Abstract

The present work was carried out to examine the slip behavior under tension and the role of island grain on the deformation and fracture in a Mo single crystal. The tensile deformation characteristics of single-crystalline molybdenum sheet containing Ca and Mg of 50ppm and oxygen of 270ppm, which was prepared by secondary recrystallization, were investigated at 300 K and compared with that of the crystal containing a low level of oxygen (10ppm) in view of slip geometry and fracture behavior. Stress was applied approximately in the [011] direction. Conclusions are as follows: (1) slip system of ({bar 3}12)[111] dominated deformation at the beginning of yield and this slip system continued up to a strain of 0.09; (2) ({bar 2}11)[111] and ({bar 1}{bar 1}2)[111] began to act as another vital slip systems at a strain over 1.00; (3) stress drop phenomenon at a strain of 0.10 might be due to the change of slip system from ({bar 3}12)[111] to ({bar 2}11)[111] and/or ({bar 1}{bar 1}2)[111] by the rotation of crystal axis against the tensile axis; (4) cracks were generated from the island grain having different orientations from the matrix and separated from the matrix intergranularly. Subsequently the crack propagated along themore » ({bar 1}{bar 1}2) plane. It might be attributed to the pile-up of dislocations and the grain boundary weakening by the segregation of oxygen.« less

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