaction kinetics, and it makes use of recent advances in analytical and experimental techniques as well as of new theoretical and computational capabilities. The Research Unit aims to integrate expertise from field- and laboratory based researchers in mineralogy, petrology, geochemistry, mineral- and petrophysics as well as from materials science, physics and applied mathematics to generate new competence in geo-materials science.
The expected outcomes of this Research Unit will help to answer long standing questions up to the mechanisms and rates of mineral reactions, the size and life times of chemical and isotopic equilibration domains and the feedback between mineral reactions and mechanical stress. They will help to critically evaluate and improve existing petrological, geochemical and geochronological models, and will contribute to a better understanding of the transient nature of bulk material properties. This will allow refinement of geodynamic models and geophysical tools, and it will foster the understanding of the links between microscopic processes, bulk material properties and the evolution of geological systems in space and time.
DFG Programme Research Units
International Connection Austria

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