Formation of 60° ⟨01(1)over-bar0⟩ boundaries between {10(1)over-bar2} twin variants in deformation of a magnesium alloy

Interrupted tensile testing along the normal direction of a rolled AZ31 magnesium plate was conducted at various strain levels from 6% to 15.5%. Prior to deformation the specimens were annealed for grains to coarsen such that multiple twin variants in one grain can be activated and interaction between variants can be better resolved. The grain structure and texture evolution were then examined via electron backscatter diffraction. The results reveal that multiple primary {10 (1) over bar2}(p) twin variants inside individual grains grow and impinge, forming profuse boundaries of 60 degrees(01 (1) over bar0) orientation relationship. These boundaries are close to {11 (2) over bar2}(11 (2) over bar(3) over bar) twin relationship, however, they are not formed by twin nucleation and are only a product of interaction between the primary twins. The morphology of these special boundaries are highly irregular. Atomistic simulations were performed to understand such interaction, and the results show that such 60 degrees < 01 (1) over bar0 > boundaries have limited mobility. Thus, a primary twin variant is able to grow at the expense of other primary twin variants. Our experimental results also show that {10 (1) over bar2} twinning is active throughout the deformation until the specimens are fractured. As the strain increases, secondary {10 (1) over bar2}(S) twins are activated inside the primary twins. As the strain further increases to near fracture, {10 (1) over bar1}(S) secondary twins are activated inside the primary twins, followed by activation of tertiary {10 (1) over bar2}(r) twins inside the {10 (1) over bar1}(S) secondary twins, a process known as {10 (1) over bar1}-{10 (1) over bar2} double twinning. The formation of irregular 60 degrees < 01 (1) over bar0 > boundaries and the sequential twinning at large strains shed new light on the twinning mechanism in Mg and other hexagonal close-packed metals.