(110244)In-situ neutron diffraction investigation on the martensite transformation, texture evolution and martensite reversion in high manganese TRIP steel

摘要

In order to reveal the behaviors of two kinds of martensites (e-M and α'-M) transformation during TRIP and reversion process and to separate transformation textures from rolling textures during the TRIP process, the phase transformation and texture evolution during cold rolling and the subsequent heating in high manganese TRIP steel were investigated by time-of-flight neutron diffraction measurement. The results show that the TRIP process occurred mainly at the rolling reductions ranging from 0% to 60%. The transformation of γ →ε-M and e-M → α'-M didn't occur synchronously and the transformation of γ →ε-M was easier and occurred earlier. The cube-oriented γ grains transformed to martensite most easily showing an orientation dependence and the y grains with other orientations tend to form preferentially the {100} orientation in a'-M phase demonstrating a strong variant selection during the TRIP process below the 60% rolling reduction. The {113}<110> texture of α'-M rotated toward a more stable orientation {112}<110> with increasing reduction and a shift of texture components from rotated cube and a-fibre to the y-fibre occurred at higher rolling reduction. The e-M texture was characterized by a constant {0001} peaks 20°-tilted toward RD at any reduction related with a high Schmid factor for basal slip. For the 60% rolled sample, the reversion of e-M and a'-M to y-phase occurred at temperatures ranging from 300 °C to 500 °C and 500 °C to 700 °C, respectively. During heating, the deformed a'-M did not change its texture until decomposition and swallowing-up by austenite, and the retained and newly nucleated y grains inherited their initial Goss and brass orientations until their recrystallization and replacing by Goss texture. This weak Goss texture remained during further heating to 900 °C and subsequent cooling. In addition, the transformation of both kinds of thermally-induced martensites during cooling can only occurred below 200 °C.