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Schmidt University Hamburg that has recently been funded by the German Research Council (DFG). The aim of this project is to investigate how microbially mediated pore-scale processes affect the overall
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important for the European economy and energy transition towards a carbon neutral future. Geothermal wells are located all over Europe and contain various minerals such as Lithium or Boron and energetic gases
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underlying these processes remain poorly represented. This PhD project aims to fill that gap by using molecular simulations to quantify the interactions of SOM and EPS with water and minerals, and to connect
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-funded project HYDROSPHEAR. The project will explore how H2O may be stored in hydrous minerals of the Earth's lower mantle by constraining their stability limits and physical properties by means
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industrial environmental burden of our generation. Disruptive innovations are required for alternative reduction processes that convert mineral ores into metals without today’s carbon-based methods
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, crystallographic and biological processes in the formation of minerals and rocks. Interactions at different geological and biological interfaces are investigated. At these interfaces, mass transfer processes
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carbon neutral future. Geothermal wells are located all over Europe and contain various minerals such as Lithium or Boron and energetic gases such as hydrogen and methane. Currently these geothermal wells
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exchanged between land, ocean and atmosphere through processes known as global biogeochemical cycles. Research activities in the IMPRS-gBGC aim at a fundamental understanding of these cycles, how
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organic compounds in the early earth ocean. We are looking for a PhD student (m/f/d) to start at the TUM this July or later. Your Task Hydrothermal vents where hot minerals stream into the ocean water are