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Exceptional ductility can be achieved when warm deformation is accompanied by austenite reversion.
This research will provide metallurgical principles for warm deformation of steel under reversed transformation.
The process of grain subdivision during warm deformation is essential for the formation of ultrafine grains in such a material.
The current work investigated the relationship between microstructure and warm deformation properties in a strong but ductile Mn-rich steel.
This included warm deformation of supercooled austenite followed by reheating in the austenite region and cooling (RHA).
Therefore, for a proper designing of an industrial forming process performing under warm deformation conditions, the effect of dynamic strain aging should be taken into account.
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Here, we address the question whether we can turn this challenge into an opportunity by creating defined thermomechanical histories in polymers, represented by a specific morphology and nanostructure, to equip polymeric shaped bodies with desired functions, e.g. a temperature-memory, by hot, warm or cold deformation into multiblock copolymers having two partially overlapping melting transitions.
The ground on the south side of the crustal deformation area (warm-colored area) moved toward the satellite, while the ground on the north side (cold-colored area) moved away from the satellite.
This peculiar phenomenon was attributed to characteristic features of the microstructure that developed during warm rolling, such as deformation-induced high-angle grain boundaries and steep in-grain orientation gradients.
In order to ensure the physics performance of the muon detectors, the deformation of the warm structure is minimised during the design phase.
We argue that the generation of seismic lamination and anisotropy in the lower crust is a consequence of the same tectonic process, that is, ductile deformation in a warm and low-viscosity lower crust.
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