Room-temperature plastic deformation of single crystals of α-manganese - hard and brittle metallic element

• Published in: International journal of plasticity Vol. 160; p. 103510
• Main Authors: Kishida, Kyosuke, Suzuki, Hirotaka, Okutani, Masaomi, Inui, Haruyuki
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.01.2023
• Subjects: Deformation structure; Dislocations; Manganese; Mechanical properties; Micropillar compression; Mechanical properties; Micropillar compression; Deformation structure; Manganese; Dislocations
• ISSN: 0749-6419; 1879-2154
• DOI: 10.1016/j.ijplas.2022.103510

•Plastic deformation behavior of α-Mn single crystals was investigated by micropillar compression at room temperature.•α-Mn single crystals are found to plastically deform by dislocation motion at room temperature, accompanied by very high yield stresses of the range of 4–6 GPa.•Slip along [111] and [001] are identified to operate.•Any low-indexed slip planes cannot be assigned for both slip, because of the significantly wavy nature of slip lines. The deformation behavior of single crystals of α-manganese has been investigated by micropillar compression at room temperature as a function of crystal orientation and specimen size. When the specimen size is reduced to the micrometer-range, single crystals of α-manganese are found to plastically deform by dislocation motion at room temperature for the first time, accompanied by very high yield stresses of the range of 4–6 GPa. Slip along [111] and [001] are identified to operate for compression axis orientations near [001] and near [011] and [1¯11], respectively. Any low-indexed planes cannot be designated as the slip plane for both slip along [111] and [001], because of the significantly wavy nature of slip lines caused by the occurrence of frequent cross-slip. Slip along [111] tends to prefer the slip plane of {112} rather than {110}. Slip along [001], on the other hand, tends to occur on the maximum resolved shear stress plane. The 1/2[111] dislocation carrying slip along [111] moves as a perfect dislocation without dissociating into partials and does not have any preferred orientation. The [001] dislocation carrying slip along [001] also moves as a perfect dislocation without dissociating into partials. Although the Peierls stress for the motion of these dislocations must be very high, there seems no deep Peierls valleys along particular directions, unlike the screw direction for the 1/2[111] dislocation in body-centered cubic metals. [Display omitted]