Electrochemical machining (ECM) uses chemical reactions to dissolve material from the surface layer of a structural component. This particular type of non-conventional machining avoids unwanted microstructural changes in the surface, such as the formation of dislocations. This makes ECM a promising processing technique for high-strength materials. In order to model the complex chemical reactions in a computationally efficient way, an inner variable is introduced that describes the degree of dissolution of the material. The evolution of the internal variable is formulated based on Faraday's law of electrolysis. Furthermore, the use of an effective formulation of the necessary material parameters allows the homogenized description of the dissolution process to be considered within an electrical finite element framework. Each effective material parameter is a result of classical mixture rules.
In cooperation with:
References:
In order to enable a mechanism-oriented analysis of the relations between manufacturing processes and the resulting material modifications at the surface of a workpiece in classical metalworking processes such as deep rolling, we have been working within the SFB/TRR 136 on the highly resolved simulation of mechanically and thermo-mechanically coupled processes. The basic assumption is that the loads present in the material during the process are responsible for its response in the form of a modification. This mechanism-oriented approach to the interaction of manufacturing processes with the material is scientifically new. In the future, it should enable manufacturing processes and process chains to be selected and adjusted in a targeted and knowledge-based manner with regard to the desired surface properties of the workpiece in order to enable a sustainable and resource-conserving production.
In cooperation with:
References:
In the lower magma reservoirs of volcanoes olivine crystals are formed. These crystals grow as they rise into the higher magma reservoirs until the volcano erupts. Diffusion chronometry is used to understand the diffusion history of the olivine crystals in volcanic eruptive products. However, the timescales which can be accessed by diffusion chronometry are restricted by recrystallization. While it has been shown in both experimental and field observations, the coupling of mechanical and chemical processes has not been explored in a quantitative framework yet. A new material model is developed, which takes the coupling of mechanical and chemical processes into account to describe the evolution of magnesium-based forsterite crystals exchanging iron as a fayalite component from the initial growth phase until the point of recrystallization.
In cooperation with:
References: